0003-017 (CSCS) Geotechnical InvestigationReport of Geotechnical Investigation
Proposed Commercial Building
State Highway I 11, West of Washington Avenue
Plaza La Quinta
La Quihia, Riverside County, California
-?S -4-3-7 Owl Ilk
CITY OF LA QUINTA
BUILDING & SAFETY DEPT
APPROVED
FOR CONSTRUCTION
DArE _jjjjet&_0 BY
FOR: cTfte-4 CV#Y
M & H Property Management, LLC
Attn: Mr. Glen Goodman
12555 High Bluff Drive,. Suite 385
San Diego, Calif6mia 92130
DATE:
February 3, 2000
PROJECTNO.
00-1562
D BY. -
PREPARE
Anthony -Taylor Consultants
3 4 17,nterprise Sti-ect
0
Escondido, California 92029
(760) 738-8800
I I TABLE OF CONTENTS
......................................................................
H. SITE DESCRIPTION .......................................................... 2
IGyneral .............................................................. 2
2. SiLc-L.C1,114"Y' . . : ....................................................... 2
3. Subsurface Condition ........ : .......................................... 2
4. Groundwate .......................................................... 3
Ill. FIE D EXPLORATION ........................................................ 3
IV. LABOR ATORY TESTING ...................................................... 4
V. CONCT I ISIONS .............................................................. 6
1. General ............................................................... 6
2. Gyroundwite .......................................................... 6
3. \Yloisrure Conten ....................................................... 6
4. FxpansiveSnik ........................................................ 7
5. Water Soluble Sulfate inSnilg ............................................. 7
6. 1 ind Slippage and Frosion ............................................... 7
7. Potentially eompressible Soils ............................................ 7
8. Seismic Considerations .................................................. 7
V1. RECOMMENDATIONS ....................................................... 10
I., Seismicity ........................................................... 10
2., Farthwork .. ............ ............................................ I I
3. Foundat ons and Slab Design ............................................ 13
4. Preliminary Pavement Mtsip ............................................ 15
5. Later3l Farth Pressures and Resistance ..................................... 16
6. Surface and Subsurface Drainagc ......................................... IS
7. Construction Observation and Plan Review .................................. 18
Vil. I-IN-11TATIONS .............................................................. Is
FIGURES:
la Vicinity Map
lb Site Map
Ila - lIc Excavation Logs
Illa Laboratory Soil Data Summary
Illb - Illc Direct Shear Test Results
Illd - Ille Consoliddtion-Pressure Curve
lIlf - Illp Mechanical Analysis - Sieve Test Data
APPENDICES:
A References
B Unified Soil Classification Chart
C Seismicity and Local Faulting
D Earthwork and Grading Guidelines
F Empirical Prediction of Earthquake - Induced Liquefaction Potential
wfifflcvmw�
ANTHONY -TAYLOR CONSULTANTS
304 Enterprise Street 0 Escondiclo, CA 92029 0 (760) 738-8800 s (760) 7.38-8232 fax
February 3, 2000
NI&H Property iNlanagement, LLC Project No. 00-1562
12555 High BlUffDrive, Suite 385
San Diego, California, 92130
Attention: Mr. Glenn Goodman
Subject: Report of Geotechnical Investigation
0
Proposed Commercial Building,
State Highway 111, West of Washington Ave
6 to
Plaza La Quinta,
La Quinta, Riverside County, California.
Dear Mr. Goodman:
In accordance with your request, Anthony -Taylor Consultants has performed a Geotechnical
Investigation to address the geotechnical conditions existing at the subject site. It is our
understanding that the proposed development will include the construction of a 6,600 square
foot commercial -type building, cement -concrete drive entrances, asphalted drive and parking
areas, and other associated improvements. The purposes of the investigation were to
determine the aeneral enoineerina characteristics of the soils underlying the subject site to
the depths explored and to provide engineenincy recommendations for the construction ofthe
proposed structures at the subject site.
This report describes: the investigation performed; the results and opinions of our findings;
and our geotechnical recommendations for constru'c'tion.
1. SCOPE
The scope,.of our geotiechnical investigation was based upon the planning information
I
provided to us, and consisted of field, laboratory, and engineering evaluation of site
conditibn's"'; to include:;
I Peview of readily available documents pertinent to the subject site (Appendix
A); '
2. Tlic excavation of 3 cxplorntory test horillgs withill bUildin(I J)Idand pirldn-
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area. The soils cncountcrcd-in the excavations were logged by our Field
Geologist and relatively undisturbed and loose bag samples were collected
S;tl) Diego, CA * Smi Franci..ico, CA - HOLISE011, TX
M&II Property Manacemcm. LLC Project No. 00-1562
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at selected intervals in the various soil types to the maximum depth of the
exploration;
3. Laboratory analysis of the collected samples;
4. Geotechnical analysis of the data and information obtained; and
5. Preparation of this report, presenting our conclusions and recommendations.
[HEMEN111"I WN.31WIDN'
1. General: The property consists of an irregular shaped lot with the approximate
dimensions of 214 by 167 feet. The area of study consists of an approximately 0.8
acre undeveloped lot located on the south side of State Highway III at
approximately 330 to 490 feet west of Washington Street, just east of the entrance
to'Plaza La Quinta Shopping Center, in the City of La Quinta, County of Riverside,
California. This site is located in a generally conunercial area and is bounded to the
north, by Highway 111, to the south and east by an asphalted parking area, and to the
west by the entrance to the Plaza La Quinta Shopping Center. Presently the site's
exposed surface consists of grass. It is our understanding that the proposed structures
and improvements are to be constructed upon surface crrades which are
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approximately similar in elevation to those currently existing.
2. Site Geolo-,Y: Regional geologic maps of the area (CDMG, 1966), indicate that the
subject site is located in an area near a contact between Quate rn ary'(rec ent)-7 aged
dUne sand deposits (alluvium), and Mesozoic granitic rocks. The site is located
approximately 5.7 miles from the Coachella Valley Portion of the San Andreas Fault
Zone, 6 miles from the San Gorgonio -Banning Fault Zone, 14 miles from the Blue
Cut Fault Zone:and 17 miles from the Hot Springs -Buck Ridge portion of the San
Jacinto Fault Zone. These fault zones are reported to have shown indications of Late
QpAternary-Ho.locene and historic seismic activity. Our review of the proper
fiterature (Hak, E. W. 1990) indicates that the subject site lies outside the present
Earthquake Fault Zones, which are described in the Alquist-Pr1olo Earthquake Fault
Zoning Act as being placed along active faults.
3. S.tibstirfau—Coliditioils: Subsurface materials encountered within our excavations
ColisisLed Of ki11dSCZ1pC tOpSoil (Fill) and dune sand (alhi%'11.1111) dcposits. Detailed
descriptions of U.-icsc matcrials can be found in the excavation logs (refer to Figure
2"Mr1r3,3
M&11 Properl) Mmiagriiiew. LLC Project No. 00-1562
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.1141:c 3 . if 20.
Nos. Ila through 11c). Based on Our Field investigation and laboratory testing, the
general characteristics of these units (from youngest to oldest) are described below.
I andscape Topsoi 1: We encountered minor amounts of landscape topsoll/fi I I soils in
all Of Our exploratory excavations. These fill soils were observed to have a thickness
of approximately Yz foot in the vicinity of our excavations. The encountered topsoil/
fill soils were observed to consist of brown sandy clay to clayey sand. This fill
material is considered to be potentially compressible and unsuitable to support any
structural loads in its present condition.
Dune Sand (Alluvium) Deposits: The encountered native soils are mapped in the
literature for this area (CD1'VIG, 1966), as being part of the Quatemary (recent) -aged
Dune sand (alluvium) deposits. These alluvial soils were observed to generally
consist of gray brown to olive brown and gray silty to clayey sands, sandy clays, and
sands. The sands crenerally ranged from very fine to fine and occasionally very fine
to medium arained. These soils were generally observed to be damp to very moist
and have a medium dense to dense consistency. This material was found to extend
to depths in excess of our deepest exploratory boring (approximately 51 V2 feet in
exploratory boring B-2). A detailed description of these soils is presented in our
excavation locys, Fiaure Nos. Ha throu-h Hc
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4. Groundwater: Free groundwater was not encountered in any of our exploratory
excavations to the maximum depths explored (approximately 51 V2 feet below
existinc, site arades), although evidence of perched water and wet conditions were
en ' countered at depth. A more detailed description of the subsurface materials
encountered in our exploratory borings is presented on the Boring Logs (Figure -Nos.
Ha through He).
Three (3),.exploratoryi;borings were drilled, logged and sampled for this study by our Field
Geologist on January 20, 2000 at the approximate locations shown on the Site Plan (Figure '
No. [b). The borings were advanced using a truck -mounted drill rig with an 6 -inch diameter,
solid-steni MI-er. Drive samples, recovered from all borings were obtained using a
Modificd Callfl�rriia Drive Sampler (2.5 -inches inside diameter and 3 -inches outside
diameter) with thin brass liners, and a Standard Penetrometer ( 2-inclics outside diameter
and I -3/8-hiclics hiside dianietcr). Thc samplers were drivcn 12 to IS Inclics into the soil
by a 140-POUnd hammer frec-falling for a distance of 30-inclics. The number of blows
required to penetrate the last 12 inches is shown on the Boring Logs. The obtained samples
M&II Properly NIjiu�cmew. LIX Project No. 00-1562
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were carefully removed, scaled to minimize moisture loss, and returned to our laboratory for
further classification and testing.
Representative bulk samples were collected from cuttings obtained from the borings. The
bulk samples were selected for classification and testing purposes and may represent a
mixture of soils within,the noted depths. Recovered samples were placed in transport
containers and returned to our laboratory for further classification and testing.
The classifications listed in the excavation logs are a result of visual classification of soil
with existing moisture contents while in the field. The classifications were assigned in
accordance with ASTM D-2488: "Description of Soils (Visual -Manual Method)", and all
applicable field soil -identification procedures described therein. These may or may not
correspond precisely to those indicated by subsequent laboratory methods. Classifications,
made in the field from auger cuttings and drive samples, were verified in the laboratory after
further examination and testing of samples.
Conditions between boring locations may vary considerably and it should be expected that
site conditions may or may not be precisely represented by any one of the bonings. Soil
deposition processes and topographic forming processes are such that soil and rock types and
conditions may change in small vertical intervals and short horizontal distances.
Stratification lines, as indicated on the Boring Logs, represent approximate changes in soil
and rock composition, moisture and color, as approximated by field personnel logging the
drilling operation and by the engineer in the laboratory from sample recovery data and by
observation of the samples. Actual depths to changes in the field may differ from those
indicated . on the logs, or transitions may occur in a gradual manner and may not be sharply
defined by a readily obvious line of demarcation.
The location of the borin-s as shown on Fi-ure No. Ib were approximately determined and
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should be considered accurate only as a reference guide.
�� WLII till MEN UsErm I OLIN I
Laboratory tests were performed on both disturbed and relatively undisturbed soil samples
in order to cvalLl,-ItC tI ' icir pertincnt physical and crigincering properties. The following tests
were conducted on the sampled soils:
I ) ' Moisturc Content
2) Density Evalt.1,16011S
ASTM D2216-71
ASTM D 1557, Mctliod A and.others
NI&II Properl Y M-An.-ircment. LLC Proftcl No. 00-1562
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3) Water Soluble Sulfate in Soil ASTM D1428, D516
4) Direct Shear Test ASTM D3080
5) Consolidation Test ASTN4 D2435
6) Sieve Analysis ASTNI D422
7) Expansion'Index Test AST?VI D4928, UBC 18-2
The relationship between the moisture and density of undisturbed soil samples give
qualitative information regarding the in-place soil strength characteristics and soil
conditions. Results of our in-place moisture and density testing are presented on the
Boring Logs (Figure Nos. Ha through IIc). The results of our maximum dry density
and optimum moisture content determinations are presented on Figure No. 111a.
I
The water soluble sulfate content of the near surface soils was deter -mined in
accordance with ASTIN/I Test Methods D1428 and D516, in order to estimate the
potential for sulfate attack on normal Type I/II cement. The results of our testing are
pr esented on Figure No. IIIa.
Direct shear testing was performed on a representative sample of the near surface
soils remolded to a relative compaction of 90 percent (based on ASTM D1557-91)
and on a representative sample of the alluvial soils in their natural state. Results of
this testing (Figure No. IIIb and HIc) indicate that in their properly compacted state,
the near -surface soils possess an apparent cohesion of 255 psf and an intemal friction
angle of 32 degrees, and the alluvial soils in their natural state have an apparent
cohesion of 190 psf and an internal friction angle of 33 degrees.
The consolidation test is used to estimate the consolidation/settlement that could
potentially occur within a soil under specific loadings (such as may be imposed by
buildings, walls, piers, etc.). The results of our testing are presented in Figure Nos.
JIld and Ille.
R i e . presentative' samples of the subsurface materials were subjected to mechanical
grain -size analysis by wet -sieving with U.S. Standard brass screens. The grain size
distribLiti011 Curves are presented in Figure Nos. IlIf through IlIp.
I
The expansion index of the Lipper foundation soils Was evaluated in accordance with
ASTM Test Pvlctliod D4928 (UBC 18-2), whCI-C I-CpI'CSCJJt!JtI Ve Sol I SItIIII)ICS il[*C tCS(CLI
a I a %
t SlItUrations near 50 percent. Expansive soils are classified s folio vs (by the
Expansion Index Test):
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-Pace 6 or 20.
0 to 20
Very Low
21 to 50
Low
51 to 90
Medium
91 to 130
High
Above 131
Very High
The tested soil sample yielded an Expansion Index of 15, which indicates a very IoNv
expansion potential for the sampled soils remolded to 90 percent relative compaction
(based on ASTIM D 15 5 7-9 1).
1. General: Based on the results of our study, it is our opinion that the proposed
structures can be -constructed as planned, provided that the recommendations
presented herein are implemented. It is our opinion that the on-site soils (when
properly processed and recompacted as recommended herein) should provide
adequate foundation support for the proposed structures and improvements.
2. Groundwater: As discussed previously, free. gToundwater was no ' t encountered in
any of our exploratory borings at the site, although a minor zone ith perched water
w
was encountered at depth. It is our opinion that this is a reasonable representation of
the minimum local groundwater depths at the site at the time of drilling. It should
be noted, however, that fluctuations in the groundwater level may occur due to
variations in ground surface topography, subsurface stratification, rainfall, imigation,
and other possible factors which may not have been evident at the -time. of our
investigation.
I
3. Pyloisture Conten : The in-place moisture contents of the samples obtained from the
upper soils, (upper 5 feet) in the proposed building area at the subject site, were
observed to range ftom 7.9 percent to 17.7 percent, with an average moisture content
.of,12.5 percent., The optimum moisture content for these upper soils was determined
''during our laboratory testing to range from 9.4 to 12.6 percent, indicating that the
ncar-SUrface soils underlying the proposed building pad area, generally possessed
moisture contents that were near optimum at the time of drilling. IVIOiStLire contents
of the near surface soils (upper 3 feet), within other areas of the site (i.e. drive and
parking areas), are anticipated to have similar moisturc contents. See Figure Nos. Ila
thl'OL11111 11C f01- 1110*1SILIN Content (k1t.1 Of 11CM- SUIT�ICC SO11S.
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4. Expansive Soil : The near -surface soils (upper I to 5 feet) encountered in our
exploratory borings were observed to consist mainly of sands. Based on our
laboratory testing of representative samples obtained at the subject site, these
materials appear to possess a very low potential for expansion. The likelihood for
expansive soils to affect the overall perfon-nance of the proposed structure
foundations and associated improvements (e.g. paving) appears to be low. Anthony -
Taylor Consultants may provide additional recommendations if indications of a
si nificant chan-e in the near -surface soils' expansion potential are encountered
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durinor construction.
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5. Water Soluble Sulfate in Soils: The principal cause of deterioration of concrete in
foundations and other below ground structures is the corrosive attack by soluble
sulfates present in the soil and groundwater. The results of water soluble sulfate
testing performed on a representative sample of the soils underlying the proposed
building structure near present finish grade elevations, indicate that proposed cement -
concrete structures that are in contact with the underlying soils are anticipated to be
affected with a nealicrible sulfate exposure.
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6. I -and Slippage and Fro-sion: No significant indications of either land slippage or
erosion were noted at the site. Therefore, it is our opinion that the potential for land
slippage or erosion to affect the proposed improvements at the site is minimal,
0
provided that the recommendations presented herein are implemented.
7. Potentially Compressible Soils: As noted before, the existing topsoil and upper
alluvium soils are considered to be potentially compressible and unsuitable for the
support of structural loads in their current condition. As a result, these upper soils
should be properly reprocessed in accordance with the recommendations presented
herein.
M
8.1 Regional and Local Faulting: The principal seismic considerations for
improvements at the subject site are surface rupture of fault traces, damage
caused by ground shaking during a seismic event, and scismically-induced
ground settlement. The potential for any or all of these hazards depends upon
the recency Of fault activity and the proximity of nearby faults to the subject
site. The possibility of damage due to ground rupture is considered unlikely
SHICC 110 ',ICtIVC EMIUS 11'C IWOW11 tO UOSS tlIC SitC 111d 110 CVidCIICC Of IIC(iVe
ElUlting MIS noted during our investigation. Review of geologic literature
(Appendix A) indicates that the Subject sitc is located in an arca Surrounded
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by active and potentially active fault zones. Tile nearest major active faults
are the Coachella Valley portion of the San Andreas Fault Zone, located
approximately 5.7 miles from ' the area of study, the San Gorgonio -Banning
Fault Zone, located approximately 6 miles from the subject site, tile Blue Cut
Fault Zone, located at approximately 14 miles from tile site and, the Hot
Springs -Buck Ridge portion of the San Jacinto Fault Zone, located at
approximately 17 miles from the area of study. A list of active and
potentially active faults located within a 100 mile radius of the subject site is
presented in Appendix D.
8.2 Seismicity: The seismic hazard most likely to impact the site is ground
shakin- due to a large earthquake on one of the major active regional faults.
Because of the proximity to the subject site and the maximum probable event,
for this fault, it appears that the San Gorgonio -Banning Fault Zone is most
0 ID
likely to affect the site with severe ground shaking, should a significant
earthquake occur along, this fault. A maximum probable event along this fault
zone could produce a peak horizontal acceleration of approximately 0.46g at
the subject site. With respect to this hazard, the site is comparable to others
in this general area within similar -eolocic settin-s. A summary of seismic
desip
g parameters associated with the major faults located within a radius of
100 miles of the site is presented in Appendix D.
8.3 Liquefaction: Liquefaction of soils can be caused by strong vibratory
motion in response to earthquakes. Both research and histonical data indicate
that loose, mostly fine sands or predominantly granular soils are susceptible
to liquefaction, while the stability of rock is not as adversely- affected by
vibratory motion. Liquefaction is generally known to occur pnimarily in
saturated or near -saturated granular soils at depths shallower than about 100
feet and is also a function of relative density, soil type and probable intensity
and duration of ground shaking. Because of the relatively deep groundwater
table and the presence of layers of dense soil and layers of cohesive materials
in the. underlying soils, it appears that the potential for liquefaction at the site
dUring'a major seismic event is relatively low.
As noted previously the Subject site is situated in an area underlain by
predominantly silty sands and sandy slits and a relatively deep groundwater
table. We have evaluated the potential for liquefaction at the site using the
LIQUEFY2 COIIII)LIICI' (1313kC, 1998). OLII' 'ifflillySiS, Which MIS
1�
performcd in accordance with the procedure rcconimcnded by Seed, ct. al.
(IM), incorporatcs the gcotechnical data obtained from our exploratory
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SIMI Properly Nhwigemcm, LLC
February 12000
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Project No. 00-1562
boring B-2 and addresses a niaxiinuni probable seismic event along San
Gorgonio -Banning Fault Zone.
Our subsurface investigation did not encounter a ground water table to the
maximum depth explored (approximately 51.5 feet in Boring B-2). Therefore
it is anticipated that the liquefaction potential is low for this site. However,
we assumed that the depth to the groundwater table could hise at some time
in the future and we performed additional calculations assuming a
groundwater table at both 20 and 40 feet below existing site grades. The
results of these calculations (Appendix D) indicate that for groundwater at
a depth of 20 feet, the subsurface materials generally possess a factor of
safety against liquefaction of greater than 1.25 but may be potentially
liqUefiable at depths between 19 and 25 feet. For the encountered depth to
(2round water of greater than 25, the subsurface materials generally possess
a factor of safety against liquefaction of greater than 1.25. As a result, it
appears that the soils encountered at the site under the present conditions, are
not considered to be potentially liquefiable. The liquefaction analysis was
performed using existinc, conditions at the time of dnilling and for
groundwater at depths of 20 and 40 feet. Changes in the existing conditions
may affect the results of this analysis, such as a fluctuation in the depth of
groundwater, may affect of the depth to liquefiable soils by raising or
lowering, this depth.
The underlying soils were found to be generally dense to very dense to the
depths explored, and consist predominantly of sands and silty sands with an
approximately 3- to 5 -foot layer of very fine plastic soils at a depth of 36 feet.
Based on these conditions, the potential for liquefaction of the upper soils at
the subject site is considered to be relatively low. As such, surface
manifestations as dynamic settlement and lateral displacement can be
expected to not affect the site during or after a seismic event. Based on
evaluations of seismically -induced settlements and lateral spreading in
accordance with the procedures suggested by TokimatSU and Seed (1987) and
Bartleit and YOLid (1995), respectively, and based on our evaluations of
Subsurface soil conditions, we estimate that total and differential dynamic
settlements across the proposcd building pad will not be large enough to
affect the proposed site construction.
8A SCiSllliC SCUIC111CIlt: SCiS1111C SCUIC111CIA OCCLII"; WlICII loose to IIIC(liLlill-
c1cii.se, granular soils consolidate (IL11-ing ground shaking. The materials which
underlie the Subject site were observed to be primarily a niedium dense silty
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sands. As such, it appears that the soils underlying the subject site possess a
relatively IoNv potential for seismically induced settlement in their present
condition. .
8.5 Design Eirtliquake Magnitude: The review of readily ava liable references
pertinent to the subject site indicates that structures should be designed to
resist moderate earthquakes with a low probability of structural damage. Such
design shall resist major or severe earthquakes with some structural damage,
but with a low probability of collapse. The moderate and major earthquakes
have been interpreted to represent the maximum probable and maximum
credible earthquakes, respectively. The maximum credible earthquake is
defined as the largest event that a specific fault is theoretically capable of
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producing within the presently kno-wri tectonic framework and is established
based on mechanical relationships of the fault and fault mechanisms and does
not consider rate of recurrence or probability of occurrence. The maximum
probable earthquake is generally defined as that seismic event along a
0 1.7
particular fault which has a 10 percent probability of being exceeded in 50
years. The repeatable high bedrock acceleration, which is considered
appropriate for structural desip, is estimated to be approximately two-thirds
of the peak acceleration for events within a radius of about 20 miles of the
site and is considered equal to the peak acceleration beyond 20 miles
(Ploessel and Slosson, 1974).
�WRDEKSMIDIX91
Based on our geotechnical study at the site, our review of readily available reports and
literature pertinent to the site (Appendix A), and our understanding of the proposed final
grades, it is our opinion that development and/or improvement of the site is feasible from a
geotechnical standpoin ; t, provided the conclusions and recommendations included in this
report are'properly incorporated into the design and construction of any proposed structures.
There appear to be no .significant geotechnical constraints on-site that cannot be mitigated
by proper plannin,'),, d e2sign, and utilization Of Sound construction practices. The engineeHng
properties of the underlying materials, surface drainage, and anticipated degree of seismic
risk offer conditions comparable to the other sites surrounding the subject project. The
following sections provide geotechnical recommendations that should be incorporated into
the design orthe proposcd improvements at the sitc.
Sdsifflrity: The MaXilllUm anticipated bedrock acceleration at the site is estimated
to be oil tile order of 0.46g, based oil a maximum probable earthquake on the San
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Gorgonio -Banning Fault Zone. However, sites founded upon non -bedrock materials
(e.g. alitlVil.11111 or compacted fill) may experience higher values of acceleration. For
design Purposes, two-thirds of the maximum anticipated bedrock acceleration may
be asSLII-ned for the repeatable high ground acceleration. The effects of seismic
shakin- can be mitigated by adhering to the current edition of the Uniform Building
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Code and/or state-of-the-art seismic design parameters of the Structural Engineers
Association of Califomia. The following earthquake design parameters are
recommended for the subject site:
Table 16 - I
Z = 0.40
Table 16 - J
Soil Type —SD
Table 16 - Q
C:�. = 0.44 N�
Table 16 - R
C, = 0.64 N,
Table 16-S
N;� = 1.0
Table 16 - T
N, = 1 2
Table 16 - U
Source Type -A
2. Farthivork: Grading, and earthwork should be performed in accordance with the
followinc, recommendations and the General Earthwork and Grading Guidelines
C,
included in Appendix E. In case of conflict, the following recommendations shall
supersede those presented in Appendix E.
24. Site Preparation: Pnior to earthwork or construction operations, the site
should be cleared of surface and subsurface obstructions and stripped of any
veo,etation in the areas proposed for development. Removed vegetation and
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debris should then be properly disposed of off-site. Holes resulting from
removal of buried obstructions which extend below finish site grades should
be backfilled with suitable fill soils compacted to a minimum 90 percent
relative compaction (based on ASTM Test Method D1557-91).
�2.2. Removal of Unsuitable Soils: As noted above, the existing landscape
topsoil . -fill and upper alluvium soils are considered to be potentially *
compressible in their current condition. As a result, we recommend the
reprocessing of these existing soils in all areas to receive new buildings
(where not anticipated to be removed during proposed site development).
Based on the results of our subsurface investigation, it is anticipated that the
NMOV�ll dCl)[11S ill thC ViCillity Of [11C J)l'OJ)OSCd bl.lildillg pad will bC Oil tllc
orcicr of 3 to 3 Y2 feet below existing grade elevations. Following removal of
the Lipper soils, tile bottoni of the cxcavation(s) should be observed and
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approvcd by a representative of this office to verify that these potentially
compressible materials have been properly removed. All areas to receive fill
and/or other surface improvements, shall be scarified to a minimum depth of
8 inches below removal grade elevations, brought to near-optimurn moisture
conditions and recompacted to at least 90 percent relative compaction (based
on ASTNI Test Method D1557-91). Theseoperations silo u Id be performed
Linder the observation and testing of a representative of this office: It should
be understood that based on the observations of our field representative,
localized deeper or shallower removals may be recommended. Any removed
soils shall be moisture conditioned as necessary to achieve a moisture content
of at least 2 percent over optimum moisture content and recompacted to a
minimum 90 percent relative compaction (based on ASTIVI Test Method
D 1557-9 1). This earthwork should extend a minimum of 3 feet beyond the
proposed footing limits.
I
2.3. Fill Placement and Compaction: If necessary, the on-site soils are suitable
for reuse as compacted fill, provided they are free of organic materials and
debris and material larger than 6 inches in diameter. All areas to receive fill
and/or other surface improvements should be scarified to a minimum depth
of 8 inches, brought to a moisture content of at least 2 percent over optimum
moisture content and recompacted to at least 90 percent relative compaction
(based on ASTM D1557-91). Should import soils be.utilized for near -surface
fills, these soils should be predominately granular, possess a low or very low
expansion potential, and be approved by the geotechnical engineer prior to
their transportation to the site. Lift thicknesses will be dependent upon the
size and type of equipment used. In general, fill should be placed in uniform
lifts not exceeding 8 inches. Placement and compaction of fill should be
performed in accordance with lo cal grading ordinances under the observation
and testing of the geotechnical consultant.
We recommend that if encountered, oversize materials (materials greater than
6 inches in maximum dimension) be removed from the upper 3 feet of fill or
placed in accordance with the General Earthwork and Grading Guidelines
'D
contained in Appendix E.
2.4. Trench Excavations and Backfill: Trenches are anticipated to be excavated
with moderate Cff0i-t using conventional construction equipment in good
operatilig condition. To Satisfy OSIIA 1'C(lUi1'C111C111S U11(i f01_ \\'01'1�111CII'S
0
safety, it will be necessary to shorc excavations deeper than 5 feet.
ME
�i
hI&II Properly %I;ma�vmcw. I.I.0
February 3. 2000
-raze t3 or 20 -
Project No. 00-1562
The on-site soils may be used as trench backfill provided they are screened
of rock sizes over 6 inches in maximum dimension and organic matter.
Trench backfill should be compacted in unifor-ril lifts (not exceeding 8 inches
in compacted thickness) by mechanical means to at least 90 percent relative
compaction (based on ASTM D1557-91).
3. Foundations and Slab Design: Foundations and slabs should be desi-ned in
accordance with structural considerations and the following recommendations.
These recommendations assume that soils exposed at finish pad grade will have a
low potential for expansion. These recommendations may be venified by performing
additional expansion tests after grading is completed. Localized areas of higher
expansion may be possible.
3.1 Foundation Design: All proposed building and non -building improvements
that are anticipated to constitute a structural load may be supported by an
appropriate foundation system designed by -the project structural engineer in
accordance with the guidelines of the Uniform Building Code and/or all
applicable local building codes. Footings adequately founded in firTn natural
soils or properly compacted fill soils should be a minimum 18 inches deep
by 12 inches wide for a one-story building structure and 24 inches deep by
15 inches wide for a two-story building. At these dimensions, footings
adequately founded properly compacted fill soil may be designed for an
allowable soil bearing value of 2000 pounds per square foot. These values
may be increased by one-third for loads of short duration including wind or
seismic forces. Foundations should be properly reinforced in accordance
with the project structural engineer's recommendations'. ' Minimum
reinforcement shall consist of two No. 4 rebar at the top and two No.4 rebar
at the bottom of the footing. We estimate that the total and differential
settlement for the proposed improvements will be on the order of 1 -inch and
approximately V4 -inch between structural elements.
To reduce the pbtential for misalignment of gara-e door openings at the site
(If th ey are proposed), we recommend that a grade beam be constructed
across each garage door entrance. These grade beams should be designed
and reinforced in accordance with tile structural engineer's requirements.
We recommend a minimum horizontal setback distance from tile face of
dCSCCIldiIIg SIOI)CS 1111(1/01' I-C(MililIg WIIIIS f0l' !III StRICtUr,11 footings 111d
SCttICI1lCI1t-SCIlSitiVC StRICtUres. This distance is Measured fi-0111 tile Outside
bottom edge ofthe footing, horizontally to the slope face or wall face and
NU11 Property Mamigement, LLC Project No. 00-1562
February 3. 2600
-Page 14' of 20.
Should be a rnininium of H/2, where H is the slope height or wall height (in
feet). Tile setback Should not be less than 5 feet and need not be greater than
10 feet. Please note that the soils within tile structural setback area may
possess poor lateral stability, and improvements (such as retaining walls,
pools, sidewalks, fences, pavement, etc.) constructed within this setback area
may be subject to lateral movement and/or differential settlement.
All foundation excavations should be observed and tested by a representative
of Anthony -Taylor Consultants prior to placement of steel and concrete.
3.2 Concrete Slabs: Interior concrete slabs should have a minimum thickness
o f 5 inches and be underlain by a I 0 -mil visqueen moisture barrier underlain
With a 2 inch layer of clean sand (sand equivalent of at least 30). The
visqueen moisture barrier should be overlain by a 2 inch layer of clean sand
'd in concrete curin-. All slabs should be constructed with preferred
to al
minimum reinforcement consisting of No.. 3 bars placed mid -height in the
slab and spaced on IS inch centers in both directions. Welded wire mesh is
not an acceptable altemative. Crack control joints should be provided in
accordance with the recommendations of the project structural engineer.
0
Exterior concrete flatwork (sidewalks, etc.) should have a minimum thickness
of 4 inches, be underlain by a 2 -inch layer of clean sa ' nd, and- reinforced with
a minimum 6x6 - 10/10 welded wire mesh placed midhelght in the slab. Care
should be taken by the contractor to ensure that the reinforcement is placed
and maintained at slab midheight. We recommend that crack control joints
for exterior flatwork be provided with a minimum spacing of 12 feet and a
maximum of 15 feet, or in accordance with the structural engineer's
recommendations. We also recommend that every third control joint be
converted to an expansion joint.
Some slab cracking due to shrinkage should be anticipated. The potential for
this slab cracking may be reduced by careful control of water/cement ratios.
The contractor should take appropriate curing precautions during the pouring
of concrete in hot weather to minimize crackin,, of slabs. We recommend
that a slipsheet (or equivalent) be utilized if crack -sensitive flooring is
planned directly on concrete slabs. All slabs should be designed in
accordi
. nce with structural considerations.
3.3 Cenient Type: As noted before, our laboratory testing of a representative
sample of tile ncar surface indicated a negligible concentration Of Soluble
IN1.0411 llrolwrly Maiw�cmrnl. LLC
Project No. 00- 1562
February 3, 2000
-Plage 15 of 20.
sulfates. Based on the guidelines presented in the current edition of the
Uniform Building Code, a minimum Type 11 cement may be utilized in
concrete that will be in direct contact with the near -surface soils.
3.5 Moistenina of Foundation Soils: Footing excavations and slab subgradds
to
should be thorouahly moistened prior to placement of concrete. The soil
0
moisture should be at least 2 percent over optimum to a depth of at least 24
inches below finish grade..
4. Preliminary Pavement Desian: For design purposes and based on our experience
with similar soils, we assumed an R -Value of 30 for the subarade soils. Actual
1.7
paving sections based on laboratory test results should be performed on samples
obtained from finish grade elevations. For preliminary design purposes, we have
assumed traffic indices of 4.5 for parkina areas and 6.0 for drive areas. These
0
assumed traffic indices should be verified by the project civil engineer prior to
construction. The preliminary recommended structural pavement sections were
calculated in accordance with the Caltrans Highway Design Manual and are
0
summarized below
Main Drive Areas
Design R -Value = 30, Assumed T.I. = 6.0
4.0 inches of asphalt concrete over 6.0 inches of Caltrans Class 2 aggregate base.
Parking Areas
Design R -Value = 30, Assumed
ID T.I..=.4.5
3..0 inches of asphalt concrete over 4.0 inches of Caltrans Class 2 aggregate base
We recommend that drive entrances and other areas subject to heavy vehicle loading
recei * ve a full -depth Portland Cement Concrete (P.C.C.) section of 5 inches over 4
inches of Caltrans Class 2 aggregate base. This rigid section is based upon a
minimum concrete strength of 3000 psi. We also recommend for these areas a
miniIIIUm reinforcement consisting of No. 3 rebar spaced at 18 inches on center in
two directions. Concrete (P.C.C.) parking areas may utilize a minimum
reinforcement of No. 3 rcbar spaced at 24 inches on cc ' ntcr in two directions. We
recommend that the rebar be placed midlicight in each slab. Care should be taken by
the contractor to ensure that the reinforcement is placed and maintained at slab
=3=14.%&A
M&II Propert.s LIA, Prnlect No. 00-1562
Vchruary J. MHO
.112ge 16 of 20.
midlicight. We recommend that crack control joints for concrete pavement be
ided with a minimum spacing of 12 feet and a maximum of 15 feet, or in
provi 1 -D
accordance with the structural engineer's recommendations. We also recommend
that every third control joint be converted to an expansion Joint. We suggest that slab
sections be nearly square as possible. Placement of concrete should be performed in
accordance with the guidelines of the American Concrete Institute (A.C.I.) and all
local building codes.
I
We recommend that curbs, gutters and sidewalks be designed by the project civil
encyineer or structural enaineer. We suggest control joints at appropriate intervals as
deten-nined by the civil encrineer or structural en-ineer be considered.
0 0
Based on the results of our subsurface investigation, and the presence of loose topsoil
in the proposed parking and drive areas, it is anticipated that the removal depths in
these areas will be on the order of I to 1'/2 feet below existing grade elevations.
Following removal of the upper soils, the bottom of the excavation(s) should be
observed and approved by a representative of this off -ice to verify that these
potentially compressible materials have been properly removed. All areas to receive
fill and/or other surface improvements be scarified to a minimum depth of 8 inches
below existing grade elevations, brought to a moisture content at least 2 percent over
the optimum moisture content for these soils and recompacted to at least 90 percent
relative compaction (based on ASTM Test Method D1557-�91). The-uppei-6 to8
inches of pavement subcYrade soils should be conditioned as necessary to achieve a
near optimum moisture content, and recompacted to at least 95 percent relative
compaction (based on ASTM Test Method D1557-91), or in accordance with the
minimum compaction requirements of the County of Riverside. The untreated Class
2 aggregate base material placed as part of the pavement structural section should
meet the requirements of Caltrans specifications and be compacted to a minimum
95 percent relative compaction (based on ASTM Test Method D 1557-9 1).
If 'pavement areas are adjacent to heavily watered landscape areas, we recommend
some measure of moisture control be taken to prevent the subgrade soils from
becoming saturated. It is recommended that the concrete curbing separating the
landscaping area from the pavement extend below the aggregate base to help seal the
ends of the ' sections where heavy landscape watering may have access to the
aggregate basc. Concrete swales should be designed in roadway or parking areas
subject to concentrated surface runoff.
S. LatuaLL, arili Pres mas—awl Resistaila: For design purposes, the following
11IM-111 C111-111 pl-CSSUre V,11LICS for level and frce-draining backfill are rcconinicrided for
N1,0411 Priplirri ' y Mmiagemew. LLC
FebruarY J. .10011
-Pace I I of 20-
1'rojcct No. 00-1562
rctaining walls (iLpmpD,=-d) backfillcd with on-sitc soils, and for those backfillcd
with sclect soils (possessing an intcmal friction angle of at least 30 degrees and
extendinI.; at least 0.5H from the upslopc face of the wall, where H is the wall height).
EQUIVALENT FLUID WEIGHT (PCF)
Conditions
I
On -Site Rackfill
Select Backfill
1 (PHI�29 Degrees)
Active
36
-1
35
At -Rest
56
55
Passive (Fill Soils)
375
350
Unrestrained (yielding) cantilever walls should be designed for an active equivalent
pressure value provided above. In the design of walls restrained from movement at
the top (nonvielding), such as basement walls or re-entrant comers, the at -rest
pressures should be used. For areas of re-entrant comers, the restrained wall design
should extend a minimum distance of twilice the height of the wall laterally from the
comer. The above values assume backfill soils will have a very low expansion
potential and free -draining conditions. If conditions other than those covered herein
are anticipated, the equivalent fluid pressures should be provided on an individual
basis by the geotechnical engineer. Retaining wall structures should be provided
with appropriate drainage. Typical drainage design is illustrated in Appendix E.
Wall backfill should be compacted by mechanical methods to at least 90 percent
relative compaction (based on ASTM Test Method D1557-91). Wall footings should
be designed in accordance with the foundation design recommendations and
reinforced in accordance with structural considerations. For all retaining walls, we
recommend a minimum horizontal dista-rice from the outside base of the footing to
daylight of 8 feet.
Lateral soil resistance developed against lateral structural movement can be obtained
from the passive pressure value provided above. Further, for sliding resistance, a
friction coefficient of 0.30 may be used at the concrete and soil interface. These
values may be increased by one-third when considering loads of short duration
illCILIC1111g Willd 01- SCiS111iC 10,1(ls. The total rcsist,�mcc may be takcii is the sum ofthc
frictional and passive resistance providcd that the passive portion does not exceed
two-thirds of the total resistance.
I - ff-
M&II Prolwrty M;sfia�cmrw. LLC Proiccl No. 00-1562
Ftbriury J. 2000
-Pige Im ir n.
6. SjLrLace and SubsurLice Drainage: Our experience indicates that surface or near
Surface ground water conditions can develop in areas where ground water conditions
did not exist prior to site development, especially in areas where a substantial
increase in Surface water infiltration results from landscape irrigation. This
sometimes occurs where relatively impermeable and/or cemented formational
materials are overlain by fill soils. In addition, during retaining wall excavations (if
they are proposed), seepage may be encountered. We recommend that Anthony -
Z
Taylor Consultants be present duning grading operations to evaluate areas of seepage.
Drainage devices for reduction of water accumulation can be recommended if these
condutions occur.
We recommend that measures be taken to properly finish grade the site, such that
Surface drainage is directed away from structure foundations, floor slabs, and tops of
slopes, at a 2 percent minimum grade for a minimum distance of 5 feet for subgade,
and I percent minimum grade for a minimum distance of 5 feet for hard finish
su rface (pavement, walkways etc.). Ponding of water should not be pen-nitted, and
installation of roof gutters which outlet into a drainage system is considered prudent.
0 ZD
Planting areas at gade should be provided with positive drainage directed away from
all buildings. Drainage design for these facilities should be provided by the design
c i 'I en,7ineer.
ivi
7. Construction Observation and Plan Review: The recommendations provided in
this report are based on subsurface conditions disclosed by field reconnaissance and
widely -spaced exploratory borings. The interpolated subsurface conditions should
be checked in the field during, construction by a representative of Anthony -Taylor
Consultants. We recommend that on-site excavations be observed during -grading for
the presence of potentially adverse geologic conditions by a representative of this
firm. Construction observation and field density testing of compacted fill should be
performed by a representative of this firm to ensure that construction is in accordance
with the recommendations of this report. The final grading plan and building plan
-should be reviewed by this office prior to construction.
V11. LIMITATIONS
This report presents recommendations pertaining to the subject site based on the assumption
that 01C SUbSurfacc conditions do not deviate appreciably from those disclosed by our
CXJ)101-M01'y CXCaVat1011S. 01.11' I-CCommendations arc based on the tcclinical inflort"ation
gallicred, 0L11- Undcrstanding of the proposcd construction, and Our cxperience in the
geotcclinical ficid. We do not provide a guarantee or warranty (either expressed or implied)
WAMCCOMT
M& It Property Maiucemcm. LLC Project No. 00-IS62
Vchmars- 3. 2000
-11ne 19 of
of the perfon-nance of the project, only that our engineering work and judgements meet the
standard of care of our profession at this time.
In vicxv of the general conditions in the area, the possibility of different local soil conditions
cannot be discounted. Any deviations or unexpected conditions observed during construction
should be brought to the attention of the Geotechnical Engineer. In this way, any required
supplemental recommendations can be made with a minimum of delay to the project.
If the proposed construction will differ from our present understanding of the project, the
existing information and possibly new factors may have to be evaluated. Any design changes
and the final grading and foundation plans should be reviewed by the Geotechnical
Consultant. Of particular importance would be extending development to new areas, changes
ges
in structural loading conditions, postponed development for more than one year, or chan.,
in ownership.
This report is issued with the understanding that it is the responsibility of the owner or
owner's representative to ensure th ' at the information and recommendations contained herein
are called to the attention of the Architects and Engineers for the project and incorporated
into the plans and that the necessary steps are taken to ensure that the Contractors and
Subcontractors carry out such recommendations in the field. This report is also subject to
review by the controlling authorities for this project.
M& If Property Min2fienicni. I.I.0
1'ehruary 3. !000
-11ace 10 or lo -
Project No. 00-1562
We appreciate this opportunity to be of service to you. If you have questions or need further
information, please refer to Project No. 00-1562 to expedite your requests.
Respectfully Submitted,
ANTHONY -TAYLOR CONSULTANTS
An Anthony -Taylor Company
"16 2d) 12 -1
Bruce Ta rry ichal
'or U
President enio roject Engineer
CEG No 9760 RCE No. C42590 0
3-S
CID
ORME W.
C M
1z
No. C 4�590 M
CEMIED
040104"EANO ExpfL4(,6
Hector. ella GEOLOWST
Project I -ist
OF C
Distribution: 3 addressee (2 originals and I copy)
HCCt4r1J1M1LA 000A GFO.wpd
TYPICAL RETAINING WALL DRAINAGE DETAIL
RETAINING WALL
WTERPROOFING AS NOTED
IN THE ATTACHED FIGURE
FINISHED GRADE
-------------------
��.comp ED FILL
-----IF APPLICABLE----------.
SOIL BACKFILL, COMPACTED TO
90 PERCENT RELATIVE COMPACTio.-i
PER ASTM D1557
18"-MI.N.
6" MIN. 'FILTER FABRIC ENVELOPE
7---7-' (MIRAF1 140N OR APPROVED
EQUIVALENT)
3/4" - 1-1/2" CLEAN GRAVEL
:L7
1 MIN -
4" (MIN.) DIAMETER PERFORA, 7 ED
PVC PIPE (SCHEDULE 40 OR
EQUIVALENT) WITH PERFORATICNS
ORIENTED DOWN AS DEPICTED
- - - MINIMUM 1 PERCENT GRADIENT
TO SUITABLE OUTLET
3" MIN.
WALL FOOTING :7
COMPETENT BEDROCK OR MATERIAL
AS EVALUATED BY THE GEOTECHNICAL
CONSULTANT
NOT TO SCAL
ANTHONY -TAYLOR CONSULTANTS
XIUN3ddV
L I Q U E F Y 2
Version 1.20
EMPIRICAL PREDICTION OF
EARTHQUAKE -INDUCED LIQUEFACTION POTENTIAL
JOB NUMBER: 00-1562 DATE: Thursday, February 3, 2000
JOB NAME: LA QUINTA
LIQUEFACTION CALCULATION NAME: LA QUINTA LIQUEFACTION STUDY
SOIL -PROFILE NAME: SANGERL
GROUND WATER DEPTH: 20.0 ft
DESIGN EARTHQUAKE MAGNITUDE: 7.00
SITE PEAK GROUND ACCELERATION: 0.462 g
K sigma BOUND: M
rd BOUND: M
N60 CORRECTION: 1.00
FIELD SPT N -VALUES < 10 FT,DEEP ARE CORRECTED FOR SHORT LENGTH OF DRIVE
RODS
NOTE: Relative density values listed below are estimated using equations
o f �. !'..
. I Giuliani -and Nicoll (1982).
-----------------------------
LIQUEFACTION ANALYSIS SUMMARY
-----------------------------
-----------------------------
Seed and Others (1985) Method PAGE
-----------------------------
I
CALC.1
TOTALI
EFF. IFIELD
lEst.D I
I
CORR.ILIQUE.1
JINDUC.ILIQUE.
SOILI
DEPTHISTRESSISTRESS1
N
I rl
C I(NI)601STRESSI
r ISTRESSISAFETY
NO.1
(ft) I
(tsf)l
(tsf)I(B/ft)
I M I
N l(B/ft)l
RATIO1
d I
RATIOIFACTOR
-----------------------------------
7 -------------------------------------------
1 1
0.251
0.0131
0.0131
14
1 71
1 @ I
@ I
@ I
@ I
@ I
@ @
1 1
0.751
0.0381
0.0381
14
1 71
1 @ I
@ I
@ I
@ I
@ I
@ @
1 1
1.251
0.0631
0.0631
14
1 71
1 @ I
@ I
@ I
@ I
@ I
@ @
1 1
1.751
0.0881
0.0881
14
1 71
1 @ I
@ I
@ I
@ I
@ I
@ @
1 1
2.251
0.1131
0.1131
14
1 71
1 @ I
@ I
@ I
@ I
@ I
@ @
1 1
2.751
0.1381
0.1381
14
1 .71
1 @ I
@ I
@ I
@ I
@ I
@ @
1 1
3.251
0.1631
0.1631
14
1 71
1 @ I
@ I
@ I
@ 1
0 1
@ @
1 1
3.751
0.1881
0.1881
14
1 71
1 @ I
@ I
@ I
@ I
@ I
@ @
1 -1
4.251
0.2131
0.2131
14
1 71
1 @ I
@ I
@ I
@ I
@ I
@ @
1 1
4.751
0.2381
0.2381
14
1 71
1 @ I
@ I
@ I
@ I
@ I
@ @
1 1
5.251
0.2631
0.2631
14
1 71
1 @ I
@ I
@ I
@ I
@ I
@ @
1 1
5.751
0.2881
0.2881
14
1 71
1 @ I
@ I
@ I
@ I
@ I
@ @
1 1
6.251
0.3131
0.3131
14
1 71
1 @ I
@ I
@ I
@ I
@ I
@ @
1 1
6.751
0.3381
0.3381
14
1 71
1 @ I
@ I
@ I
@ I
@ I
@ @
1 1
7.251
0.3631
0.3631
14
1 71
1 @ I
@ I
@ I
@ I
@ I
@ @
1 1
7.751
0.3881
0.3881
14
1 71
1 @ I
@ I
@ I
@ I
@ I
@ @
1 1
8.251
0.4131
0.4131
14
1 71
1 @ I
@ I
@ I
@ I
@ I
@ @
1 1
8.751
0.4381
0.4381
14
1 71
1 @ I
@ I
@ I
@ I
@ I
@ @
1 1
9.251
0.4631
0.4631
14
1 71
1 @ I
@ I
@ I
@ I
@ I
@ @
2 1
9.751
0.4881
0.4881
15
1 66
1. @ I
@ I
@ I
@ I
@ I
@ @
2 1
10.251
0.51410.5141
15
1 66
1 @ I
@ I
@ I
@ I
@ I
@ @
2 1
10.751
0.5411
0.5411
15
1 66
1 @ I
@ I
@ I
@ I
@ I
@ @
2 1
11.251
0.5671
0.5671
15
1 66
1 @ I
@ I
@ I
@ I
@ I
@ @
2 1
11.751
0.5931
0.5931
15
1 66
1 @ I
@ I
@ I
@ I
@ I
@ @
2 1
12.251
0.6191
0.6191
15
1 66
1 @ I
@ I
@ I
@ I
@ I
@ @
2 1
12.751
0.6461
0.6461
15
1 66
1 @ I
@ I
@ I
@ I
@ I
@ @
2 1
13.251
0.6721
0.6721
15
1 66
1 @ I
@ I
@ I
@ I
@ I
@ @
2 1
13.75.1
0.6981
0.6981
15
1 66
1 @ I
@ I
@ I
@ I
@ I
@ @
2 1
14.251
0.7241
0.7241
15
1 66
1 @ I
@ I
@ I
@ I
@ I
@ @
3 1
14.751
0.7511
0.7511
22
1 74
1 @ I
@ I
@ I
@ I
@ I
@ @
3 1
15.251
0.7771
0.7771
22
1 74
1 @ I
@ I
@ I
@ I
@ I
@ @
3 1
15.751
0.8031
0.8031
22
1 74
1 @ I
@ I
@ I
@ I
@ I'
@ @
3 1
16.251
0.8291
0.8291
22
1 74
1 @ I
@ I
@ I
@ I
@ I
@ @
3 1
16.751
0.8561
0.8561
22
1 74
.1 @ I
@ I
@ I
@ I
@ I
@ @
3 1
17.251
0.8821
0.8821
22
1 74
1 @ I
@ I
@ I
@ I
@ I
@ @
3 1
17.751
0.9081
0.9081
22
1 74
1 @ I
- @ I
@ I
@ I
@ I
@ @-
3 1
18.251
0.9341
0.9341
22
1 74
1 @ I
@ I
@ I
@ I
@ I
@ @
4 1
-1 - 8.751
0.9611
0.9611
18
1 63
1 @ I
@ I
@ I
@ I
@ I
@ @
4:1
19.251
0.9871
0.9871
18
1 63
1 @ I
@ I
@ I
@ I
@ I
@ @
4 1
19.751
1,0131
1.0131
18
1 63
1 @ I
@ I
@ I
@ I
@ I
@ @
4 ;,J'�0.251
1.03'91
1.0321
18
1 63
10.9951
17.9 1
0.21310.9571
0.2901
0.74
4 1
20.751
1.0661
1.0421
18
1 63
10.9951
17.9 1
0.21310.9551
0.2931
0.73
4 1
21.251
1.0921
.1.0531
18
1 63
10.9951
17.9 1
0.21310.9541
0.2971
0.72
4 1
21.751
1.1181
1.0641
18
1 63
10.9951
17.9 1
0.21310.9521
0.3011
0.71
4 1
22.251
1.1441
1.0741
18
1 63
10.9951
17.9 1
0.21310.9511
0.3041
0.70
4 1
22.751
1.1711
1.0851
18
1 63
10.9951
17.9 1
0.21210.9491
0.3081
0.69
-----------------------------
Seed and Others (1985] Method PAGE
-----------------------------
I CALC.1
TOTALI
EFF. IFIELD lEst.D I
I
CORR.ILIQUE.1
JINDUC.ILIQUE.
SOILI
DEPTHISTRESSISTRESSI
N I
rl
C I(Nl)601STRESSI
r ISTRESSISAFETY
NO.
I (f t) I
(tsf) I
(tsf) I (B/f t) I
I
N l(B/ft)l
RATIOJ
d I
RATIOIFACTOR
--------------------------------------------------------------------------------
4
1 23.251
1.1971
1.0961
18 1
63
10.9951
17.9
1 0.21210.9471
0.3111 0.68
4
1'23.751
1.2231
1.1061
18 1
63
10.9951
17.9
1 0.21210.9461
0.3141 0.68
4
1 24.251
1.2491
1.1171
18 1
63
10.9951
17.9
1 0.21210.9441
0.3171 0.67
5
1 .24.751
1.2761
1.1271
46 1
98
10.9541
43.9
lInfin
10.9431
0.320IInfin
5
1 25.251
1.3021
1.1381
46 1
98
10.9541
43.9
lInfin
10.9411
0.32311nfin
5
1 25.751
1.3281
1.1491
46 1
98
10.9541
43.9
lInfin
10.9391
0.32611nfin
5
1 26.251
1.3541
1.1591
46 1
98
10.9541
43.9
lInfin
10.9371
0.32911nfin
5
1 26.751
1.3811
1.1701
46 1
.98
10.9541
43.9
lInfin
10.9341
0.331IInfin
5
1 27.251
1.4071
1.1811
46 1
98
10.9541
43.9
lInfin
10.9321
0.33411nfin
5
1 27.751
1.4331
1.1911
46 1
98
10.9541
43.9
lInfin
10.9301
0.33611nfin
5
1 28.251
1.4591
1.2021
46 1
98
10.9541
43.9
lInfin
10.9281
0.338IInfin
5
1 28.751
1.4861
1.2131
46 1
98
10.9541
43.9
lInfin
10.9261
0.341IInfin
5
1 29.251
1.5121
1.2231
46 1
98
10.9541
43.9
lInfin
10.9231
0.34311nfin
6
1 29.751
1.5381
1.2341
54 1
104
10.9161
49.5
lInfin
10.9211
0.34511nfin
6
1 30.251
1.5641
1.2451
54 1
104
10.9161
49.5
[Infin
10.9191
0.347[Infin
6
1 30.751
1.5911
1.2551
54 1
104
10.9161
49.5
lInfin
10.9161
0.34911nfin
6
1 31.251
1.6171
1.2661
54 1
104
10.9161
49.5
lInfin
10.9131
0.350IInfin
6
1.31.751
1.6431
1.2771
54 1
104
10.9161
49.5
lInfin
10.9101
0.35211nfin
6
1.32.251
1.6691
1.2871
54 1
104
10.9161
49.5
lInfin
10.9071
0.35311nfin
6
1-32.751
1.6961
1.2981
54 1
104
10.9161
49.5
[Infin
10.9041
0.35511nfin
6
1 33.251
1.7221
1.3091
54 1
104
10.9161
49.5
lInfin
10.9021
0.35611nfin
6
1 33.751
1.7481
1.3191
54 1
104
10.9161
49.5
lInfin
10.8991
0.35811nfin
6
1 34.251
1.7741
1.3301
54 1
104
10.9161
49.5
lInfin
10.8961
0.35911nfin
7
1 34.751
1.8011
1.3401
28 1
73
10.8881
24.9
lInfin
10.8931
0.360IInfin
7
1 35.251
1.8271
1.3511
28 1
73
10.8881
24.9
lInfin
10.8901
0.361IInfin
7
1 35.751
1.8531
1.3621
28 1
73
10.8881
24.9
lInfin
10.8861
0.36211nfin
7
1 36.251
1.8791
1.3721
28 1
73
10.8881
24.9
lInfin
10.8821
0.36311nfin
7
1 36.751
1.9061
1.3831
28 1
73
10.8881
24.9
lInfin
10.8781
0.36311nfin
7
1 37.251
1.9321
1.3941
28 1
73
10.8881
24.9
lInfin
10.8741
0.36411nfin
8
1 37.751
1.9581
1.4041
69 1
11i
10.8611
59.4
lInfin
10.8701
0.36411nfin
8
1 38.251
1.9841
1.4151
69 1
113
10.8611
59.4
lInfin
10.8661
0.36511nfin
8
1 38.751
2.0111
1.4261
69 1
113
10.8611
59.4
lInfin
10.8621
0.36511nfin
8
1 39.251
2.0371
1.4361
69 1
113
10.8611
59.4
lInfin
10.8581.0.366IInfin
8
1 39.751
2.0631
1.4471
69 1
113
10.8611
59.4
lInfin
10.8551
0.36611nfin
8
1 40.251
2.0891
1.4581
69 1
113
10.8611
59.4
lInfin
10.8501
0.36611nfin
8
1 40.751
2.1161
1.4681
69 1
113 '10.8611
59.4
lInfin
10.8451
0.36611nfin
8
1 41.251
2.1421
1.4791
69 1
113
10.8611
59.4
lInfin
10.8401
0.36611nfin
8
1 41.751
2.1681
1.4901
69 1
113
10.8611
59.4
lInfin
10.8361
0.36511nfin
8
1 42.251
2.1941
1.5001
69 1
113
10.8611
59.4
lInfin
10.8311
0.36511nfin
8
1,42.751
2.2:�lj
1.5111
69 1
113
10.8611
59.4
lInfin
10.8261
0.36511nfin
8:
1 �3.251
2.2471
1.5221
69 1
113
10.8611
59.4
lInfin
10.8211
0.36411nfin
8
1 43.751
2 ' .2731
1.5321
69 1
113
10.8611
59.4
lInfin
10.8161
0.36411nfin
8' -Il
. 44.251
2.2§91
1.5431
69 1
113
10.8611
59.4
lInfin
10.8111
0.36311nfin
9
1 44.751
2.3261
1.5531
33 1
77
10.8361
27.6
lInfin
10.8061
0.36311nfin
9
1 45.251
2.3521
1.5641
33 1
77
10.8361
27.6
lInfin
10.8011
0.36211nfin
9
1 45.751
2.3781
1.5751
33 1
77
10.8361
27.6
lInfin
10.7961
0.36111nfin
9
1 46.251
2.4041
1.5851
33 1
77
10.8361
27.6
lInfin
10.7911
0.360IInfin
9
1 46.751-2.4311
1.5961
33 1
77
10.8361
27.6
lInfin
10.7861
0.360IInfin
9
-------------------------------------------------------------------------------
1 47.251
2.4571
1.6071
33 1
77
10.8361
27.6
lInfin
10.7811
0.35911nfin
L I Q U E F Y 2
Version 1.20
EMPIRICAL PREDICTION OF
EARTHQUAKE -INDUCED LIQUEFACTION POTENTIAL
JOB NUMBER: 00-1562 DATE: Thursday, February 3, 2000
JOB NAME: LA QUINTA
LIQUEFACTION CALCULATION NAME: LA QUINTA LIQUEFACTION STUDY
SOIL -PROFILE NAME: SANGERL
GROUND WATER DEPTH: 40.0 ft
DESIGN EARTHQUAKE MAGNITUDE: 7.00
SITE PEAK GROUND ACCELERATION: 0.462 g
K sigma'BOUND: M
rd BOUND: M
N60 CORRECTION: 1.00
FIELDSPT N -VALUES < 10 FT DEEP ARE CORRECTED FOR SHORT LENGTH OF DRIVE
RODS
NOTE: ..Relative density values listed below are estimated using equations
of
Giuliaiii,and Nicoll (1982).
-----------------------------
LIQUEFACTION ANALYSIS SUMMARY
-----------------------------
-----------------------------
Seed and Others (19851 Method
-----------------------------
PAGE
I
CALC.]
TOTALI
EFF. IFIELD
lEst.D I
I CORR.ILIQUE.]
JINDUC.JLIQUE.
SOILI
DEPTHISTRESSISTRESS1
N
I rl
C
I(Nl)60]STRESSI
r
ISTRESSISAFETY
NO. I
(f t) I
(tsf) I
(tsf) I (B/f
t)
I I
N
l(B/ft)l
RATIO1
d
I RATIOIFACTOR
-------------------------------------------------------------------------------
1 1
0.251
0.0131
0.0131
14
1 71 1
@
I @ I
@ I
@
I @
I @
@
1 1
0.751
0.0381
0.0381
14
1 71 1
@
I @ I
@ I
@
I @
I @
@
1 1
1.251
0.0631
0.0631
14
1 71 1
@
I @ I
@ I
@
I @
I @
@
1 1
1.751
0.0881
0.0881
14
1 71 1
@
I @ I
@ I
@
I @
I @
@
1 1
2.251
0.1131
0.1131
14
1 71 1
@
I @ I
@ I
@
I @
I @
@
1 1
2.751
0.1381
0.1381
14
1 71 1
@
I @ I
@ I
@
I @
I @
@
1 1
3.251
0.1631
0.1631
14
1 71 1
@
I @ I
@ I
@
I @
I @
@
1 1
3.751
0.1881
0.1881
14
1 71 1
@
I @ I
@ I
@
I @
I @
@
1 1
4.251
0,2131
0.2131
14
1 71 1
@
I @ I
@ I
@
I @
I @
@
1 1
4.751
0.2381
0.2381
14
1 71 1
@
I @ I
@ I
@
I @
I @
@
1 1
5.251
0.2631
0.2631
14
1 71 1
@
I @ I
@ I
@
I @
I @
@
1 1
5.751
0.2881
0.2881
14
1 71 1
@
I @ I
@ I
@
I @
I @
@
1 1
6.251
0.3131
0.3131
14
1 71 1
@
I @ I
@ I
@
I @
I @
@
1 1
6.751
0.3381
0.3381
14
1 71 1
@
1 4 1
@ I
@
I @
I @
@
1 1
7.251
0.3631
0.3631
14
1 71 1
@
I @ I
@ I
@
I @
I @
@
1 1
7.751
0.3881
0.3881
14
1 71 1
@
I @ I
@ I
@
I @
I @
@
1 1
8.251
0.4131
0.4131
14
1 71 1
@
I @ I
@ I
@
I @
I @
@
1 1
8. 751
0.4381
0.4381
14
1 71 1
@
I @ I
@ I
@
I @
I @
@
1 1
9.251
0.4631
0.4631
14
1 71 1
@
I @ I
@ I
@
I @
I @
@
2 1
9.751
0.4881
0.4881
15
1 66 1
@
I @ I
@ I
@
I @
I @
@
2 1
10.251
0.5141
0.5141
15
1 66 1
@
I @ I
@ I
@
I @
I @
@
2 1
10.751
0.5411
0.5411
15
1 66 1
@
I @ I
@ I
@
I @
I @
@
2 1
11.251
0.5671
0.5671
15
1 66 1
@
I @ I
@ I
@
I @
I @
@
2 1
11.751
0.5931
0.5931
15
1 66 1
@
I @ I
@ I
@
I @
I @
@
2 1
12.251
0.6191
0.6191
15
1 66 1
@
I @ I
@ I
@
I @
I @
@
2 1
12.751
0.6461
0.6461
15
1 66 1
@
I @ I
@ I
@
I @
I @
@
2 1
13.251
0.6721
0.6721
15
1 66 1
@
I @ I
@ I
@
I @
I @
@
2 1
13.751
0.6981
0.6981
15
1 66 1
@
I @ I
@ I
@
I @
I @
@
2 1
14.251
0.7241
0.7241
15
1 66 1
@
I @ I
@ I
@
I @
I @
@
3 1
14.751
0.7511
0.7511
22
1 74 1
@
I @ I
@ I
@
I @
I' @
@
3 1
15.251
0.7771
0.7771
22
1 74 1
@
I @ I
@ I
@
I @
I @
@
3 1
15.751
0.8031
0.8031
22
1 74 '1
@
I @ I
@ I
@
I @
I @
@
3 1
16.251
0.8291
0.8291
22
1 74 1
@
I @ I
@ I
@
I @
I @
@
3 1
16.751
0.8561
0.8561
22
1 74 1
@
I @ I
@ I
@
I @
I @
@-
3 1
17.251
0.882,1
0.8821
22
1 74 1
@
I @ I
@ I
@
I @
I @
@
3 1
1.7.751
0.90811
0.9081
22
1 74 1
@
I @ I
@ I
@
I @
I @
@
3 :1
18.251
0.9341
0.9341
22
1 74 1
@
I @ I
@ I
@
I @
I @
@
4 1
18.751
0.9611
0.9611
18
1 63 1
@
I @ I
@ I
@
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I @
@
4 1
'i9.251
0.98)1
0.9871
18
1 63 1
@
I @ I
@ I
@
1 6
1 @
@
4 1
19.751
1.0131
1.0131
18
1 63 1
@
I @ I
@ I
@
I @
I @
@
4 1
20.251
1.0391
1.0391
18
1 63 1
@
I @ I
@ I
@
I @
I @
@
4 1
20,.751
1.0661
1.0661
18
1 63 1
@
I @ I
@ I
@
I @
I @
@
4 1
21.251
1.0921
1.0921
18
1 63 1
@
I @ I
@ I
@
I @
I @
@
4 1
21.751
'1.1181
1.1181
18
1 63 1
@
I @ I
@ I
@
I @
I @
@
4 1
22.251
1.1441
1.1441
18
1 63 1
@
I @ I
@ I
@
I @
I @
@
4 1
22.751
1.1711
1.1711
18
1 63 1
@
I @ 1
0 1
@
I @
1 0
@
Seed and Other3 (1985) Method PAGE
-----------------------------
I CALC.1
TOTALI
EFF. IFIELD
lEst.D I
I
CORR.ILIQUE.1
JINDUC.ILIQUE.
SOILI DEPTHISTRESSISTRESSI
N
I rl
C I(NI)601STRESSI
r ISTRESSISAFETY
NO.1
(ft) I
(tsf)l
(t3f)I(B/ft)
I I
N l(B/ft)l
RATIOI
d I
RATIOIFACTOR
-------------------------------------------------------------------------------
4
1 23.251
1.1971
1.1971
18
1 63
1 @ I
@
I @
I @ I
@ I @ @
4
1 23.751
1.2231
1.2231
18
1 63
1 @ I
@
I @
I @ I
@ I @ @
4
1 24.251
1.2491
1.2491
18
1 63
1 @ I
@
I @
I @ I
@ I @ @
5
1 24.751
1.2761
1.2761
46
1 95
1 @ I
@
I @
I @ I
@ I @ @
5
1 25.251
1.3021
1.3021
46
1 95
1 @ I
@
I @
I @ I
@ I @ @
5
1 25.751
1.3281
1.3281
46
1 95
1 @ I
@
I @
I @ I
@ I @ @
5
1 26.251
1.3541
1.3541
46
1 95
1 @ I
@
I @
I @ I
@ I @ @
5
1 26.751
1.3811
1.3811
46
1 .95
1 @ I
@
I @
I @ I
@ I @ @
5
1 27.251
1.4071
1.4071
46
1 95
1 @ I
@
I @
I @ I
@ I @ @
5
1 27.751
1.4331
1.4331
46
1 95
1 @ I
@
I @
I @ I
@ I @ @
5
1 28.251
1.4591
1.4591
46
1 95
1 @ I
@
I @
I @ I
@ I @ @
5
1 28.751
1.4861
1.4861
46
1 95
1 @ I
@
I @
I @ I
@ I @ @
5
1 29.251
1.5121
1.5121
46
1 95
1 @ I
@
I @
I @ I
@ I @ @
6
1 29.751
1.5381
1.5381
54
1 98
1 @ I
@
I @
I @ I
@ I @ @
6
1 30.251
1.5641
1.5641
54
1 98
1 @ I
@
I @
I @ I
@ I @ @
6
1 30.751
1.5911
1.5911
54
1 98
1 @ I
@
I @
I @ I
@ I @ @
6
1 31.251
1.6171
1.6171
54
1 98
1 @ I
@
I @
I @ I
@ I @ @
6
1.31.751
1.6431
1.6431
54
1 98
1 @ I
@
I @
I @ I
@ I @ @
6
1.32.251
1.6691
1.6691
54
1 98
1 @ I
@
I @
I @ I
@ I @ @
6
1,32.751
1.6961
1.6961
54
1 98
1 @ I
@
I @
I @ I
@ I @ @
6
1 33.251
1.7221
1.7221
54
1 98
1 @ I
@
I @
I @ I
@ I @ @
6
1 33.751
1.7481
1.7481
54
1 98
1 @ I
@
I @
I @ I
@ I @ @
6
1 34.251
1.7741
1.7741
54
1 98
1 @ I
@
I @
I @ I
@ I @ @
7
1 34.751
1.8011
1.8011
28
1 68
1 @ I
@
I @
I @ I
@ I @ @
7
1 35.251
1.8271
1.8271
28
1 68
1 @ I
@
I @
I @ I
@ I @ @
7
1 35.751
1.8531
1.8531
28
1 68
1 @ I
@
I @
I @ I
@ I @ @
7
1 36.251
1.8791
1.8791
28
1 68
1 @ I
@
I @
I @ I
@ I @ @
7
1 36.751
1.9061
1.9061
28
1 68
1 @ I
@
I @
I @ I
@ I @ @
7
1 37.251
1.9321
1.9321
28
1 68
1 @ I
@
I @
I @ I
@ I @ @
8
1 37.751
1.9581
1.9581
69
1 102
1 @ I
@
I @
I @ I
@ I @ @
8
1 38.251
1.9841
1.9841
69
1 102
1 @ I
@
I @
I @ I
@ I @ @
8
1 38.751
2.0111
2.0111
69
1 102
1 @ I
@
I @
I @ I
@ I @ @
8
1 39.251
2.0371
2.0371
69
1 102
1 @ I
@
I @
I @ I
@ I @ @
8
1 39.751
2.0631
2.0631
69
1 102
1 @ I
@
I @
I @ I
@ r @ @
8
1 40.251
2.0891
2.0821
69
1 102
10.7331
50.6
lInfin
10.8501
0.25611nfin
8
1 40.751
2.1161
2.0921
69
1 102 .10.7331
50.6
lInfin
10.8451
0.25711nfin
8
1 41.251
2.1421
2.1031
69
1 102
10.7331
50.6
lInfin
10.8401
0.25711nfin
8
1 41.751
2.1681
2.1141
69
1 102
10.7331
50.6
lInfin
10.8361
0.25711nfin
8
1 42.251
2.1941
2.1241
69
1 102
10.7331
50.6
[Infin
10.8311
0.258IInfin
8
1 -4.2.751
2.22il
2.1351
69
1 102
10.7331
50.6
lInfin
10.8261
0.258IInfin
8:
1 43.251
2.2471
2.1461
69
1 102
10.7331
50.6
lInfin
10.8211
0.258IInfin
8
1".43.751
2.2731
2.1561
69
1 102
10.7331
50.6
lInfin
10.8161
0.258IInfin
811
'44.251
2.29;91
2.1671
69
1 102
10.7331
50.6
lInfin
10.8111
0.25911nfin
9
1 44.751
2.3261
2.1771
33
1 70
10.7151
23.6
lInfin
10.8061
0.25911nfin
9
1 45.251
2.3521
2.1881
33
1 70
10.7151
23.6
lInfin
10.8011
0.25911nfin
9
1 45.751
2.3781
2.1991
33
1 70
10.7151
23.6
lInfin
10.7961
0.25911nfin
9
1 46.251
2.4041
2.2091
33
1 70
10.7151
23.6
lInfin
10.7911
0.25911nfin
9
1 46.751-2.4311
2.2201
33
1 70
10.7151
23.6
lInfin
10.7861
0.258IInfin
9
-------------------------------------------------------------------------------
1 47.251
2.4571
2.2311
33
1 70
10.7151
23.6
lInfin
10.7811
0.258[Infin
SOIL PROFILE LOG
- - - - - - - - - - - - - - - - - - - - - - - -
S'OTL-PROFILE NAME: SANGERL
---------------------------
LAYtR
BASE DEPTH
SPT FIELD -N
LIQUEFACTION
WET UNIT
FINES
D (mm)
DEPTH OF
# I
(ft)
(blows/ft)
SUSCEPTIBILITY
WT. (pcf)
%<#200
50
SPT (ft)
-----
1
----------
4.0
-----------
50.0
-----------------
UNSUSCEPTIBLE (0)
---------
133.0
------
26.0
------
0.080
--------
2.25
-----
2.
----------
9.0
-----------
26.0
-----------------
UNSUSCEPTIBLE (0)
---------
104.0
------
26.0
------
0.080
--------
5.25
--
3
----------
14.5
-----------
40.0
-----------------
UNSUSCEPTIBLE (0)
---------
122.0
------
10.0
------
0.110
--------
12.25
-----
4
----------
20.0
-----------
29.0
-----------------
SUSCEPTIBLE (1)
---------
114.0
------
27.0
------
0.085
--------
15.25
-----
5�
------
----------
25.0
----------
-----------
20.0
--------- -
-----------------
SUSCEPTIBLE (1)
-----------------
---------
118.0
---------
------
58.0
------
------
0.048
------
--------
20.25
--------
.6
310.0
7
20.0
SUSCEPTIBLE (1)
131.0
33.0
0.120
25.25
7
7
7 -
34.0 :
-----------
25.0
-----------------
SUSCEPTIBLE (1)
7 --------
118.0
------
87.0
------
0.003
--------
'30.25
-----
�8
----------
39. 0
-----------
39.0
-----------------
SUSCEPTIBLE (1)
---------
138.0
------
48.0
------
0.080
--------
35.25
-----
.9
----------
44.0
-----------
27.0
-----------------
SUSCEPTIBLE (1)
---------
119.0
------
27.0
------
0.090
--------
40.25
7 - - -
10.
-------------------------------------------------------------------------------
- - - - - - - - - -
51.5
----------
- - - - - - - - - - -
31.0
-----------
- - - - - - - - - - - - - - - - -
SUSCEPTIBLE (1)
-----------------
- - - - - - - - -
115.0
---------
- - - - - -
19.0
------
- - - - - -
0.095
------
- - - - - - - -
46.25
--------
VICINITY MAP
ANTHONY -TAYLOR CONSULTANTS
C�v C—t 1-
5300 OW �. 66�0560
1:7 7, 71 1
'C' A W19
go, ? 30. ,boo u w 1534
SCALE: NTS JOB NAME:
LA OUINTA
SITE ADDRESS:
W OF HWY 111 AND WASHINGTON ST. LA QUINTA, CA.
JOB NUMBER: I REVIEWED BY: DATC: ��FIG, No.
00-1562 HGE 101/2 XOO la
SITE MAP
(A
z
u
(A
B-3
B-1 PAD 3 B-2
6,600 SO FT
LEGEND
ANTI-IONY-TAYLOR CONSULTANTS
APPROXIMATE LOCATION OF
Z�m
-1 ;s -Dell.
.,c, 92029 U. 04105
176010 38-8600
V C.-4 A—
530co,w,.�. 1... 540
TR 7�1001
Ml .6, 35 6
B-3 EXPLORATORY BORING
JOB NAME:
LA QUINTA
SITE ADDRESS:
W OF HWY 111 AND WASHINGTON ST. LA
QUINTA, CA.
JOB NUMBER:
00-1562
I REVIEWED BY:
HGE
I DATE: 8/001
01/2
FIG. NO.
lb
49mmuw=4 4
EXCAVATION LOG
EQUIPMENT:
DIMENSION & TYPE OF EXCAVATION:
DATE LOGGED:
HOLLOW STEM AUGER DRILL RIC
6" DIAMETER AUGER BORING
01120100
SURFACE ELEVATION:
GROUNDWATER DEPTH:
LOG ED BY:
GR
BORING No:
EXISTING ELEVATION
NONE ENCOUNTERED
W
B-1
Li
-i
IZZ
FIELD DESCRIP11ON AND CLASSIFICATION
et
—
tZ 0
M
a-
:E
Uj
-,
a-
Lj �
U w
Lj 0
a.
M
<
0
Z
5 w
5 0'
::1
67,
Q- >-
Lj
0
V)
m Z)
DESCRIPTION AND REMARKS
Vi
CL
I
CL �:
D
>
:1 , _
Z
a
<
m
0
rain size, Density, Moisture, Color)
Ln
Z LA
— 0
I r
Z 'i
— Z
CL
0 Ln
0
x
Z
w
Lj
0 —
7T7
SILTY SANDY CLAY/CLAYEY SAND, STIFF/LOOSE, MOIST.
CIL
BROWN. LANDSCAPE TOPS01 L
'S -C
16
SILTY VERY FINE TO FINE SAND, MEDIUM DENSE, MOIST,
SM
17.7
104.9
9.4
131.0
BROWN TO CRAY BROWN.
61
BECOMES.DENSE.
7.9
120.8
5
24
SLIGHTLY SILTY TO SILTY, VERY FINE TO FINE SAND,
SID
MEDIUM DENSE, MOIST, LIGHT GRAY BROWN.
10
55
BECOMES DENSE.
7.8
100.7
15 -
12
SILTY, FINE TO MEDIUM SAND, LOOSE, MOIST, LIGHT GRAY,
BROWN.
ALLUVIUM
10.5,
20-
TOTAL DEPTH 6.5 FT.
NO GROUNDWATER ENCOUNTERED
NO CAVING
BORING BACKFILLED: 01/20/00
25 -
VALUE AS PER SIMILAR SOIL TYPE
WATER TABLE
ANTHONY -TAYLOR CONSULTANTS
LOOSE BAG SAMPLE
10A
SPT SAMPLE
JOB NAME:
-LA QUINTA
DRIVE SAMPLE
NO SAMPLE RECOVERY
SITE ADDRESS:
DISTURBED SAMPLE
W OF HWY I 11 AND WASHINGTON ST. LA QUINTAI CA.
# DISTURBED BLOWCOUNT No.
JOB NUMBER:
I REVIEWED BY:
DATE:
FIG. NO.
.1,
00- 1562
1 HGE I
01/28/001
Ila
EXCAVATION LOG
EQUIPMENT:
DIMENSION & TYPE OF EXCAVATION:
DATE LOGGED:
HOLLOW STEM AUGER DRILL RIC
6" DIAMETER AUGER BORING
01/20/00
-SURFACE ELEVATION:
GROUNDWATER DEPTH:
LOGGED BY:
BORING No:
-EXISTING ELEVATION
NONE ENCOUNTERED
RW
B-2
'"W411"
_j
RELD DESCRIP71ON AND CLASSIFICATION
X
-U
0
LA.
_j
0
a-
2
Uj
_j
(L
V)
L) L'
U
M LJ
X
M
:)
CL
m
:1
4
V)
:2
<
0
_j Z
m D
DESCRIPTION AND REMARKS
6
CL D
1 ,,
0-
I
D
0- �-_
V)
m >-
t:
;7< v)
0M
Z -
0
LA
0
V)
0
U
(Grain size, Density, Moisture, Color)
7
Z
0
Z
m
0—
7. .1
SILTY SANDY CLAY, CLAYEY SAND, STIFF/LOOSE, MOIST,
SC
BROWN.
LANDSCAPE TOPSOIL
CL
SILTY FINE TO VERY FINE SAND, MEDIUM DENSE, VERY
Sm
12.1
118.6
50
MOIST, BROWN TO OLIVE BROWN.
12.6
122.0
SLIGHTLY SILTY TO SILTY, FINE SAND, MEDIUM DENSE,
S P
5
DAMP TO MOIST, BROWN -TO OLIVE BROWN AND GRAY.
�_M
27
25
6.8
96.7
10
40
12.7
108.1
WATER SEEP, PERCHED VWER. -
15
SLIGHTLY SILTY, FINE SAND, MEDIUM DENSE, MOIST, LIGHT
SP
29
GRAY—BROWN.
5.1
20-
20
SILTY FINE SAND, MEDIUM DENSE, MOIST, LIGHT
SM
8.1
j
GRAY—BROWN.
I
2 5
20
SLIGHTLY CLAYEY FINE SANDY SILT, VERY MOIST, BROWN
M L
20.6
—
. .
X.
TO LIGHT GRAY —bROWN.
VALUE AS PER SIMILAR SOIL TYPE
ANTFIONY-TAYLOR CONSULTANTS
Y WATER TABLE
,- -, —1, - - --on.,
11 :7:! . . . . 6.1 47:.' A. .. 32's 1. '"
LOOSE BAG SAMPLE
. '.. I... . . ).(!=
.=.,C. W. C. ud.3 CA .415W L..
1.41
SPT SAMPLE
JOB NAME:
DRIVE SAMPLE
LA QUINTA
SITE ADDRESS:
W OF HWY 111 AND WASHINGTON ST. LA QUINTA, CA.
NO SAMPLE RECOVERY
DISTURBED SAMPLE
JOB NUMBER:
I REVIEWED BY:
I DATE:
FIG. NO.
11b
# DISTUR-BED BLOWCOUNT No.
00-1562
HGE
01/2 8/001
'"W411"
EXCAVATION LOG
EOUIPMENT:
DIMENSION & TYPE OF EXCAVATION:
DATE LOGGED:
.HOLLOW STEM AUGER DRILL RIG
6" DIAMETER AUGER BORING
01120100
SURFACE ELEVATION:
GROUNDWATER DEPTH:
LOGGED BY:
BORING No:
EXISTING ELEVATION
NONE ENCOUNTERED
RW
B-2 CON7
)
Uj
ANTHONY -TAYLOR CONSULTANTS
y
FiELD DESCRIPTION AND CLASSIFICATION
X
_U
SPT SAMPLE'
JOB NAME:
LA. _j
0
_j
LU
_j
N11
NO SAMPLE RECOVERY
DISTURBED SAMPLE
DISTURBED BLOWCOUNT No.
1
Uj
U LU
LU
q Q.
—
I DATE: 0
01/28/0
1 FIG. NO, 11b'
vi
V)
a-
m
3: V)
0
j Z
a:
CL =1
(L
W :2
Z
CL >_
Uj Ln
V)
M
DESCRIPTION AND REMARKS
6
Z'i
Uj
0
0
U
(Grain size, Density, Moisture, Color)
vi
Z'
—0
Z
0 0
Z
30—
25
SILTY FINE SAND, MEDIUM DENSE, MOIST, BROWN TO
Sm
9.0
OLIVE BROWN AND CRAY.
FINE SANDY, CLAYEY SILT, HARD, VERY MOIST TO WET,
ML
35
LIGHt BROWN.
IYK
�v
39
27.1
S I LTY, VERY FINE TO FINE SAND, MEDIUM DENSE, VERY
M
4 0
MOIST, BROWN TO OLIVE—BROWN AND GRAY.
27
9.9
.4 .,::1
BECOMES DENSE.
4 5
32
6.9
SLIGHTLY SILTY FINE SAND, MOIST, LIGHT GRAY —BROWN
TO BROWN.
50
30
ALLUVI um
6.6
55—
TOTAL DEPTH 51.5 FT.
NO GROUNDWATER ENCOUNTERED
NO CAVING
BORING BACKFILLED: 01/20/00
)
VALUE AS PER SIMILAR SOIL TYPE
ANTHONY -TAYLOR CONSULTANTS
y
WATER TABLE
LOOSE BAG SAMPLE
Is — I I=:T:!. —
" "o' CA 64.�
SPT SAMPLE'
JOB NAME:
DRIVE SAMPLE
LA QUINTA
SITE ADDRESS:
W OF HWY 111 AND WASHINGTON ST. LA QUINTA, CA.
#
NO SAMPLE RECOVERY
DISTURBED SAMPLE
DISTURBED BLOWCOUNT No.
1
JOB NUMBER:
00-1562
I REVIEWED BY:
HGE
I DATE: 0
01/28/0
1 FIG. NO, 11b'
ammmaSu'l
EXCAVATION LOG
EOUIPMENT:
FIELD DESCRIPrI7ION A ND CLASSIFICATION
DIMENSION & TYPE OF EXCAVATION:
DATE LOGGED:
FIOLLOW STEM AUGER DRILL
RIC
6" DIAMETER AUGER BORING
01/20/00
SURFACE ELEVATION:
GROUNDWATER DEPTH:
LOGGED BY:
BORING No:
EXISTING ELEVATION
NONE ENCOUNTERED
RW
B-3
tZ
FIELD DESCRIPrI7ION A ND CLASSIFICATION
0
Uj
3: Ln
U Lj
X m
0
01—
Z
M D
DESCRIPTION AND REMARKS
"n
:E
Z
Ln
L)
<
(A
0
U
(Grain size, Density, Moisture, Color)
vi
F5
Z
Lj
0
05
x
< Z
w
0
m
0
0—
SILTY SANDY CLAY/CLAYEY SAND, STIFF/LOOSE, MOIST,
CL
BROWN.
LANDSCAPE TOPSOIL
42
SILTY VERY FINE TO FINE SAND, MEDIUM DENSE, MOIST,
Sm
BROWN TO GRAY BROWN.
26
5
SLIGHTLY SILTY FINE TO VERY FINE SAND, MEDIUM DENSE,
SP
DAMP, BROWN.
25
10 —
SILTY VERY FINE SAND, MEDIUM DENSE, MOIST, BROWN.
Sm
20
j
1, :1:.1: T:1
S P
J:
15 1.:�: 1. :
12
ALLUVIUM
20—
TOTAL DEPTH 16.5 FT.
-
NO GROUNDWATER ENCOUNTERED
NO CAVING
BORING BACKFILLED: 01/20/00
25—
VALUE AS PER SIMILAR SOIL TYPE
EM ANTHONY -TAYLOR CONSULTANTS
WATER TABLE
LOOSE BAG SAMPLE
loll
SPT SAMPLE
JOB NAME:
DRIVE SAMPLE
LA QUINTA
SITE ADDRESS:
W OF HWY 111 AND WASHINGTON ST. LA QUINTA, CA.
NO SAMPLE RECOVERY
DISTURBED SAMPLE
JOB NUMBER:
REVIEWED BY:
DATE:
FIG. NO.
# DISTURBED BLOWCOUNT No.
00-1562
I HGE
01/28/00
11c
I
. I LABORATORY SOIL DATA SUMMARY
I ISO
140
130
irce
ifEl
owe
nn
0
10 20 30 40
UBLE SULFATE IN SOIL (%)
JE
SULFATE CEMENT
I
EXPOSURE TYPE
5
NEGLIGIBLE 2
'XPANSION TEST
DATA
TYPE
1_ 2
RY DENSITY (pcf)
116.6
ATER CONTENT
8.4
f)
144
SWELL
1.5
SPECIFIC GRAVITY
ZERO AIR VOIDS CURVES.
SOIL
BORING
TRENCH
SOIL CLASSIFICATION
SOIL CLASSIFICATION
TYPE
NO
NO
1
BROWN, SLI ' GHTLY SILTY TO SILTY,
B-1
x
2.0 TO 4.0 FT
VERY FINE TO MEDIUM SAND.
2
GRAY, BROWN, SILTY VERY FINE TO
B-2
x
3.0 TO 7.0 FT
FINE SAND.
3
ANTI-IONY-TAYLOR CONSUIJANTS
A
Dug. (C—p—t-) S 3300 Y.C.
E.".' '. 315 V.. .'.. 250 11;60 5.0
920 s— N.W.— C. 91.05
'36.
17601 swo 1"31 061.3556
JOB NAME:
LA QUINTA
SITE ADDRESS:
W OF HWY 111 AND WASHINGTON ST. LA QUINTA, CA.
JOB NUMBER: REVIEWED BY: DA� FIG. NO.
00— 1562 HGE 101 28/00 ilia
7777=
DIRECT SHEAR TEST RESULTS
3000
1-1�
LL- 2000
(A
11-
Lij
Of
ry
Ld
—17
(A 1000
0
0 .577 1000 1154 1731 2000 2308
NORMAL PRESSURE (PSF)
3000
SYMBOL
SAMPLE LOCATION
COHESION (psf)
FRICTION
ANGLE (a)
REMARKS
0
8— 1 @ 2.0 TO 4.0 FT
255
32
REMOLDED @ 90% R:C.
SITE ADDRESS:
W OF HWY 111 AND WASHINGTON ST. LA QUINTA, CA.
Psamr=
ANTHONY -TAYLOR CONSULTANTS
S r— - C.V C —1 A-
30 . ..... F'.. �, $I.. ".. 150 �30 ". 560
3" — . 0
(59-1d . CA 9202 no.cisco. ca. 94io fx I? of
17601' 738. adoo M31 06,3536
JOB NAME:
LA QUINTA
SITE ADDRESS:
W OF HWY 111 AND WASHINGTON ST. LA QUINTA, CA.
JOB NumeER:
I REVIEWED Ely:
DAT�
1
FIG. NO.
111b
00-1562
HGE
28/001
Psamr=
3C
1-1%
LL- 2000
V)
CL
z
LLJ
V)
LLJ
—F
Lf) 1000
I
'01
DIRECT SHEARTEST RESULTS
0 577 '1000 1154 1731 2000 2308
NORMAL PRESSURE (PSF)
3000
i
SYMBOL
SAMPLE LOCATION
COHESION (psf)
FRICTION
ANGLE
REMARKS
0
Ef-3 @ 8.5 FT
190
33'
NATURAL FIELD SHEARS
SITE ADDRESS:
W OF HWY I I I AND WASHINGTON ST. LA QU NTA, CA.
JOB NUMBER:
00-1-562
PWMI ANTI-IONY-TAYLOR CONSULTANTS
fcwp—.t.) I", C"v C-1
30 c� —".. 51 ... I _4 s '50 5300 W--..
m
E ... X, CA 92029 S.- "o 01
,60, , 36-OWO
JOB NAME:
LA QUINTA
SITE ADDRESS:
W OF HWY I I I AND WASHINGTON ST. LA QU NTA, CA.
JOB NUMBER:
00-1-562
REVIEWED BY:
HGE
DATE:
101/28/001
FIG. NO. 111c
1
I . CONSOLIDATION - PRESSURE CURVE
PRESSURE
— LBS/SQ
FT
0
0 0 0
.0 0
(D
0
0
0
0 0 0 -t co
(o 0
0
(D 04 0 t co
r- 0
0
04
Lo —
0
2
3
ui
4
uj
0-
5
Z
0
6
-
-
-T
I
<
I
I I
7
0
Ln
F ---- T--
z
III
0
8
H
9
10
ORIGINAL MOISTURE
0 SATURATED
CONSOLIDATION
REBOUND
JOB NAME:
LA QUINTA
ANTHONY -TAYLOR CONSULTANTS
SAMPLE -13-11 a 7.5 Fr.
SITE ADDRESS:
W OF HWY 111 AND
WASHINGTON ST. LA QUINTA, CA.
JOB NUMBER: REVIEWED BY: DA TE: NO.
1 101/28/00 FlIG- lild
00-1562 HGE
I CONSOLIDATION - PRESSURE CURVE
0
2
3
u
of 4
uj
EL
5
0
6
n
7
0
v)
z
0
9
10
4 4
PRESSURE - LBS/SQ FT C)
C)
0 0 0- 0 C) 0
0 0 0 0 't 00 (D C) 0
C14 C) It 00 r- C)
r�, — — c"I Lo C3
(j) ORIGINAL MOISTURE SATURATED CONSOLIDATION REBOUND
JOB NAME:
LA QUINTA
ANTHONY -TAYLOR CONSULTANTS SITE ADDRESS:
SAMPLE B-2 6.5 Fr. —�. .., *— —,
E. - . . . . . . . . . W OF HWY 111 AND WASHINGTON ST. LA QUINTA, CA.
,— v —z -1 DATE: F"I G. N 0.
-FREVIEWE
JOB NUMBER: D BY:
00-1562 1 HGE 01/28/001 ille
MECHANICAL ANALYSIS - SIEVE TEST DATA
0
10
20
30
z
40
0: 50
II -
z
w Go
u
IL 70
80
90
100
U.S. STANDARD SIEVE SIZES
50 ao
100 50 10.0 5.0 1.0 0.5 0.1 .05 .01 .005
PARTICLE SIZE IN MILLIMETERS
100
20
so
70
60 0
(A
4
50
z
40 w
0
cz
L.j
30 Q.
20
10
0
.001
U.S. STD. SIEVE
CRAVEL
SAND
#4
0.0
100.0
#8 -
0.0
m
#16
0.0
SILT AND CLAY
#30
0.0
100.0
#50
2.0
m
0
#100
UP
COARSE
FINE
COARSE
MEDIUM
FINE
U.S. STD. SIEVE
MINUS #4
% RET.
SAMPLE
% PASS
#4
0.0
100.0
#8 -
0.0
100.0
#16
0.0
100.0
#30
0.0
100.0
#50
2.0
98.0
#100
30.1
69.9
#200
68.7
31.3
BORING: B-1
PIM ANTHONY -TAYLOR CONSULTANTS
341..c I j—
........ c. lao ........ lool
Ir4ol 734 -moo
DEPTH: 15.0 FT.
JOB NAME:
LA QUINTA
SITE ADDRESS:
WOFHWY 111 AND WASHINGTON ST. LA QUINTA, CA.
JOB NUMBER:
REVIEWED BY:
DATE:
FIG. NO.
00-1562
IHGE
p 1 /28/00
.MECHANICAL ANALYSIS -
SIEVE
TEST DATA
S G.y C. -I 4'..
315 )to I I ...
11 --os
MESA .1601 135-6400
U.S. STANDARD SIEVE SIZES
LA QUINTA
SITE ADDRESS:
7
50 80
4 3 2 I'/l 3/ 1/ 3/ 1/ 4 610 14 20 30 40 60 100 200 325
JOB NUMBER:
REVIEWED BY:
1
DATE:
101/28/001
FIG. No.
lllg
0-
00-1562
2 8
100
io-
90
20-
-so
0
3 -
-70
0
z
0-
-60
W
(A
Li
50-
- 50
CL
z
!-40
z
w
w
Q
60-
u
cc
(r
w
w
(L
70-
30
(L
80-
20
go-
0
100-
100
50 10.0 5.0 1.0 0.5 0.1
.05 .01
.005 .001
PARTICLE SIZE IN MILLIMETERS
GRAVEL
SAND
SILT AND CLAY
0
COARSE
FINE
COARSE
MEDIUM
FINE
MINUS #4
SAMPLE
U.S. STD. SIEVE
% RET.
% PASS
#4
0.0
100.0
#8
0.0
100.0
#16
0.0
100.0
#30
0.0
100.0
#50
1.6
98.4
#100
33,.4
66.6
#200 1
73.7
26.3
am— I- —
BORING: B-2
ANTI-IONY-TAYLOR CONSULTANTS
DEPTH: 9.0 FT.
S G.y C. -I 4'..
315 )to I I ...
11 --os
MESA .1601 135-6400
JOB NAME:
LA QUINTA
SITE ADDRESS:
W OF HWY 111 AND WASHINGTON ST. LA QUI TA, CA.
JOB NUMBER:
REVIEWED BY:
1
DATE:
101/28/001
FIG. No.
lllg
00-1562
BORING: B-2
ANTI-IONY-TAYLOR CONSULTANTS
DEPTH: 9.0 FT.
S G.y C. -I 4'..
315 )to I I ...
11 --os
MESA .1601 135-6400
JOB NAME:
LA QUINTA
SITE ADDRESS:
W OF HWY 111 AND WASHINGTON ST. LA QUI TA, CA.
JOB NUMBER:
REVIEWED BY:
1
DATE:
101/28/001
FIG. No.
lllg
00-1562
HGE
'M'"ECHANICAL ANALYSIS -
SIEVE
TEST DATA
c — — I., I ?w 1 1-1 ...
0",!. --r I
U.S. STANDARD SIEVE SIZES
JOB NAME:
LA QUINTA
7
so ao
4 3 2 1 "2 3/ 1/ 3/ 1/ 4 5110 14 20 30 40 60 100 200 325
W OF HWY 111 AND WASHINGTON ST. LA 01,111 TA, CA.
JOB NUMBER:
0-
4 - -
FIG. NO.
100
HGE
01/28/00
io-
90
20-
80
3
70
ul
c
AD-
v)
Li
cc
5
10
50
CL
z
z
Ld
Li
Go -
-40
Li
L'i
(L
70-
30
(L
so-
20
go-
10
too-
100 50 10.0 5.0 1.0 0.5 0.1
.05 .01
.005 .001
PARTICLE SIZE IN MILLIMETERS
GRAVEL
SAND
SILT
AND CLAY
0
u
COARSE
FINE
COARSE
MEDIUM
FINE
MINUS #4
SAMPLE
U.S. STD. SIEVE
% RET.
% PASS
#4
0.0
100.0
#8
0.0
100.0
#16
0.0
100.0
#30
0.0
100.0
#50
13.8
86.2
#100
69.2
30.8
#200
89.7
10.3
BORING: B-2
ANTHONY -TAYLOR CONSULTANrrs
DEPTH: 16.0 FT.
c — — I., I ?w 1 1-1 ...
0",!. --r I
1,
........ lool
C. 920as T;
JOB NAME:
LA QUINTA
SITE ADDRESS:
W OF HWY 111 AND WASHINGTON ST. LA 01,111 TA, CA.
JOB NUMBER:
REVIEWED BY:
DATE:
FIG. NO.
00-1562
HGE
01/28/00
111h
MECHANICAL A.NALYSIS - SIEVE TEST DATA
0
10
20
0 30
La
z
40
w
so
z
Go
w
(L 70
80
90
100
U.S. STANDARD SIEVE SIZES
so so
loo so 10.0 5.0 1.0 0.5 0.1 .05 01 .005 .001
PARTICLE SIZE IN MILLIMETERS
In
CRAVEL
SANO
#4
co
0
SILT ANO CLAY
-�OARSE
0.0
100.0
#16
0.0
u
#30
TIME
COARSE
MEDIUM
FINE
97.2
U.S. STD. SIEVE
MINUS #4
% RET.
SAMPLE
% PASS
#4
0.0
100.0
#8
0.0
100.0
#16
0.0
100.0
#30
0.0
100.01
#50
2.8
97.2
# 100
32.4
62.6
#200
72.4
27.8
0
(L
z
Li
u
(L
BORING: B-2 ANTIJONY-TAYLOR CONSULTANTS
DEPTH: 21.0 FT. Allf..I.l
313 Mil 0.
It .... . .. C. 02019 fi� 144S ... 1. 11.0 1
11401
JOB NAME:
LA QUINTA
SITE ADDRESS:
W OF HWY 111 AND WASHINGTON ST. LA QUII TA, CA.
JOB NUMBER: I REVIEWED BY: JDAT E 0 1 FIG. N 0.
00-1562 HGE 01/28/0
vascm.1m
MECHANICAL ANALYSIS - SIEVE TEST DATA
0
to
20
30
z
4 40
so
z
UJI 60
u
It. 70
80
90
100
U.S. STANDARD SIEVE SIZES
50 80
too 50 10.0 5.0 1.0 0.5 0.1 .05 .01 .005
PARTICLE SIZE IN MILLIMETERS
100
90
ao
70
60
(L
50
z
40 w
u
(z
61
30 Q.
20
10
0
.001
U.S. STD. SIEVE
CRAVEL
SAND
#4
C3
0
100.0
#8
SILT AND CLAY
100.0
#16
0.4
99.6
#30
u
COARSE
I FINE
C0.7RSE
MEDIUM
I FINE
24.6
U.S. STD. SIEVE
MINUS #4
% RET.
SAMPLE
% PASS
#4
0.0
100.0
#8
0.0
100.0
#16
0.4
99.6
#30
0.7
99.3
#50
4.5
95.5
#100
24.6
75.4
#200
42.1
57.9
BORING: B-2
ANTI-IONY-TAYLOR CONSULTANTS
DEPTH: 26.0 FT.
1, , Cl C. -I A—
0,i ...
E .... 02.21 ...... 100,
11601' 38.6400
JOB NAME:
LA QUINTA
SITE ADDRESS:
W OF HWY 111 AND WASHINGTON ST. LA QUINTA, CA.
JOB NUMBER:
00— 1562
REVIEWED BY:
1 HGE
DA7
101 :28/00
FIG. No.
ilij
w=a6br.zi. I
MECHANICAL ANALYSIS - SIEVE TEST DATA
0
to
20
30
z
40
so
z
w Go
u
0:
w
Q. 70
so
90
100
U.S. STANDARO SIEVE SIZES
50 80
100 50 10.0 5.0 1.0 0.5 0.1 .05 .01 .005
PARTICLE SIZE IN MILLIMETERS
100
90
80
70
60
V)
(L
30
z
40
w
30 Q.
20
10
0
.001
U.S. STD. SIEVE
GRAVEL
SAND
#4
10
0
100.0
#8
SILT AND CLAY
100.0
#16
0.5
99.5
#30
u
COARSE
I FINE
COARSE I
MEDIUM
I FINE
31.4
U.S. STD. SIEVE
MINUS #4
% RET.
SAMPLE
% PASS
#4
0.0
100.0
#8
0.0
100.0
#16
0.5
99.5
#30
0.8
99.2
#50
4.0
96.0
#100
31.4
68.6
#200
1 66.6
33.4
BORING: B-2
ANTI-IONY-TAYLOR CONSULTANTS
DEPTH: 31.0 FT.
'....4f , no
C. 92020
JOB NAME:
LA QUINTA
SITE ADDRESS:
W OF HWY 111 AND WASHINGTON ST. LA QUII TA, CA.
JOB NUMBER:
00-1562
REVIEWED BY:
1 HGE
DATE:
101/28/00
FIG. NO.
1 111k
MECHANICAL ANALYSIS -
SIEVE
TEST
DATA
1.1-W, CA 11019 . .......
116*1
U.S. STANOARO SIEVE SIZES
LA QUINTA
SITE ADDRESS:
7 4
50 so
3 2 1 /2 1 31 1/ 3/ 1 4 610 14 20 30 40 60 100 200
323
DATE:
FIG. NO.
00-1562
I HGE
01/28/00
100
10
90
20
80
70
(5
z
40
60
w
tn
Li
a:
so
-50
0.
z
z
60
40
Lj
u
ix
lx
w
CL,
70-
30
w
(L
80-
20
0 -
10
,:0
0
100
50 10.0 5.0 1.0 0.5 0.1
.05 .01
.005
.001
PARTICLE SIZE IN MILLIMETERS
GRAVEL SAND
SILT AND CLAY
C3
0
u
COARSE FINE COARSE MEDIUM FINE
MINUS #4
SAMPLE
U. S. STD. SIEVE
% RET.
% PASS
#4
0.6
99.4
#8
1.2
98.8
#16
2.2
97.8
#30
3.2
96.8
#50
4. 1
95.9
#100
6.7
93.3
#200
12.8
87.2
BORING: B-2
ANTHONY -TAYLOR CONSULTANTS
DEPTH: 36.0 FT.
"y C-1 -.
50
1.1-W, CA 11019 . .......
116*1
JOB NAME:
LA QUINTA
SITE ADDRESS:
W OF HWY 111 AND WASHINGTON ST. LA QUINTA, CA.
JOB NUMBER:
REVIEWED BY:
DATE:
FIG. NO.
00-1562
I HGE
01/28/00
MECHANICAL ANALYSIS - SIEVE TEST DATA
0
10
20
a 30
Li
z
40
Li
50
z
w 60
u
0!
w
0. 70
so
90
100
U.S. STANDARD SIEVE SIZES
50 80
100 50 10.0 5.0 1.0 0.5 0.1 .05 .01 .005 .001
PARTICLE SIZE IN MILLIMETERS
(A
GRAVEL
SAND
#4
C3
0
SILT AND CLAY
#8
1.3
98.7
#15
1.7
u
COARSE
FINE
COARSE
MEDIUM
FINE
97.3
U. S. STD. SIEVE
MINUS #4
% RET.
SAMPLE
% PASS
#4
0.7
99.3
#8
1.3
98.7
#15
1.7
98.3
#30
2.0
98.0
#50
2.7
97.3
#100
25.5
74.5
#200
69.6
30.4
00
D
D
D
Z
(A
(L
D
z
D w
u
0
D
D
BORING: B-2
ANTI-IONY-TAYLOR CONSULTANTS
DEPTH: 41.0 FT.
1- 11 .. - r C. C., '(1 -
315 150
C. 42029 9.0s ........ 1.
JOB NAME:
LA QUINTA
SITE ADDRESS:
W OF HWY 111 AND WASHINGTON ST. LA OUI TA, CA.
JOB NUMBER:
00- 1562
REVIEWED BY:
1 HGE
DATE:
10 1 128ZOO
FIG. N 10.
I Him
Wga�-w t
MECHANICAL ANALYSIS - SIEVE TEST DATA
0
10
20
a 30
Li
z
40
Li
50
z
Ll 60
u
0:
W
a. 70
so
90
100
U.S. STANDARD SIEVE SIZES
50 ao
100 50 10.0 5.0 1.0 0.5 0.1 .05 .01 .005
PARTICLE SIZE IN MILLIMETERS
too
go
80
70 0
z
80 tA
vi
n
so
z
40 uj
u
30 (L
20
10
0
001
U.S. STD. SIEVE
GRAVEL
SAND
% RET.
0
StLT AND CLAY
ZT1,
100.0
# a . .
0.0
100.0
u
0.0
N E
COARSE
I MEDIUM
I FINE
#50
U.S. STD. SIEVE
MI -NUS #4
SAMPLE
% RET.
% PASS
#4
0.0
100.0
# a . .
0.0
100.0
#16
0.0
100.0
#30
0.0
100.0
#50
3.7
96.3
#100
36.7
63.3
#200
72.4
27.6
13ORING: 8-2
ANTI-IONY-TAYLOR CONSULTANTS
DEPTH: 46.0 FT.
S. P -w..
I "'i "o
CA'o :2'024 r—,.. 45
1?601 ?35-6800
JOB NAME:
LA QUINTA
SITE ADDRESS:
W OF HWY 111 AND WASHINGTON ST. LA QUII TA, CA.
JOB NUMBER:
I REVIEWED BY:
DATE:
NO.
Illn
00-1562
HGE _I
01/28/00
MECHANICAL ANALYSIS -
SIEVE
TEST DATA
- too , C.y C. -t. I...
I .... C. 910)t
U.S. STANDARD SIEVE SIZES
JOB NAME:
LA QUINTA
SITE ADDRESS:
7
so 60
4 3 2 1 /2 '1 3/. 3/. 1/4 4 510 14 2030 40 60 WO 200 325
W OF HWY 111 AND WASHINGTON ST. LA QUINTA, CA.
JOB NUMBER:
00-1562
I REVIEWED BY:
HGE
DAT
01728/001
FIG. NO. 1110
- I
100
10-
20-
so
a
3wo -
70
La
z
.4
40
60
Ln
Ln
(L
Of
50
50
t -
z
z
La
w
Go
40
u
cr
cc
w
70
30
(L
so
20
90
0
100
0,
100 50 10.0 5.0 1.0 0.5 0.1
.05 .01
.005 .001
PARTICLE SIZE IN MILLIMETERS
CRAVEL
SAND
SILT AND CLAY
,-SE
FINE
COARSE
MEDIUM
FINE
C3
0
u
MINUS #4
SAMPLE
U.S. STD. SIEVE
% RET.
% PASS
#4
0.0
100.0
#8
0.0
100.0
#16
0.0
100.0
#30
0.0
100.0
#50
1.2
98.8
#100
35.3
64.7
#200
81.4
18.6
BORING: B-2
A NTI-IONY-TAYLOR CONSULTANTS
DEPTH: 51.0 FT.
- too , C.y C. -t. I...
I .... C. 910)t
11401,
JOB NAME:
LA QUINTA
SITE ADDRESS:
W OF HWY 111 AND WASHINGTON ST. LA QUINTA, CA.
JOB NUMBER:
00-1562
I REVIEWED BY:
HGE
DAT
01728/001
FIG. NO. 1110
- I
MECHANICAL ANALYSIS -
SIEVE
TEST
DATA
U.S. STANDARD SIEVE SIZES
LA QUINTA
SITE ADDRESS:
7 4
so so
6 100
3 2 1 '2 1 3/ 14 3/ 1/ 1 510 14 20 30 40 0 200
325
REVIEWED BY:
1 HGE
DATE:
101/28/001
FIG. NO.
HIP
100
10
go
20
ao
30
70
z
40-
60
tn
V)
50-
50
z
z
La
w
u
Go-
-40
u
a:
a.
70-
30
80
20
90
10
00
:110
100 50 10.0 5.0 1.0 0.5 0.1
.05 .01
.005
.001
PARTICLE SIZE IN MILLIMETERS
GRAVEL SAND
-FlINE
SILT
AND CLAY
03
0
u COARSE COARSE MEDIUM FINE
MINUS #4
SAMPLE
U.S. STD. SIEVE
% RET..
% PASS
#4
0.0
100.0
#8
0.0
100.0
#16
0.0
100.0
#30
0.0
100.0
#50
4.3
95.7
#100
33.0
67.0
#200
73.2
26.8
lt2V&ktWA I
BORING: B-3
ANTI-IONY-TAYLOR CONSULTANTS
DEPTH: 16.0 FT.
v.lm"A. -s-1.1 "y C-1 I...
C. 170)9 t, .....
JOB NAME:
LA QUINTA
SITE ADDRESS:
OF HWY 111 AND WASHINGTON ST. LA QUINTA, CA.
-W
JOB NUMBER:
00- 1562
REVIEWED BY:
1 HGE
DATE:
101/28/001
FIG. NO.
HIP
BORING: B-3
ANTI-IONY-TAYLOR CONSULTANTS
DEPTH: 16.0 FT.
v.lm"A. -s-1.1 "y C-1 I...
C. 170)9 t, .....
JOB NAME:
LA QUINTA
SITE ADDRESS:
OF HWY 111 AND WASHINGTON ST. LA QUINTA, CA.
-W
JOB NUMBER:
00- 1562
REVIEWED BY:
1 HGE
DATE:
101/28/001
FIG. NO.
HIP
APPENDIX A
Engm! M.'am
Blake, T.F., 1996, EQFAULT Software, Version 2.20
Blake, T.F., 1998, LIQUEFY2 Software, Version
Campbell, K.W., 1993, Empirical Prediction of Near -Source Ground Motion from Large
Earthquakes, in Proceedings of International Workshop on Earthquake Hazard and
Large Dams in the Himalaya, Sponsored by the Indian National Trust for Art and
0
Cultural Heritage (INTACH), New Delhi, India, January 15-16.
California Division of Mines and Geology, 1966, Geologic Map of California, Santa Ana
Sheet. Olaf P. Jenkins Edition, compiled by C.W. Jennings, Scale 1:250,000, Fourth
Printing, 1992.
Greensfelder, R., 1974, Maximum Credible Rock Acceleration From Earthquakes in
California, California Division of Mines and Geology, Map Sheet 23, dated 1972 and
revised August, 1974.
Hart, E. W., W. A. Bryant, 1997, Fault -Rupture Hazard Zones in California, Department
of Conservation Division of Mines and Geology, Special Publication 42, revised
1997.
International Conference of Building Officials, 1997, Uniform Building Code Volume 2,
Structural Engineering Design Provision. Dated April 1997.
International Conference of Building Officials, 1998, Maps of Active Fault Near -Source
Zones in California and Adjacent Portions of Nevada. To be used with the 1997,
Uniform Building Code. Dated February 1998
Jennings, C.W., 1992, Preliminary Fault Map of California, California Division of Mines
and Geology Open -File Report 92-03.
Murphy, J.R., and O'Brian, L.J., 1978, Analysis of Worldwide Strong Motion Data
Sample to Develop an Improved Correlation Between Peak Acceleration, Seismic
Intensity, and Other Physical Parameters, U.S. Nuclear Regulatory Commission,
NUREd-0402.
Ploessel, M.R., and Slosson, J.E., 1974, Repeatable High Ground Accelerations from
Earthquakes - - Important Design Criteria, California Geology, vol. 27, no. 9.
APPENDIX B
'UNIFIED SOIL CLASSIFICATION CHART
SOIL DESCRIPTION
COARSE-GRAINED
N11dre than half of material is larger than a No. 200 sieve
GRAVELS. CLEAN GRAVELS
More that half of coarse fraction is larger
than No. 4 sieve size, but smaller than 3"
GRAVELS WITH FINES
(appreciable amount)
SANDS, CLEAN SANDS
More than half of coarse fraction is
smaller than a No.4 Sieve
SANDS WITH FINES
(appreciable amount)
FINE-GRAINED
More than half of material is smaller than a No. 200 sieve
SILTS AND CLAYS
Liguid Limit Less Than 50
Liguid Limit Greitcr Than 50
I ll(;I ILY ORGANIC SOILS
04�&ww,� t
P'I
G W
Well -graded gravel and sand mixtures,
little or no fines.
GP
Poorly graded gravels, gravel and sand
mixtures, little or no fines
GN,l
Silty gravels. poorly graded
OL
grave I-sand-si It mixtures.
GC
Clay gravels, poorly graded
NTH
gravel -sand silt mixtures.
SW
Well -graded sand, gravelly sands, little
or no fines.
SP
Poorly graded sands, gravelly sands,
little or no Fines.
S?vI
Silty sands, poorly graded sand and
silty mixtures.
SC
Clayey sands, poorly graded sand and
clay mixtures.
ML Inorganic silts and very fine sands,
rock flour, sandy silt and clayey -silt
sand mixtures with a slight plasticity.
CL
Inorganic clays of low to medium
plasticity, gravelly clays, sandy clays,
silty clays, clean clays. .
OL
Organic silts and organic silty clays of
low plasticity.
NTH
Inorganic silts, micaceous or
diatomaceous fine sandy or silty soils,
elastic silts.
CH
Inorganic clays of high plasticity, fat
clays
01.1
Organic clays of medium to high
plasticity
11catand
other highly organic soils
xlaNgddv
DATE: Tuesday, February 1, 2000
E Q F A U L T
Ver. 2.20
(Estimation of Peak Horizontal Acceleration
From Digitized California Faults)
SEARCH PERFORMED FOR: M&H Property Management, LLC
JOB NUMBER: 00-1562
JOB NAME: La Quinta
SITE COORDINATES:
LATITUDE: 33.7149 N
-LONGITUDE: 116.296 W
SEARCH RADIUS: 100 mi
ATTENUATION RELATION: 1) Campbell & Bozorgnia (1994) Horiz. Alluvium
UNCERTAINTY (M=Mean, S=Mean+l-Sigma): M.
S60ND: 0.
COMPUTE PEAK HORIZONTAL ACCELERATION
FAULT -DATA FILE USED: CALIFLT.DAT
-SOURCE OF DEPTH VALUES (A=Attenuation File, F=Fault Data File): A
-----------------------------
DETERMINISTIC SITE PARAMETERS
-----------------------------
Page 1
-----------------------------------------------------------------------------
I
IMAX. CREDIBLE
EVENTJIMAX. PROBABLE EVENT1
I
APPROX. I
-------------------
11
-------------------
I
ABBREVIATED IDISTANCE I
K;LX.1
PEAK I
SITE 11
MAX.1
PEAK I
SITE I
FAULT NAME I
mi
(km) ICRED.1
SITE JINTENSI]PROB.1
SITE IINTENSI
I
'I
I
MAG.JACC. gl
MM 11
MAG.IACC. gl
MM I
-------------------------- I
IBLUE CUT 1
---------
14
I
( 22)l
----- I
7.001
------ I
0.2211
------ 11
IX 11
----- I
6.001
------ I
0.1041
------ I
VII I
I-------------------------- I
ISORREGO MTN. (San Jacinto)l
---------
36
I
( 58)l
----- I
6.501
------ I
0.0481
------ 11
VI 11
----- I
5.751
------ I
0.0241
------ I
V I
I--------------------------
IBRISTOL MOUNTAIN
---------
69
I
(111)1
----- I
7.001
------ I
0.0321
------ 11
V 11
----- I
5.751
------ I
0.0101
------ I
111 1
I--------------------------
ICALICO NEWBERRY 1
---------
46
I
( 74)1
----- I
7.201
------ I
0.0641
------ 11
VI 11
----- I
5.751
------ I
0.0181
------ I
IV I
I-------- ------------------ I
ICAMP ROCK-EMER.-COPPER MTNI
---------
32
I
( 51)1.
----- I
7.001
------ I
0.0861
------ II
VII 11
----- I
5.751
------ I
0.0291
------ I
V I
I-------------------------- I
ICASA LOMA-CLARK (S.Jacin.)l
---------
20
I
( 32)l
----- I
7.001
------ I
0.1491
------ 11
VIII 11
----- I
6.751
------ I
0.1221
------ I
VII I
I-------------------------- I
ICHINO 1
---------
71
(115)1
7.001
------ I
0.0281
------ 11
V 11
----- I
5.501
------ I
0.0081
------ I
111 1
I----- 7 -------------------- I
ICOYOTE CREEK (San Jacinto)l
---------
22
I
( 35)1
----- I
7.001
------ I
0.1331
------ 11
VIII 11
----- I
5.751
------ I
0.0461
------ I
VI I
I-------------------------- I
ICUCAMONGA 1
---------
73
I
(117)1
----- I
7.001
------ I
0.0271
------ 11
V 11
----- I
6.251
------ I
0.0151
------ I
IV I
I-------------------------- I
IELSINORE' 1
:
---------
43
I
( 69)l
----- I
7.501
------ I
0.0901
------ 11
YII 11
----- I
6.751
------ I
0.0471
------ I
VI I
I--------- ----------------- I
IGLN.HELEN-LYTLE CR-CLREMNTI
---------
37
I
( 60)l
----- I
7.001
------ I
0.0701
------ 11
VI 11
----- I
6.501
------ I
0.0451
------ I
VI I
I-------------------------- I
IHARPER 1
z
---------
89
I
(144)1
----- I
7.001
------ I
0.0231
------ 11
IV 11
----- I
5.251
------ I
0.0051
------ I
11 1
I------------ ------------- I
IHELENDALE 1
---------
45
I
( 72)1
----- I
7.301
------ I
0.0721
------ 11
VII 11
----- I
S.751
------ I
0.0181
------ I
IV I
I-------------------------- I
IHOMESTEAD VALLEY - 1
---------
39
I
( 63)1
----- I
7.501
------ I
0.1011
------ 11
VII 11
----- I
4.001
------ I
0.0051
------ I
1 1
I-------------------------- I
IHOT S -BUCK RDG.(S.Jacinto)l
---------
17
I
( 28)l
----- I
7.001
------ I
0.1751
------
VIII 11
6.001
------ I
0.0781
------
VII
I-------------------------- I
JIMPERIAL - BRAWLEY 1
---------
68
I
(110)]
----- I
7.001
------ I
0.0321
------ 11
V 11
----- I
6.751
------ I
0.0261
------
V I
I-------------------------- I
IJOHNSON VALLEY 1
---------
32
I
( 51)1
----- I
7.501
------ I
0.1291
------ 11
VIII 11
------ I
5.251
------ I
0.018'1
------ I
IV .1
I-------------------------- I
ILA NACION 1
---------
77
I
(123)1
----- I
6.501
------ I
0.0171
------ 11
IV 11
----- I
4.251
------ I
0.0031
------ I
1 1
I-------------------------- I
ILENWOOD-OLD WOMAN SPRINGS 1
---------
43
I
( 69)l
----- I
7.301
------ I
0.0761
------ 11
VII 11
----- I
5.251
------ I
0.0121
------ I
111 1
I-------------------------- I
ILOCKHART., 1
---------
92
I
(148)1
----- I
7.301
------ I
0.0281
------ 11
V 11
----- I
5.751
------ I
0.0071
------ I
11 1
I--------------------- I
ILUDLOW ... 1 0
; 1
-------------------------- I
---------
55
---------
( 89)l
I
7.001
----- I
------ I
0.0421
------ I
------ 11
VI 11
------ 11
5.751
----- I
------ I
0.0141
------ I
------
IV I
------ I
IMANNIX 1 87 (139)1 6.60
1 -------------------------- I --------- I -----
INEWPORT-INGLEWOOD-OFFSHOREI 78 (125)1 7.00
1 --------------- 7 ---------- I --------- I -----
INORTH FRONTAL FAULT ZONE 1 47 ( 76)1 7.70
1 -------------------------- I --------- I -----
IPALOS VERD-CORON.B.-A.BLANI 92 (148)1 7.50
1 -------------------------- I --------- I -----
0161 IV 11 5.751 0.0081 11
0271 V 11 5.751 0.0091 111
------ I ------ I I ----- I ------ I ------ 1
0.0951 VII 11 5.751 0.0171 IV I
------ I ------ 11 ----- I ------ I ------ 1
0.0341 V 11 6.751 0.0171 IV I
------ I ------ 11 ----- I ------ I ------ I
------------------------------
DETERMINISTIC SITE PARAMETERS
-----------------------------
Page 2
-----------------------------------------------------------------------------
I
IMAX. CREDIBLE
EVENT11MAX.
PROBABLE
EVENT
I
APPROX. I
-------------------
11
-------------------
ABBREVIATED IDISTANCE I
K;LX.1
PEAK I
SITE 11
MAX.1
PEAK I
SITE
FAULT NAME I
mi
(km) ICRED.1
SITE JINTENS11PROB.1
SITE JINTENS
I
I
MAG.JACC. gl
MM .11
HAG.JACC. gl
MM
-------------------------- I
IPINTO MOUNTAIN - MORONGO 1
---------
28
I
( 45)1
----- I
7.301
------ I
0.1271
------ 11
VIII 11
----- I
5.751
------ I ------
0.0341
V
I--------------------------- I
JPISGAH - BULLION 1
---------
35
I
( 57)1
----- I
7.001
------ I
0.0751
------ 11
VII 11
----- I
6.001
------ I ------
0.0311
V
I-------------------------- I
[ROSE CANYON 1
----------
76
I
(122)1
----- I
7.001
------ I
0.0281
------ 11
V 11
----- I
6.001
------ I
0.0111
------
111
I-------------------------- I
ISAN ANDREAS (Coachella V.)J
---------
6
I
( 9)1
----- I
8.001
------ I
0.4921
------ 11
X 11
----- I
7.001
------ I
0.3931
------
X
I -------------------------- I
ISAN ANDREAS (Mojave) 1
---------
78
I
(126)1.8.301
----- I
------ I
0.0841
------ 11
VII 11
----- I
8.001
------ I
0.0651
------
VI
I-------------------------- I
ISAN ANDREAS (S. Bern.Mtn.)l
---------
25
I
( 41)1
----- I
8.001
------ I
0.2361
------ 11
IX 11
----- I
6.751
------ I
0.0911
------
Vii
I-------------------------- I
ISAND HILLS 1
---------
42
I
( 67)1
----- I
8.001
------ I
0.1401
------ 11
VIII 11
----- I
6.751
------ I
0.0491
------
VI
I----- I --------------------- I
ISAN GORGONIO - BANNING 1
---------
6
I
( 10)1
----- I
7.501
------ I
0.5101
------ 11
X 11
----- I
7.001
------ I
0.4621
------
X
I-------------------------- I
ISIERRA MADRE-SAN FERNANDO 1
---------
91
I
(146)1
----- I
7.501
------ I
0.0301
------ 11
V 11
----- I
6.001
------ I
0.0091
------
111
I-------------------------- I
ISUPERSTITION HLS.(S.Jacin)l
:
---------
54
I
( 88)1
----- I
7.001
------ I
0.0431
------ 11
YI 11
----- I
6.251
------ I
0.0221
------
IV
I-------- ------------------ I
ISUPERSTITION MTN.(S.Jacin)l
---------
53
I
(.86)1
----- I
7.001
------ I
0.0441
------ 11
VI 11
----- I
6.251
------ I
0.0231
------
IV
I-------------------------- I
1WHITTIER - NORTH ELSINORE 1
---------
70
I
(113)1
----- I
7.501
------ I
0.0481
------ 11
VI 11
----- I
6.001
------ I
0.0131
------
111
--------------------------- I ---------
------ I ------ 11
------ I ------
-END OF SEARCH- 37 FAULTS FOUND WITHIN THE SPECIFIED SEARCH RADIUS.
THE SAN ANDREAS (Coachella V.) FAULT IS CLOSEST TO THE SITE.
IT IS ABOUT 5.7 MILES AWAY.
LARGEST KAXIMUM-CREDIBLE SITE ACCELERATION: 0.510 g
LARGEST MAXIMUM -PROBABLE SITE ACCELERATION: 0.462 g
wtm�w_u Y
Based on equation of Murphy & O'Brian (1978) for western U.S
xii
Damage total or nearly total.
1.0—
xi
z
0
xMajor
damage, such a's collapse
of weak buildings and
Ixcracking
of strong buildings
v I I I
Moderate damage, such as fractues of
weak walls and top.pled chimneys.
V I I
Same structural damage, such as
�4
V I
cracks in walls and chimneys.
Felt by most people; objects disturbed;
no structural damage.
IV
0.01
Felt indoors by some people; no damage
Not g'eneraily felt by people.
COMPARISON OF
PEAK HORIZONTAL ACCELERATION
AND
MODIFIED MERCALLI INTENS"
Based on equation of Murphy & O'Brian (1978) for western U.S
EARTHWORK AND GRADING GUIDELINES
1. GENERAL
A. These guidelines present general procedures and requirements for earthwork
and grading. including preparation of areas to be filled. placement of fill,
installation ofsub-drains and excavations. The recommendations contained
in the geotechnical report are part of the earthwork and grading guidelines
and would supersede the provisions contained hereafter in the case of
conflict. Evaluation performed by the consultant during the course of
grading may result in new recommendations which could supersede these
guidelines or the recommendations contained in the geotechnical report.
B. The contractor is responsible for the satisfactory completion of all earthwork
in accordance with provisions of the project plans and specifications. The
project soil engineer and engineenng geologist (geotechnical consultant) or
It . 4 their representatives should provide observation and testing services, and
geotechnical consultation during the duration of the project.
11. EARTHWORK OBSERVATIONS AND TESTING
A. Geotechnical Consultant
Prior to the conunencement of grading, a qualified geotechnical. consultant
(soil engineer and engineering geologist) should be employed for the purpose
0 0.
of observinQ earthwork procedures and testing the fills for conformance with
the reconunendations of the geotechr&al report, the approved grading plans,
and applicable grading codes and ordinances.
The geotechnical consultant should provide testing and observation so that
determination may be made that the work is being accomplished as specified.
It is the responsibility of the contractor to assist the consultants and keep
them appraised of anticipated work schedules and changes, so theat they may
schedl.l.lie their personncl accordingly.
All clean -outs, prepared ground to receive fill, key excavations, and sub -
drains should be observed and documented by the project engineering
geologist and/or soil engineer prior to placing any fill.' It is the contractor's
responsibility to nolify the engineering geologist and soil engineer when such
areas are ready for observation.
M3=w--W- i
0
B. Laboritory and Field Test
Maximum dry density tests to determine tile degree ofcompaction should be
performed in accordance with American Standard Testing Materials test
rilethod ASTNM designation D- 15 5 7. Random field compaction tests should
be performed in with method ASTNI designations D-1 556-82. D-2937 or D-
2922 & D-3)0 17. at intervals of approximately two (2) feet of fill height or
every 1000 cubic yards of fill placed. These criteria would vary depending
on the'soil conditions and the size of the project. The location and frequency
of testing would be at the discretion of the geotechnical consultant.
C. Contractor's Responsibility -
All clearing. site preparation, and earthwork performed on the project should
be conducted by the contractor, with observation by geotechnical consultants
and staaed approval by the governing agencies. It is the contractor's
responsibility to prepare the ground surface, to receive the fill, to the
satisfaction of the soil engineer. And to place, spread, moisture condition,
mix and compact the fill in accordance with the recommendations of the soil
engineer. The contractor should also remove all major non -earth material
considered unsatisfactory by the soil engineer.
It is the sole responsibility of the contractor to provide adequate equipment
and methods to accomplish the earthwork in accordance with applicable
grading guidelines, codes or agency ordinances, and approved grading plans.
Sufficient watering apparatus and compaction equipment should be provided
by the contractor with due consideration for the fill material, rate of
placement, and climatic conditions. If, the opinion of the geotechnical
consultant, ' unsatisfactory conditions such as questionable weather, excessive
oversized rock, or deleterious material, insufficient support equipment, etc.,
are resulting in a quality of work that is not acceptable, the consultant will
inform the contractor, and the contractor is expected to rectify the conditions,
and if necessary, stop work until conditions are satisfactory.
Durina construction, the contractor shall properly grade all surfaces to
maintdin"good drainage and prevent ponding of water. The contractor shall
take remedial measures to control surface water and to prevent erosion of
graded areas until such time as permanent drainage and erosion control
measures have been installed.
Ill SITE PREPARATION
A. All major vegetition, including brush, trees, thick grasses, organic debris, and
other deleterious material ShOUld be removed and disposed of oft-sitc. These
removals nlUst be coilcludc(l prior to placing f1l. Existing fill, soil, alluvium,
U,
C011LIVium, or rock materials det ' ermined by tile soil engineer or engineering
geologist as being unsuitable in-place should be removed prior to fill
placement. Depending upon tile soil conditions, these materials may be
reused as compacted fill. Any materials incorporated as part of the
compacted Cills should be approved by the soil engineer.
B. Any underground structures such as cesspools, cisterns, mining shafts,
tunnels, septic tanks, wells, pipelines, or other structures not located prior to
grading are to be removed or treated in a manner recommended by the soil
engineer. Soft, dry, spongy, highly fractured, or otherwise unsuitable ground
extendina to such a depth that surface processing cannot adequately improve
the condition should be over excavated down to firm cyround and approved
by the soil engineer before compaction and filling operations continue. Over
excavated and processed soils which have been properly mixed and moisture -
conditioned should be recompacted to the minimum relative compaction as
specified in these guidelines.
C. Existing, gound which is determined to be satisfactory for support of the fills
should be scarified to a minimum depth of six (6) inches or as directed by the
soil en2ineer. After the scarified ground is brought to optimum moisture or
greater and mixed,.the materials should be compacted as specified herein.
If the scarified zone is greater than 6 inches in depth, it may be necessary to
remove the excess and place the material in lifts restricted to about six (6)
inches in compacted thickness.
D. Emsting ground which is not satisfacto to support compacted fill should be
over excavated as required in the geotechnical report or by the on-site soils
engineering geologist. Scarification, dicing, or other acceptable form of
mixing should continue until the soils are broken down and free of large
lumps or clods, until the working surface is reasonably uniform and free from
ruts, hollows, hummocks, or other uneven features which would inhibit
compacti on as described in Item III, C, above.
E. Where fills are to be placed on ground with slopes steeper than 5:1
(horizontal to vertical), the ground should be stepped or benched. The lowest
bench, which will act as a key, should be a minimum of 15 feet wide and
should be at least two (2) feet deep into firm material, and approved by the
soil engineer and/or engineering geologist.
In fill over cut slope conditions the recommended minimum width of the
lowest bench or key is also 15 flect with tile key founded on firm material, ans
dcsignatcd by the Geotechnical Consultant. As a general rule, unless
I.,
specifically recommended otherwise by tile Soil Engineer. the minimum
%vidth oCtill keys should beapproximately equal to one-halt*(1/2) the height
oCtlie slope.
F. Standard benching is generally four feet (minimum) vertically. exposing firm,
acceptable material. Benching may be used to remove unsuitable materials,
although it is understood that the vertical height of the bench may exceed, four
feet. Pre -stripping may be considered for unsuitable materials in excess of
four feet in thickness.
G. All areas to receive fill, including processed areas, removal areas, and toe of
fill benches should be observed and approved by the soil engineer and/or
engineering geologist prior to placement of fill. Fills may then be properly
placed and compacted until design grades are attained.
IV. CONIPACTED FILLS
A. Any earth materials imported or excavated on the property may be utilized in
the fill provided that each material has been determined to be suitable by the
soil engineer. These materials should be free of roots, tree branches, other
orQanic matter or other deleterious materials. All unsuitable materials should
be removed from the fill as directed by the soil engineer. Soils of poor
gradation, undesirable expansion potential, or substandard strength
characteristics may be designated by the consultant as unsuitable and may
require blending with other soils to serve as a satisfactory fill material.
B. Fill materials derived from benching operations should be dispersed
throughout the fill area and blended with other bedrock -derived material.
Benching operations should not result in the benched material being placed
only within a single equipment width away from the fillfbedrock contact.
C. Oversized materials defined as rock or other irreducible materials with a
maximum dimension greater than 12 inches should not be buried or placed
in fills,un'less the location of materials and disposal methods are specifically
approve by the soil engineer.
Oversized material should be taken off-site or placed in accordance with
reco I mmendations of the soil engineer in areas designated as suitable for rock
disposal. Oversized material should not be placed within 10 feet vertically
of finish grade or within 20 feet horizontally of slope faces. To facilitate
trenching, rock should not be placed within the range or foundation
excavations, future utilities, or underground construction unless specifically
approved by the soil engineer and/or the developers representative.
it' import material is required j -or grading, representative samples Of the
D. as compacted fill should be analyzed in the laboratory
material to be utilized determine its physical . properties- If any material other
by he soil engineer to tested is encountered during grading, an appropriate
than that previously al should be conducted by the soil engineer as soon as
analysis of this materi
possible. ill in
E. Approved fill material should be placed in areas prepared to receive f
near-hOrizontal layers that when compacted should not exceed six (6) inches
thicker lifts if testing indicates
in thickness- 'Me soil engineer may' approve paction is being achieved
ing procedures are such that adequate com
the grad .
with lifts of greater thickness. Each layer should be spread evenly and
. of material and moisture suitable for compaction.
blended to attain _un_i_f_0_rM__1t_Y—
F. Fill lavers at a moisture content less than optimum should be watered and
by scarification or should be
mixed, and Nvet fill layers should be aerated ng and mixing of
blende . d with drier material. 'i'vloisture conditioning, blendil " 'form moisture
til the fill materials have a uni
the fill lavers should continue un
content at or above optimum moisture.
been evenly spread, moisture -conditioned and mixed', it
G. After each layer has . . Urn of go percent of Maximum
should be uniformly compacted to a minim -78, or as otherwi . se
density as determined by ASTNI test desiLrnation, D 1557
tgineer. Compaction equipment should be
recommended by the soil er ction or
ately sized and should be specifically designed for soil compa
adequ degree of compaction.
of proven reliability to efficiently achieve the specified
Where tests indicate that the density of any layer of fill, or portion'thereof, is
below the required density and/or moisture content has been attained. No
ntil the last placed lift of till has
additional fill shall be placed in an area u equirements, and is
been tested and found to meet the density and moisture r
approved by the soil engineer.
inimum
e accomplished by over -building a m
Compaction of slopes should b ently trimming back to the design
of three (3) feet horizontally, and subsequ rformed as the fill is elevated to
slop e configuration. Testing shall be pe Special efforts may
evaluated compaction as the fill core is being developed.
be necessary to attain the specified compaction in the fill slope zone.
Final slope shaping should be performed by trimming and removing loose
materialS with appropriate equipment.
Q
paction should be based on observation
A final actcrmination of fill slope com III slopes are
c face. Where compacted r
and/or testing of tile finished stop aterial types, a relative
designed steeper than 2. 1, aa�_d& m may be recommended.
compaction, and pacted Fill slopes
r -building and cutting back the com
if an alternative to Ove effort should be mad to achieve the required
is selected. then special of each lift of fill by undertaking the
compaction in the outer 10 feet
following* LVV short-shanked
ent consisting of a hea
Ia. An extra piece of equipm nta-1) parallel to the slopes
sheepsfOOt should be used to roll (horizO hould -also be
as fill is placed. The sheepsfoot roller s
continuously and extend out over the slope
used to roll perpendicular to the slopes,
to provide adequate compaction to the face of the slope-
er the face of the slope as each
1b. Loose fill should not be spilled out OV x a previously completed
lift is compacted. Ariy . loose ,,, spilled ove e-rollin-a",
ed off or be subject to r
slope face should be triMM
(horizontal) two (2)
Ic. Field compaction tests will be made in the outer, vertical intervals,
to eight- (9) feet of the slope at appropriate
ction operations.
subsequent to compa slope, the slope face should be shaped with
Id. After completion of the epsfoot to achieve
a small tractor and then re -rolled with a she
nt to testing to verify
n to near the slope face. Subseque
compactio s should be grid -rolled to achieve compaction
compaction, the slope testing should be used to confirm compaction
to the slope face. Final .
after grid rolling. than adequate action, the contractor
sting indicates less comprecompact the Slope
le. Where te water, m.ix and
,yill be responsible to rip, I testing
to achieve compaction. Additiona
materials as necessary -ipaction.
should be performed to verify con
drainage devices should be designed by the
if. Erosion control and 1pliance with the ordinances of the
project civil engineer in con' ies, and/or in ,1ccordance with the
controlling govcmmental agenc lincering geologist.
recommendations Of the soil engineer Or eng
A
V. S1jB_i)gA1N INSTALLATION
A. SUb-drains should be installed in approved ground in accordance with the
approximate alignment and details indicated by the geotechnical consultant.
Sub -drain locations or materials should not be changed or modified without
approval of the geotechnical consultant. The soil engineer and/or engineering
izeologist may recommend and direct changes in sub -drain line, grade and
drain material in the field, pending exposed conditions. The location of
constructed sub -drains should be recorded by the project civil engineer.
V I. EX- , �kv A T =Nt�
A. Excavations and cut slopes should be examined during grading- by the
locrist and/or geotechnical engineer. If directed by the
ensaineer-ing geo C,
engineer geologist, further excavations or over -excavation and refilling of cut
areas should be performed and/or remedial grading of cut slopes should . be
performed. When fill over cut slopes are to be graded, unless otherwise
approved, the cut portion of the slope should be observed by the engineer
ill portion
geologist prior to placement of materials for construction of the fi
of the slope.
B. The engineer geologist should observe all cut slopes and should be notified
1.7 0
by the contractor when cut slopes are started.
C. If, during the course of grading, unforeseen adverse. or potentially adverse
geologic conditions are encountered, the engineering geologist and soil
engineer should investigate', evaluate and make recommendations to treat
these problems. The need for cut slope buttressing or stab il izi ng,'should be
based on in -grading evaluations by the engineering geologist, whether
anticipated previously or not. ' .
D. Unless otherwise specified in soil and geological reports, no cut slopes should
be excavated higher or steeper than that allowed by the ordinances of
Additionally, short-term stability of
controlling gov.emmental agencies. the contractors
-y cut slopes or temporary excavation is
temporar
responsibility.
E. Erosion control and drainage devices should be designed by the project civil
engineer and ShOUld be constnicted in compliance with the ordinances of the
controlling governmental agencies, and/or in accordance with the
reconimendations of the s . oil engineer or engineering geologist.
MOMM"11
VII. al consultant should
A. Observation, testing and consultation by the gcotechnic an opinion that
be conducted during the grading operations in order to state
all cut and filled areas are graded in accordance with the app roved project
Spec i fications.
B. After completion of grading and after the soil engineer and engineering
their observations of the work, final reports should be
inished No
geologist have r review by the controlling governmental agencies.
submitted subject to
ftuther excavation or filling should be undertaken without prior notification
. eering geologist.
of the soil engineer and/or engin
C. All finished cut and fill slopes should be protected from erosion and/or be
roject. specifications and/or as recommended
planted in accordance with the p h protection and/or Planning should be
by a landscape architect. Suc ter completion of grading.
undertaken as soon as practical af