1991-1170 G/H Street Address
C 2G
Category Serial #
1 C, C`-J
Name Description
Plan ck. # Year
recdescv
LAND DEVELOPMENT ENGINEERING • PLANNING • SURVEYING
(6191756-937 4
The Fairbanks Village Plaza, RO. Box 9661
Rancho Santa Fe, CA 92067
ij
H Y ��oL-n&y OLA
NA v To W� v tj L 14- IN
- D u Z AZ —7 Dr� C A P-7
7=
4
ofESSI
Q A.
Ca
C*' to
rn
W rn
w No. 29375
T F- E ET) = EXP. 3-31-95
Cp IV%
OF 0 ��
rn
r
N
H
c
° - n d
r- m o
v ° z oA
A> v �v�
> r C
n o N n 3
�A orno
o> 0 =�-Z1m
n z b W
"0> W c) C)
n > o r- -n Z
WO p p y N �. W �, (A p
00
om O
r =7 ar
L) x n O
t > O
> o ? n W
H .. Cif z p -
V1 0 2 ;a a ti
>
r> -
> 0 "' n
CD
%°
9 CD
r �' _ t ..J i � � ✓ FYI
O
no ..)ice ( ` \ //• //�� ^� �, // �����qil ~
Co) CD
CD
00 �MM
Ln
LAJ
m � O
'Tl V C
rn . r- m 0
V 6 - 0 C:
tZ 7
7; > o >
> r
n o CA
0 rm 0
= z -n
;;o LA
0 >
n > -n
f- 2 _
0 a tA U
"7 1
z >
> 0
rn
> 0
co V OMM&
O m CD
ly\
.00)
CD C:zt
7/21'
CD
cm
o
cr>
yn
C
cn
CD
z .a r ice; ` •. Q 1 j ".>? .._ �' - _ °/ v'' / �
co
Lri
"ICI
rri
c lA n uAauuv d5 end ..�...�..., . _ k
=' S✓ �' Y' P P ; o
l �
3 1 1 Wi
C -
If
I T
-� _ - - y • O '•Cy H H
0% H V
C+ A -
� i� !�tl IIiII .j ! it � II li — — - _ I c .. 1i - -� .w ►i fD A
I
0 J 0
C I I I r -- — ---- -J i r ' I 1 1 I O ►i C+ Z
I I
tn I I � / --
I I -�- i � I �. N• r1 � Z
0
IL
cn
-+— N N - W twi aA/:
to r a c*'
O Cn O cn O cn «r
G7
(sayOU uOLj? �dLaaJd anOH -g
T_
O Ul -P W N .�
r CD
►-+ C+ "D N -+• c+ -1 _0 v o v c•+ C+ e-+ A N - n C)
0 CL cn o 0 � =r -s -4 o = = n. CD sL m - � -1 r+
II v.
--a Iv CD -+• O w U CD Gu cam. to CD O --•.
II c 11 CD C+ cn C+ :E C+ C+ v c-+ C -`f• C Cn Or a O
w 0 -1•
>F CD CD O 0 [1 CD C+
Z (�� rL Cj Q w O --• C) =• - s O cn 0) a w r
- n o rt CD S r+ -1 O --• v a A o
.J . J. O a -- I=. O w O
- -1 - 1 O J.
a cn O rD 4r - S C
cr =r CD rD r•1• - Z:3 O J CD In 0) - o
-' CD rD - 1 n 0 :.T - 1 n C+ -•
/�• �- :3 J. (D O J J. J• CD CD DA y -b J• J•
• I O :3 - 0 C) O c 0 0- O - S 00 0
Q O' 3 ? O O' r+ e-+ c-+ -S O c+
< - _j - S 11 a c cu Cv =- -•+• CD --+ C+ c+ n -+-
m p co cD a � ° ofl.mv
c+ -+ vn CD O O ^s C+ a In
a O
N c+ p • O O c 'S =5 CD cL
Cy CD � < O O -0 =3 LL -+ CD
CD d 1 �- O CD _�
n H a � n to
rD "S c C •+ -. O -� .� y CD C+
'T I �E S =' O
_J •� =s .A J r cal CD - •• c -h (D
CD II O a -' "7 9 P, n
] to - ' L] - 7 ID n + CD O1
O n tD r -� O to c C S
-.f O C __j C) Q Z CD ••T
1 CI) W cn - T CD O
< v c a n � CL 0
0 CD O
ae rD o (D �— -s ' < a 3
> p =r - Ln O d
-h O 0
/� EQLIAT /ON
-
C //. 9L � 1.385
Feel Tc f/ )
5000 Tc = Tune of concenfral
4000 L ° Length of watershed
H • 0 111 /n elevation a/o ,7g
3oDD ellect /ve s/o oe 1117 (See 'fVpendiX X -,�V 7e-
W1 5
FGe� flours Miaufes
2000 ¢ 2¢D
3 /BD
/D
/DOD.
900
Bloc 2-- 12,0
700
600
\ S 90
SOD \ gp
� 50
200 \ \ 2
a0
/00 / SDOD
•�QDD 20
\ /B
40 2000 \ \ 12
/800 \
310 NOTE
/SOD g
F OR NATURA WATERSF -DS, 1200 B
20 ADD TEN UTES TO /DOD 7
COMPUTED TIM F CON - 900
U CENTRATION_ BOO 6 � -�-s- -- --�
-- — � 700
600 5
/O 500 ¢
¢DD
5 00 3
2
200
A/ L Az
SAN DIEGO COUNTY NOMOGR )kH FOR DETERMINATION
DEPARTMENT OF SPECIAL DISTRICT SERVICES OF TIME ONCENTRATION (Tc)
DESIGN MANUAL FOR NATO L WATERSHEDS
APPROVED DATE /z 4 APPENDIX X -A
L-A-10 Rev. 5/81
Group B
Soils having moderate infiltration rates when
thoroughly wetted, consisting chiefly of mod-
erately deep to deep, moderately well to well
drained soils with moderately fine to mod-
erately coarse textures. These soils have a
moderate rate of water transmission.
Grou C
Soils having slow infiltration rates when
thoroughly wetted, consisting chiefly of
(1) soils with a layer that impedes the
downward movement of water, of (2) soils
with moderately fine to fine texture and a
slow infiltration rate. These soils have a
slow rate of water transmission.
Group D
Soils having very slow infiltration rates when
thoroughly wetted, consisting chiefly of (1)
clay soils with a high swelling potential;
(2) soils with a high permanent water table;
(3) soils with clay pan or clay layer at
or near the surface; and (4) shallow soils over
nearly impervious materials. These soils have
a very slow rate of water transmission.
Soil group and soil cover maps have been prepared by the Soil Con-
servation Service, and include most of the County. The maps are
available at the offices of the Department of Sanitation and Flood
Control.
The Department of Sanitation and Flood Control has developed a computer
program for calculating CN numbers after soils groups and covers have
been tabulated for given basin and sub - basins. Tabulation is usually
accomplished by using a one -half or one inch square grid and listing
the group and cover at each intersection.
The hydrologic condition of soil cover must be determined for each
basin or sub - basin. Photos and slides showing typical hydrologic
conditions of soil cover for many areas of San Diego County can be
examined at the office of the Department of Sanitation and Flood
Control. I -A -4
0
REV. 11/75
t
TABLE 2
RUNOFF COEFFICIENTS (RATIONAL METHOD)
DEVELOPED AREAS (URBAN)
Coeffic C
� • So Group tl)
Land Use
L Residential: A B L.J p
t
Single Family .40 .45 .50 .55
Multi -Units .45 .50 .60 .70
Mobile homes .45 .50 .55 .65
Rural (lots greater than 1/2 acre) .30 .35 40 .45
l
Comme rc i a) (2)
.70 .75 .80 .85
80° / Impervious
!: Industrial 2) .80 .85 .90 .95
s . 90% Impervious
r -
NOTES:
i
( ' ) Soil Group mans are available at the offices of the Department of Public Works.
( actual conditions deviate significantly from the tabulated impervious-
ness values of 80% or 90%, the values given for coefficient C, may be revised
by multiplying 80% or 90% by the ratio of actual imperviousness to the
t. tabulated imperviousness. However, in no case shall the final coefficient
be less than 0.50. For example: Consider commercial property on D soil:-group.
Actual imperviousness = 50%
Tabulated imperviousness - 80%
Revised C = $O x 0.85 = 0.53
IV -A -9
APPENDIX IX -B O
Rev. 5/81
CScE �lCGC�rn N (s Zc�o ACA t� M►A�'�
MAQUAL
►��
0
or eoof4 .0"t,
45bx )r
X
10
All
C- i,
2 107 3. 02
• io l' i 1 I11 11 1 t 1 1 :1 •i,TM��l:j 11 •Il1. l�: l i 1 1 -
i 177
Q � � • -. _ ._.;mss.._ b - ( ( ( = 1 I -
---T-
P =2 ka +b) I V f w �...
A
I kil
LO , / 1 1 i 1 111:: 1: 11:• li r1111.:1i . p ° ).) 1 I ! I °-
-
.v � t � I � I i ( ( 1 �� 1 �� i � 1 1 _ � •
w
I 17 1 u 2 -
LtJ
r —m—
VJ ( � P/ P - S. I OH �
Fil
1 I i I
• o.l c I I f f ! I �,_.,_,_f ' I I i I`f I _ •
H EADS Uj? T!0 VEI(d) IES
HEA A 2 l.4 Icl:����!c�5 !,V I I>=s
S
H EAT B ► ti� c1 J E4,� .°z l =,
• i i' ! 1 i 1
.!
S 040: I:V!1JL =1 NIT
"i ( { ! ! I I ( ={
I I I I f� I } � �' •.
I f I I F 1 '
I I I i
ri
L r31Sr'r':.FtG PER =0 0: P'.R, :i- 1 �`!� Ali* JIS Ll "D - -' r`�= E_
4 .. P r:. F J CI T A.� /
C I 1 / 111111••1.1• Lt.:!.111 111 •I•i.i•.. 1 1, rrI1 • 1. :I� 1 .. {11 'a I. 1 1 ` 1 1,
0.1 ,5 .G .! .J.J i.0 :v �i 5 7 U "J l0 '1
UUR2 Au 0.= PUDLIC ROADS CAPACITY OF GRATE hill' i_E s` 1N' SU.Mp
f OIVISIC ?J T; W 1 10 Q
A�,t U.C. Vrr,TE R PONoEo ON GRAT
- TTY
c
11 — PIPES FLOWING FULL OR PART -FULL
A. Instructions For Us.( Pipe Flow Charts — P Flowing F or Part -Full
1. These charts are designed to enable direct solution of the Manning formula for full flow
and for uniform part -full flow in circular pipes. Each chart applies to pipe of a certain
diameter. The abscissa and ordinate scales represent discharge Q and normal velocity
V for two roughness coefficients n, when read in co.tijunction with the superimposed
lines for slope and normal depth of flow d
2.._J:,"p" ;rnd r :l ...... s;; : :�� :., !;v i.r�. charts for part -full flow apply only to pipe in which
u f at riOrRlai depth has b?2ri established by sufficient length of pipe oil a con-
stant slope when the flow is not affected by backwater.
3. Depth of uniform flow for a given discharge Q in a given size pipe on a given slope S
and with roughness coefficients n = 0. 015 or 0. 024 may be determined directl
from the chart for that size by entering on the appropriate Q -scale and reading depth at
the intersection with the appropriate slope line (or an interpolated slope). Normal veloc-
ity may be read on the appropriate V -scale opposite this same point. The procedure may
be reversed to determine discharge at a given depth of flow.
4. Where the Q- ordinate intersects a slope line, S in the area near its right terminus,
two alternate depths will be indicated if d is greater than 0. 82 diameter. For these
cases, flow will occur at the lesser of the alternate depths.
5. For pipe roughness coefficients other than those of n =0. 015 or 0. 024 shown on
the cl...rt scales, enter the chart on the im o „_al,. for n =0. 015 . tiz an. .,• c d vaiueof
Q = design Q(n /0. 015) to determine depth and velocity. Read depth directly trom the
chart at the pipe slope line, S, and obtain velocity by dividing the value read on the V-
scale for n = 0. 015 by the same ratio n /0. 015. In reversing the above procedure to deter-
mine design Q for a given depth, or agiven friction slope if the pine flows full, read Q on
the scale for n = 0. 015 and divide by the ratio n /0. 015 to obtain the design Q.
6. Tb e— n)aximum_rate.of..dischaxge,,in uniform flow of any circular pipe on a given slope, not
flowing under pressure, will occur with a depth of flow of b. 94 diameter. Therefore, to
determine the maximum capacity of a pipe on a given slope S notflowing under pressure
read the Q- ordinate for the appropriate value of n at the maximum value reached by the
sharply curved slope line (depth equals 0. 94 diameter). Interpolated slopes follow the
same pattern as the designated slope lines.
7. Where the Q- ordinate passes to the right of the sharply curved slope line for pipe slope. S
the pipewillflow full and under pressure. For this case the charts may be used to deter-
mine the slope of the pressure and energy lines, which are parallel when the pipe flows
full. This sloe is the friction slope S or rate
p l f, at which energy is lost by resistance to
flow. Sf willbegreater than the pipe slope S Enter the chart with Q, or an adjusted Q = `.
for the appropriate n value, intersect the line for depth equal to pipe diameter and read
friction slope by interpolation between the short right. -angle marks indicating slope. The
discharge capacity for a pipe f lowing full with a given friction Mope Sf is found by reading
dischargeat the proper slope point along the line for depth equal to pipe diameter.
8. Flow at critical depth may occur in a e flowing with a free water surface that is
P Y P�A 6 ,Part-
ly full. Critical depth d for a given discharge is read by interpolation: from the depth lines
at the point where the Q- ordinate on the a = 0. 015 scale and the critical curve intersect, j
,.n:._ regardless of pipe roughness. Critical velocity VC is the reading on the V- scale for
n = 0. 015 for this Game paint. Critical depths greater than that represented by the last
l - depth line on the charts, just less than a diameter, leave little significance since wave
I action may intermitterOy fiil the pipe. Ii
11 -2
Y ,9. Where n = 0. 015, critical slope S is read at the critical depth point as found in 8 above.
Critical slope will vary with pipe roughnness, therefore, to determine critical slope for
other values of roughness coefficient it is first necessary to determine critical depth.
Critical slope is then interpolated from the slope lines at the intersection of this depth
with the Q from the scale for the appropriate v i!ue of n, or with an adjusted value of Q
for values of n other than shown on chart (see 5 above
2
10. Critical depth d specific head at critical depth h critical slope S
. d + 2
I �( —), pe Cl
friction slope Sf, and relative velocity at constant discharge V /(Vfull) as well as rela-
tive friction slope at constant discharge SF. �
/(Sf full) c�t,� be determined directly by refer-
ence to charts 46 through 79 (pp. 11- 22 to II -55), thus avoiding interpolation. The charts
include all the common structural types.
Xa �trance control curves are-based on expeririental data from a Bureau of Standards Re-
search Project. The curves involving outlet control with a free water surface, on mild = -
slopes, are based on backwater curves assuminn critical depth at the outlet. The limit-
ing value of L /100S where entrance control no longer governs was based on the consid-
eration of pressure plus momentum within the culvert. In cases of outlet control, errors
are less than 6% with respect to more detailed analysis.
12.. Examples:
a. Determine the depth and velocity of flow in a long 30 -in. concrete pipe, n = 0.015,
on a 0. 5 percent slope (S = 0. 005) discharging 25 cfs. Enter chart 35 (p. II- 1G3 at
Q = 25 on n = 0. 015 scale, follow up to intersection with line for slope S = 0.005,
and read normal depth a = 2. 05 ft and normal velocity V = 5.8 fps. To find critical
depth, enter chart at Q = 25 on n = 0. 015 scab, and read critical depth d = 1.7 ft at
intersection with dotted critical curve. Also, critical velocity V = 7. 0 fps. d may
Li A
e verified on Chat 4t3. o
b. Determine friction slope for a 30 -in. corrugated metal 2
ga pipe, n = 0.0.,1, on a slope
S = 0.-008 ft /ft with a discharge Q = 25 cfs. Enter chart 35 at Q = 25 on the Q -scale
for n = 0.024. Note that this ordinate faits to the right of the 0.008 slope line; there-
fore, the pipe will flow full. Read friction slope Sf = 0.012 at the line for depth
equal to pipe diameter.
C. Determine the discharge for the pipe in example b if flowing at a depth of 1.4 ft.
Enter chart 35 at the intersection of depth line 1.4 and slope line 0.008. Design dis-
charge for n = 0. 024 equals 12 cfs. , Read ve locity on n = 0. 024 scale as V =4. 2 fps.
d. Determine critical depth, critical velocity, and critical slope for a 60 -in. concrete
pipe, n = 0. 015 discharging 160 cfs. Enter chart 41 (p. H -16) at Q = 160 on n = 0. 015
scale. At intersection with critical curve read d = 3. 6 ft, V = 10. 5 fps, and
S = 0. 0065 ft /ft.
t ,tea- 1/�,
Tls As
. si 24- .�i•�
00"ti O SL000o--
CHART 2 g o
TT'
q �
P D I I !
.0
1 i
{• � � ii � I ..� �. - \ � --`''' -100 i I I I a N -
\11 E 00`0
{—
�+— — —
It
�► �. J 0 1 , i I
-- It 710 -
0
I r I y N CO
! 0 I O
m i
It
0 0 0 OG l to
4
o0
l co
0 to
, - t
t V 1 �
— = `
U 1� - � i •t� � i I
o l
to
—
j ! Vp0O OV OO C90
;.il \, c o 0 300,0, 00 00000
S /O' U Sdd - ^ - dl/0073A
a om a m r. c h a a d /O' =U Q
O mI to h R M H O h ►� b h 7"-M
i
PIPE FL 0W Cf A R r
20 oi 7�
Type I - With Sil
0 or
-- —�� ly.j, 2 - Vithreit sill
.77;
Icrcte Chinno
[.•I• Lidth of Ce.
_SELECTIC.71 OF RIPPO A FILTER
piprC9 Filter glanket
Velocity Pock Thickness Upper La.�Cr Lcti�r_L
C3 Ft/Sec. Cla"Sificatior (1) Ft. Sec. 2W- s 40-3•
cv
6-) ..3. 3 Zackin!j 3/1 C2
7-8 * No. 2 !ackinq . 1.0 1/4" B3
P-10 Facipi 1.4 3/8"
10-12 tirht 2.0 1/2•• -
C I2 -14 1/4 Ton 2.7 $and
3/4"
If-I& 112 Ton, 3:4 V ... S3nd
zm 16-18 1 Ton 4.3 1 112 'Sand
18-20 1 2. Ton 5.4 2" Sand
PI;A.Fi I ttr 03nket Thickness I Foot or
Flo-w
Z
,o
c cf,00,cm- % I- V1 I I
.4
30 or 31'! 7 r 0i1+ A- A
6' min Sec L
• A Sill � •
Class 8 concrete,
'PLAN if shown on Plans.
• NOTES:
Concrete Channel I- Type of riprap
a Regular Quarry stone.
b: Broken Concrete if S110-40 On Plans,
C. Cobbles not acceptable.
2— Gradation and Placement as specified in
Regional Standards Com, Ste, Spec. Prov,
cr W Sec. .200-1.6.
L. Z:
-)F3_ Piprap is to be Placed over a filter
1/1, blan�et v.hi
11-2 VIA ch May be granular r8terial
or plastic cloth.
Granular r2terial specs. in Table
above.
b. Plastic cloth specs. in Peg. Stds,
Co Std. • Spec. Sec. 200-1.6
• ELEVATION
2- 1) >
Standard Specifications for Public Works
Construction by So. CA Chap. of /%P',-.'A 1, ABC
THE Sm. C-1160 SAN DIEGO REGIONAL STANDARD DRAWING Flev;*.;on et Aprro D.a1z
-
RIP RAP ENERGY DISSIPATOR
En — 1
n MID B-40 It
t
GEOTECHNICAL INVESTIGATION
' 2926 Lone Jack Road
Encinitas, California
1
' HE
THERINGTON ENGINEERING, INC.
1 '
' HETHERINGTON ENGINEERING, INC.
GEOTECHNICAL CONSULTANTS .
' February 26, 1991
Project No. 626.1
Mr. Thomas Frost
4255 Ocean Blvd.
San Diego, CA 92109
' Subject: GEOTECHNICAL INVESTIGATION
2926 Lone Jack Road
' Encinitas, California
References: Attached
Dear Mr. Frost:
' In accordance with your request, we have performed a geotechnical
investigation at the subject site. The purpose of our
investigation was to evaluate the property with respect to
t geotechnical conditions, and to provide recommendations for
precise grading and foundation design for a single- family
residential addition and appurtenant improvements. We were
' provided with a previous geotechnical report for the site and a
"Grading Plan for Building Addition and Pool," prepared by The
Laret Company, undated, for the property which has been used as
the base map for our attached Geotechnical Plan, Figure 1. As
instructed by you, our scope of services has not included a
comprehensive investigation of a possible ancient landslide
within or adjacent to the site.
' With the above in mind, our scope of service has included the
following:
1. Review of available published soil and geologic reports for
the site and vicinity (see attached References);
2. Three backhoe excavations for visual observation, geologic
mapping and soil /bedrock sampling;
., 3. Laboratory testing of representative samples obtained;
4. Engineering and geologic analyses of the data; and,
' 5. The preparation of this report presenting our findings,
conclusions and recommendations along with the supporting
data.
' 5245 AVENIDA ENCINAS • SUITE G • CARLSBAD, CALIFORNIA 92008 • (619) 931 -1917
GEOTECHNICAL INVESTIGATION
Project No. 626.1
February 26, 1991
' Page 2
PROPOSED DEVELOPMENT
Based on discussions with you and review of the "Grading Plan for
Building Addition and Pool," we understand that a detached, two
to three - story, wood - frame, living area and garage addition is
proposed. Conventional continuous /spread foundations with slab -
on -grade ground floors are anticipated. Numerous retaining walls
are proposed to a maximum height of 11 feet, retaining both level
and 2:1 (horizontal to vertical) sloping backfill. Proposed
appurtenant improvements include a swimming pool, play yard,
driveway and other on -grade concrete flatwork.
' Proposed grading consists of designed cut to a maximum depth of
approximately 14 feet and designed fill to a maximum depth of
approximately 12 feet. Fill slopes are proposed to a maximum
height of 20 feet and cut slopes to a maximum height of 6 feet.
All fill slopes are at slope ratios of 2:1 (horizontal to
vertical) or flatter. Cut slopes are indicated at both 1.5:1 and
' 2:1 slope ratios. Temporary cuts to a maximum height of 11 feet
will be required for retaining wall construction.
t SITE DESCRIPTION
' The subject site consists of a previously graded lot with an
existing residence located in the Olivenhain area of Encinitas,
California. The site is bounded by developed lots to the north
and south, and open space to the west and east.
' Topographically, the site is characterized by the existing
relatively level building pad which is situated on a south
' facing, overall 200+ feet high, 5:1 (horizontal to vertical)
natural slope.
RESEARCH
Previous geotechnical reports were reviewed for the site and
' adjacent sites. The referenced report, by Tri City Engineers,
for the subject property indicated that no geologic hazards were
present and provided conventional grading and foundation
' recommendations for the existing structure. No as -built reports
for the existing structure were located. The referenced Leighton
and Associates report for two lots north of the subject property
' indicate both ancient and recent landsliding exists beneath these
two lots. The limits of the ancient landslide are uncertain but
HETHERINGTON ENGINEERING, INC.
' GEOTECHNICAL INVESTIGATION
Project No. 626.1
February 26, 1991
1 Page 3
are inferred to be roughly contiguous with the north property
line of the subject site. Leighton and Associates further
' concluded that residential development was "feasible provided
mitigation of the existing landslide materials is provided."
Specific mitigation measures were to be provided based on
preliminary development plans. No other reports were found or
reviewed.
SUBSURFACE EXPLORATION
Subsurface conditions were explored by excavating three test pits
' to depths ranging from 10.5 to 13 feet. The approximate
locations of the test pits are indicated on the Geotechnical
Plan, Figure 1. The test pits were excavated using a backhoe.
The excavations were logged by a geologist from our office, who
' visually classified the soil (Unified Soil Classification System)
and bedrock materials, and obtained bulk samples for laboratory
testing. The Test Pit Logs are attached as Figures 3 and 4.
1
LABORATORY TESTING
Laboratory tests were performed on the samples obtained during
the subsurface exploration. Tests performed consisted of the
following:
1. Dry Density /Moisture Content (ASTM: D 1188)
2. Atterberg Limits (ASTM: D 4318)
3. Direct Shear (ASTM: D 3080)
' 4. Expansion (ASTM: D 4829)
1 5. Particle Size Analyses (ASTM: D 422)
Results of dry density /moisture content determinations are
presented on the Test Pit Logs, Figures 3 and 4. The remaining
' laboratory test results are provided on Figures 5 through 7.
SOIL AND GEOLOGIC CONDITIONS
1. Geologic Setting
' The subject property is situated on a portion of the coastal
plain that is generally characterized by a number of
Pleistocene marine terraces and rolling hill type topography
' that descends generally from areas of higher elevation east of
the site down to the present day coastline to the west.
HETHERINGT N ENGINEERING, NGINEERING, INC.
GEOTECHNICAL INVESTIGATION
Project No. 626.1
February 26, 1991
' Page 4
The proposed construction site is underlain entirely by
' disturbed bedrock of the Tertiary age Scripps Formation which
is in turn reportedly underlain at depth by marine sedimentary
bedrock deposits of the Del Mar Formation. A relatively thin
' layer of colluvium overlies the disturbed bedrock.
2. Geologic Units
a. Colluvium - A thin layer of surficial soils consisting of
dry to moist, loose to medium dense, brown clayey sand was
observed in the test pits. These soils were encountered to
' a maximum depth of 2 feet.
b. Landslide Debris ( ?) - The entire site is underlain by
' disturbed bedrock materials of the Scripps Formation.
These materials consist of green -gray sandstone, green
claystone and mottled siltstone, sandstone and claystone.
At this time, clear evidence relevant to the existence or
absence of landsliding has not been observed. Due to the
identified landsliding on property to the north and the
visually disturbed nature of the bedrock materials on -site,
I I, we are currently indicating this material to consist of
slide debris. Remnant bedding and sheared, slickensided
zones were mapped. Additional investigation would be
' necessary to make a more precise determination.
3. Groundwater
No groundwater was observed in the test pits during our
investigation. It should be noted, however, that fluctuations
in the amount and level of groundwater may occur due to
I variations in rainfall, irrigation, and other factors which may
not have been evident at the time of our field investigation.
' SEISMICITY
The site is within the seismically active southern California
region. There are, however, no active or potentially active faults
located within or adjacent to the site. Active faults within the
general site region include the offshore extension of the Newport-
' Inglewood /Rose Canyon and the Elsinore fault zones which lie at
distances of approximately 12 miles and 24 miles, respectively.
Seismic risks on -site are limited to ground shaking during seismic
' events on active faults in the region.
1
' HETHERINGTON ENGINEERING INC.
GEOTECHNICAL INVESTIGATION
' Project No. 626.1
February 26, 1991
Page 5
The table below lists the known active and potentially active
faults which would have the greatest impact on the site.
t Maximum Probable
Earthquake Estimated Bedrock Acceleration
Fault (Moment Magnitude) Peak Repeatable
Newport- Inglewood/
Rose Canyon
(12 miles SW) 6.5 0.30g 0.19g
Elsinore
' (24 miles NE) 7.0 0.188 0.18g
' SEISMIC EFFECTS
1. Ground Acceleration
The most significant probable earthquake event to effect the
property, would be a 6.5 magnitude earthquake on the Newport -
Inglewood /Rose Canyon fault. Potentially, repeatable
horizontal ground acceleration on the order of 0.19g is
possible with a duration of strong ground motion exceeding 20
seconds. Peak (instantaneous) accelerations would be higher.
3. Landsliding
The potential for future landsliding, whether seismically
induced or otherwise is beyond the scope of our authorized
work. Additional investigation, including deep borings both on-
site and off -site, would be necessary to allow for
1 comprehensive analysis.
4. Ground Rupture
' Fault rupture on -site is not likely. However, ground cracks
are possible during future seismic events, throughout southern
California.
CONCLUSIONS AND RECOMMENDATIONS
1 1. General
The proposed construction is feasible from a geotechnical
standpoint. As previously noted, possible ancient landsliding
has been identified within the site area. At this time, the
presence or absence of landsliding on the property has not been
1
' HETHERINGTON ENGINEERING, ER NG, INC.
GEOTECHNICAL INVESTIGATION
Project No. 626.1
February 26, 1991
Page 6
conclusively determined. In order to comprehensively investi-
gate the possible landsliding, deep borings and stability
analyses would be required.
The following recommendations are not intended to mitigate
possible landslide associated ground movements. These
recommendations are intended to create a residential addition
which is compatible with the existing residence. Risk
associated with possible landsliding cannot be evaluated
without further subsurface work.
1 2. Slopes
Cut and fill slopes should be inclined at 2:1 (horizontal to
vertical) or flatter. Temporary slopes to facilitate retaining
wall construction should be inclined at 1:1 (horizontal to
vertical) or flatter.
3. Site Grading
a. Clearing Existing vegetation and miscellaneous debris
1 should be cleared and removed from areas to be graded.
Holes resulting from the removal of buried obstructions,
which extend below finished site grades, should be replaced
with compacted fill.
b. Surface Soil Preparation After site clearing, colluvium
within the limits of proposed fill placement and structural
improvements should be overexcavated. Overexcavation
depths on the order of 2.0 to 3.0 feet are expected.
I ' Cut /fill transitions on the living area and garage building
pads should be eliminated by overexcavation of the cut
portion of the pad to provide a minimum of 3 feet of
1 compacted fill below pad grade. The overexcavation should
extend at least 5 feet beyond the proposed structures.
c. Scarification All areas to receive fill should, after the
required excavations have been made, be scarified to a
minimum depth of 6 to 8- inches, brought to near optimum
moisture content, and compacted to at least 90 percent
relative compaction.
d. Compacted Fill All fill soils should be brought to near
optimum moisture conditions, thoroughly blended to assure
uniform moisture dispersal and compacted in 6 to 8 -inch
thick layers to a minimum of 90 percent of the maximum
density based upon ASTM: D 1557. Oversize (8- inches or
larger) materials should not be incorporated into the fill.
I HETHERIN T
G ON ENGINEERING, INC.
GEOTECHNICAL INVESTIGATION
Project No. 626.1
February 26, 1991
Page 7
Fills constructed on slopes steeper than 5:1 (horizontal to
vertical) should be keyed and benched into bedrock. The
key should have a minimum width of 15 feet and minimum
depth of 5 feet.
' Fill slopes should be overbuilt and cutback followed by
grid rolling to achieve required compaction on the slope
' face.
Subdrain systems will be required behind the fill key and
beneath the canyon fill. These systems should consist of 4-
' inch diameter Schedule 40 perforated PVC pipe placed at the
base of the key or bottom of the canyon, surrounded with a
minimum of 3 cubic feet per lineal foot of crushed rock for
the fill key drain and 9 cubic feet per linear foot of
crushed rock for the canyon drain.
' 3. Foundation and Slab Recommendations
The proposed structure may be supported on conventional
' continuous /spread footings bearing in compacted fill soils.
Footings should extend to a minimum depth of 24- inches into
compacted fill. Footings located adjacent to utility trenches
should extend below a 1:1 plane projected upward from the
inside bottom corner of the trench. All footings should be
reinforced with a minimum of two #5 bars, one top and one
bottom.
1 Footings located adjacent to sloping ground should be extended
to a sufficient depth to provide at least 10 feet of horizontal
' distance between the footing and the face of slope.
Footings bearing as recommended may be designed for a dead plus
live load bearing value of 1500 pounds per square foot. This
value may be increased by one -third for loads including wind or
seismic forces. A lateral bearing value of 250 pounds per
square foot per foot of depth and a coefficient of friction
between foundation soil and concrete of 0.4 may be assumed.
These values assume that footings will be poured neat against
the foundation soils. Footing excavations should be inspected
I by the Geotechnical Engineer prior to the placement of steel to
ensure that they are founded in suitable bearing materials.
An 24 -inch deep grade beam should be placed across the garage
door opening and reinforced as for footings.
HETHERINGTON ENGINEERING, INC.
1 GEOTECHNICAL INVESTIGATION
Project No. 626.1
February 26, 1991
Page 8
' On -grade floor slabs should be at least 4- inches thick and
reinforced with No. 3 bars spaced at 12- inches center to center
' in two directions. Reinforcement should be placed on chairs so
that the reinforcement is in the center of the slab. Floor
slabs should be underlain by 1 -inch of clean sand over a 6 -mil
1 visqueen moisture barrier over 4- inches of rounded gravel or
clean sand.
Slab subgrade soils should be presaturated to 5% over optimum
' moisture content to a depth of 24- inches and verified by the
Geotechnical Engineer prior to pouring concrete.
' 4. Retaining Walls
Retaining walls free to rotate (cantilevered walls) should be
designed for an active pressure of 45 pounds per cubic foot,
equivalent fluid pressure, assuming level backfill consisting
of the on -site soils. Walls with a 2:1 (horizontal to
vertical) surcharge should be designed for an active pressure
' of 60 pounds per cubic foot, equivalent fluid pressure,
respectively.
' Walls restrained from movement at the top should be designed
for an additional uniform soil pressure of 8xH pounds per
square foot where H is the height of the wall in feet. Any
additional surcharge pressure behind the wall should be added
1 to these values.
Retaining wall footings may be founded in compacted fill and /or
' terrace deposits and should be designed in accordance with the
previous building foundation recommendations.
Retaining walls should be provided with adequate drainage to
'1 prevent buildup of hydrostatic pressure and should be
adequately water - proofed.
5. Trench and Retaining Wall Backfill
All trench and retaining wall backfill should be compacted to
at least 90 percent relative compaction (ASTM: D 1557) and
tested by the geotechnical consultant.
' 6. Site Drainage
The following recommendations are intended to minimize the
potential adverse effects of water on the structure and
appurtenances.
a. Consideration should be given to providing the structure
with roof gutters and downspouts.
HETHERINGTON ENGINEERING, INC.
GEOTECHNICAL INVESTIGATION
Project No. 626.1
February 26, 1991
Page 9
b. All site drainage should be directed to the street and not
' allowed to flow over slopes.
C. No landscaping should be allowed against the structure.
Moisture accumulation or watering adjacent to footings can
result in deterioration of wood /stucco and may adversely
effect footing performance.
d. Irrigated areas should not be over - watered. Irrigation
should be limited to that required to maintain the
vegetation. Additionally, automatic systems must be
' seasonally adjusted to minimize over - saturation potential
particularly in the winter (rainy) season.
e. All slope, yard, and roof drains should.be periodically
checked to verify they are not blocked and flow properly.
This may be accomplished either visually or, in the case of
subsurface drains, placing a hose at the inlet and checking
the outlet for flow.
7. Grading Plan Review
' Final grading and foundation plans should be reviewed by the
geotechnical consultant to confirm conformance with the
recommendations presented herein or to modify the
recommendations as necessary.
LIMITS OF INVESTIGATION
The analyses, conclusions and recommendations contained in this
report are based on site conditions as reported by others and as
they existed at the time of our investigation, and further assume
the excavations to be representative of the subsurface conditions
throughout the site. If different subsurface conditions from those
' encountered during our exploration are observed or appear to be
present in excavations, the Soils Engineer and Geologist should be
promptly notified for review and reconsideration of
' recommendations.
Our investigation was performed using the degree of care and skill
ordinarily exercised, under similar circumstances, by reputable
' Soils Engineers and Geologists practicing in this or similar
localities. No other warranty, express or implied, is made as to
the conclusions and professional advice included in this report.
HETHERINGTON ENGINEERING, INC.
GEOTECHNICAL INVESTIGATION
Project No. 626.1
February 26, 1991
' Page 10
' This opportunity to be of service is sincerely appreciated. If you
have any questions, please call.
' Sincerely,
HETHERINGTON ENGINEERING, INC.
PAUL A. BOGSETHS
RIM
Certified Engine ing Geologist 1153 Civ' er 30488
' (expires 6/30/92) Geotechnica/l Engineer 397
(both ex 92)
MDH PAB ss
' cc: 6 Address �f
Attachments' �; �� +� No. 397
s.� E.G. 1153
` M
OF mW
HETHERINGTON ENGINEERING, INC.
' REFERENCES
Landslide Hazards in the Rancho Santa Fe Quadrangle, CDMG OFR 86-
' 15LA, 1987.
"Report of Soil Investigation for APN 264- 160- 32...," by the Tri-
' City Engineers, dated January 4, 1982.
"Supplemental Geotechnical Evaluation, Proposed Two Lot Residential
Subdivision, 2920 Lone Jack Road...," by Leighton and Associates,
Inc., dated June 25, 1990.
' AERIAL PHOTOS
Flight SDPD, June 17, 1974
' Flight AXN, 1953 -1959
' HETHERINGTON ENGINEERING IN
, . _ C
1�
1
1
EGEND
1
'ROXI MATE LOCATION
1 % TEST PI T
ti KE AND DIP OF BEDDING
1 LIKE AND DIP OF SHEAR p
Z
W
k )LOGIC CROSS SECTION Z
1 w
i y ti
W
1 � t
h Q 0
_ IL
IL
1 r
W
1 L
r 1-' Z H co
i 0 EE
W W a
U W
1 Z
0�
Z z
ORTH
1 WO
U
LE: 1's Z 32' J
O v
1 �z
Z =
� U
1 WW
2 0
F— O
W W
= t7
1
' 234 234
218 EXISTING LIMITS OF 218
RESIDENCE PROPOSED ADDI TI ON
' 202 - 202
TP -1
186 '�� -- - - -� _ TP- 2 186
l rj -
170 PROPOSED GRADE U 170
' 154 154
A TREND N 10W A'
' GEOLOGIC CROSS SECTION
HETHERINGTON ENGINEERING I FROST RESIDENCE
GEOTECHNICAL CONSULTANTS
PROJECT NO. 828.1 I FIGURE NO. 2
' BACKHOE COMPANY: Bob Welch BUCKET SIZE: 18" DATE: 1/24/91
w ¢ cn
F W
J H H ,� w w SOIL DESCRIPTION
C <E z W M z 0. H z X H W TEST PIT NO. TP -1 ELEVATION: 194
' o�' ¢¢ww 0w a oo� o�
F- O 0 � E U � (A �
0 SC COLLUVIUM Brown clayey fine sand, dry to moist, loose to
medium dense, desiccated in upper one foot
' SLIDE DEBRIS(?) Orange and light gray silty fine sandstone,
moist, loose to medium dense, several (approximately 6 inch)
zones of brown silty sand, friable
' S
...................................................................................................................... ...............................
Gray silty claystone, moist, firm to stiff, caliche blebs,
93 24.4 mottled zones with numerous micro - slicks, variable consistency,
yellow and rust staining along fractures
@ 6 feet (middle of trench): general contact of sandstone and
10 claystone: N65E /25NW
' @ 6.5 feet (south side): general trend of yellow sand laminae
(not continuous): N45E /23NW
@ 7 fLiandstone, t (south side): general trend of 1/4" olive green silt
not continuous): N40E /25NW
............................................................................................................. ..............................:
' (middle of trench): light gray silty fine to medium
15 moist, medium dense
Total depth: 12.5 feet
' No groundwater
No caving
' 20
TEST PIT NO. TP -2 ELEVATION: 181
0
' SC COLLUVIUM Brown clayey sand, dry to moist, loose to medium
dense, desiccated in upper one foot
SLIDE DEBRIS(?) Green, light gray, and orange silty fine
sandstone, moist, loose to medium dense, friable
5 @ 4.5 feet: grades to claystone, moist, firm, numerous micro -
slicks
...................................................................................................................................... ...............................
t Light gray silty fine to medium sandstone, moist, dense, friable,
(fades out halfway through trench, other half of trench is
claystone)
.....................................................................-............................................................... ..............................:
' 10 Green clay and claystone, moist, firm to stiff, fractured,
numerous micro - slicks, blebs of sandstone, variable consistency
@ 7 feet: general trend of contact: N28E /10NW
@ 8 feet (south side): orange and light gray silty fine sandstone
:........... _ .......................... ............................... _.................. _............................................ ..............................:
' Grades to light gray and orange sand and sandstone, moist,
loose to medium dense, several roots
:...................................................................................................................................... ..............................:
15 Green claystone, moist, stiff
' @ 12.5 feet: Approximately 1/2" thick remolded clay seam,
olive green clay, very moist, soft, several slick surfaces,
N80E /05NW, N -S /25E
' Total depth: 13 feet
20 — No groundwater, No cavin
' LOG OF TEST PITS
HETHERINGTON ENGINEERING Frost Residence
' GEOTECHNICAL CONSULTANTS PROJECT NO. 626 I FIGURE NO. 3
t BACKHOE COMPANY: Bob Welch BUCKET SIZE: 18" DATE: 1/24/91
vi I
W ¢ cis
.-. J H i ., w SOIL DESCRIPTION
W 0r- (n >Z U HZ�. H
m N o � o wo a = U , N TEST PIT NO. TP -3 ELEVATION: 179
0 SC COLLUVIUM Brown clayey fine sand, dry to moist, loose to
medium dense, desiccated in upper one foot
' SLIDE DEBRIS( ?) : Light gray and green clayey to silty fine
sandstone, moist, medium dense, friable; zones of dense green
sandstone, several concretions
' S
.............................................................................................................................. ...............................
@ 6 feet (nort h side): green cIaystone and sandstone with
light gray and orange friable sand lenses, moist, firm and
medium dense to dense
10 @ 9 feet (north side): concretions, appear to be fractured,
surrounding sand and clay matrix appears glazed at one
' location (concretions @ 5 feet on south side of hole)
Total depth: 10.5 feet
No groundwater
No caving
15
t 20
1
LOG OF TEST PITS
' HETHERINGTON ENGINEERING Frost Residence
' GEOTECHNICAL CONSULTANTS PROJECT NO. 626 I FIGURE NO. 4
3000
2500 .................. . ..... ....... ........... ............................................................ .................................. ....................................
....................................
2000 .............. ... ................ ................ ................... .................................... ..... . .... ....... . .............. :
....... ..............................> ... ... .........................
4-
CD
Z 1500 ........................................................................ .......................... ....... . ................................... ....................................
.......................... .......
Cn
Cn
w
1000 .................. .......... i ........................ ......
.....................
................... ...............................
•
500 ................ ... .............. ......................... . .............................. ......... .......... ......... ....................................
0
0 500 1000 1500 2000 2500 3000
NORMAL PRESSURE (psf)
SYMBOL SAMPLE LOCATION COHESION FRICTION ANGLE REMARKS
' • TP-1 at 7.0 200 23 remolded to in-situ density,
saturated, drained
DIRECT SHEAR TEST RESULTS
HETHERINGTON ENGINEERING Frost Residence
GEOTECHNICAL CONSULTANTS PROJECT NO. 626.1 I FIGURE NO. 5
' U.S. STANDARD SIEVE SIZES HYDROMETER
3 1 3/4 3/8 4 8 16 20 30 40 50 100 200
100 100
............ .... ....... ......`:...................
.......
....:.... .
E
i
..: ............ :
go
80 .... ............................... ...... ... _ ... __ _ _....
E
:.. ...E....:....
70 ...........................t ......... ...... .. _ ... _ .. .. _ ....... _ .... 0
s .. .
t
..:... ....:.....
W .... ....... .....................t......... _ ... _ _ .. _ ....... _ .... ......... 60
W
Z
Z
H .........
ILL
H
<L
Z 50 ...................... `.....:......... ...... _ _ _ _ _ .... Z
' W W
U U
L
W
LLJ
.. ...:....
............
0
20 .. ............. `:.... ... s...s...€ ....... _ _ _ _ ....... _ .... .. ......
...:....:.
10 ............... .... ... ........ ...`......_ ...... _ . _ _ _ _ .... .. ...... 0
.......[........
......:....
0 0
' 100 10 1 0.1 0.01 0.001
GRAIN SIZE (mm)
' COBBLES GRAVEL SAND
Coarse Fine Coarse Medium Fine SILT and CLAY
t
SYMBOL SAMPLE LOCATION FIELD % PASSING % FINER UNIFIED SOIL
MOISTURE ( %) NO. 200 SIEVE 2 MICRONS CLASSIFICATION
' TP -3 at 4.0 34
' GRADATION TEST RESULTS
HETHERINGTON ENGINEERING Frost Residence
' GEOTECHNICAL CONSULTANTS PROJECT NO. 626.1 I FIGURE NO. 6
1 '
t LABORATORY TEST RESULTS
Expansion
(ASTM: D 4829)
' Expansion Expansion
Sample Location Index Potential
' TP -1 @ 7' 113 High
TP -3 @ 4' 62 Medium
ATTERBERG LIMITS
(ASTM: D 4318)
Unified
' Sample Liquid Plastic Plasticity Soil
Location Limit Limit Index Class
' TP -1 @ 7 44 21 23 CL
' Project No. 626.1
Figure No. 7
I'
1 1 ' _
�o
Jai es A. Laret, P.E. i Dana M. Seguin, P.L.S.
LAND DEVELOPMENT ENGINEERING • PLANNING • SURVEYING
Client No. 251
0V D
3 1J%
City Engineer vIG6
City of Encinitas ENGIN EERING S NR AS
505 S. Vulcan Avenue 61V GF ENG
Encinitas, CA 92024 -3633
FINAL GRADING ENGINEER'S REPORT FOR FROST RESIDENCE
GRADING PERMIT NO. 1170 -G
Pursuant to section 23.24.310 of, the Encinitas Municipal Code, this letter report is hereby
submitted as a final grading report for the subject project. As supervising grading
engineer on the project, I hereby state all grading, lot drainage, and drainage facilities on
the site have been completed and installed in conformance with the approved plans and
requirements of the City of Encinitas Codes and Standards.
I have inspected the site and found the embankment and cut slopes to have been cut to
their proper line and grade in conformance with sections 23.24.450 through 23.24.500.
All building pad sizes, elevations, drainage and berming have been completed in
substantial compliance with the approved plans and any approved revision thereto.
In addition, in my professional opinion, all work incorporated in the landscape and
irrigation plans authorized under the P ermit have been constructed in accordance with
the approved plans, any approved revisions thereto and Section 23.24.510 of the
Encinitas Municipal Code.
An "As- Built" grading plan has been corn pteted ' T r or under my direction and has
been submitted to the City for review aKd `p rQva( N. ,
A t,
Ja es A. Laret, RCE 29W
5708 Calzada Del Bosque • (619) 756 -9374
P.O. Box 9661, Rancho Santa Fe, CA 92067 • Fax (619) 756 -4231
' AS- GRADED GEOTECHNICAL REPORT
Proposed Building Addition
and Appurtenances
' 2926 Lone Jack Road
Encinitas, California
�1
1
1
' 3
NOV 1 1991
' CITY OF ENCINITAS
DEPT. OF PUBLIC WORKS
ENGINEERING DEPT.
HETHERINGTON ENGINEERING, INC.
HETHERINGTON ENGINEERING, INC.
GEOTECHNICAL CONSULTANTS
' October 31, 1991
Project No. 626.1
' Mr. Thomas Frost
4255 Ocean Blvd.
' San Diego, CA 92109
Subject. AS- GRADED GEOTECHNICAL REPORT
Proposed Building Addition and Appurtenances
' 2926 Lone Jack Road
Encinitas, California
' References: Attached
' Dear Mr. Frost:
In accordance with your request, we have performed geotechnical
services in conjunction with grading at the subject site. The
' grading was conducted in September and October 1991. The purpose
of the grading was to create building pad areas for the proposed
building addition and appurtenances in a manner consistent with the
' existing structure. As discussed in Reference 4, the grading was
not intended to mitigate possible future damage due to landslide
associated ground movement. Our services consisted of compaction
testing and observation of grading, geological observations,
' laboratory testing and the preparation of this report which
presents the results of our testing and observations, and our
conclusions and recommendations.
SITE GRADING
' Prior to grading, the site was cleared of surface obstructions,
vegetation and debris. In areas to receive fill, existing
colluvium was removed. The exposed materials were scarified to a
depth of 6 to 8- inches, brought to near optimum moisture conditions
and recompacted to at least 90 percent relative compaction as
determined by ASTM: D 1557A. The approximate elevations of the
' bottoms of the removals are indicated on the accompanying Plot
Plan, Plate 1.
1 Fill placement occurred over the southeastern portion of the site
to create building pad areas for the proposed addition and
appurtenances, and over the southwestern portion of the site to
create a level "play yard" area. The limits of fill placement are
' shown on the Plot Plan, Plate 1.
A fill key was constructed at the south end of the "play yard"
' fill. A backdrain was constructed along the bottom of the fill key
I '
5245 AVENIDA ENCINAS • SUITE G • CARLSBAD, CALIFORNIA 92008 • (619) 931 -1917
' AS- GRADED GEOTECHNICAL REPORT
Project No. 626.1
October 31, 1991
Page 2
' as shown on the Plot Plan, Plate 1. The backdrain consisted of a fl-
inch diameter perforated schedule 40 PVC pipe surrounded by 9 cubic
1 feet per lineal foot of 3/4 -inch crushed rock wrapped in filter
fabric. A 66 foot long, 12 -inch diameter, corrugated metal pipe
was installed along the western side of the site. Extending from a
grated inlet at the northwest corner of the property and entering
the "play yard" fill at a second grated inlet, the drain daylights
into 6 to 12 -inch diameter rock at the toe of the 2:1 (horizontal
to vertical) fill slope. We understand that the final as- graded
pad elevation for the "play yard" fill was approximately 4 feet
higher than the elevations shown on the referenced "Grading
Plan..." (Reference 6).
' A fill key was also constructed along the southeast corner of the
fill pads for the proposed addition and appurtenances as shown on
the Plot Plan, Plate 1. Overexcavations on the order of 3 feet
' deep were performed in the areas of the building addition to
eliminate cut /fill transitions.
SOIL TYPES
The soils utilized as fill consisted of on -site materials generally
1 composed of light red -brown silty sand, gray -green silty clay,
green -brown sandy clay and red - orange slightly clayey silty sand.
FILL PLACEMENT
Fill soils were laced in 6 to 8 -inch
P thick, near horizontal lifts,
moisture conditioned to near optimum moisture content, and
compacted by mechanical means to a minimum of 90 percent relative
compaction as determined by ASTM: D 1557A. Compacted fill was
benched into temporary 1:1 cut slopes at the margins of the
removals. Compaction was achieved by track rolling with a
' Caterpillar D4H dozer and a Caterpillar 963 loader. Fill was
placed in general accordance with the geotechnical guidelines
presented in Reference 4.
' Density tests were performed in accordance with ASTM: D 1556 (Sand -
Cone Method) and ASTM: D 2922 (Nuclear Guage Method). The results
' of the density tests are presented on the attached Summary of Field
Density Tests, Table I. The approximate locations of the field
density tests are indicated on the accompanying Plot Plan, plate
' 1. Optimum moisture content /maximum dry density determinations of
soils utilized as fill are presented on the attached Summary of
Maximum Dry Density /Optimum Moisture Content Determinations, Table
II.
HETHERINGTON ENGINEERING, INC.
' AS- GRADED GEOTECHNICAL REPORT
Project No. 626.1
October 31, 1991
Page 3
GEOLOGIC OBSERVATIONS
Geologic mapping performed during grading at the subject site and a
review of geotechnical reports for properties in the site vicinity,
further support the possibility that a landslide or remnants of a
' landslide exist on your property. Geologic structure observed in
temporary cut slopes during site grading indicate. bedding generally
strikes N70 -80 degrees E and dips to the north at 25 to 40
degrees. Bedding attitudes were obtained on sand lenses and
layers, within siltstone and claystone beds. Geologic attitudes
and locations are available in our files. In order to
' comprehensively investigate the possible landsliding, deep borings
and stability analyses would be required.
CONCLUSIONS AND RECOMMENDATIONS
1. General
' Based on our observations and the results of our testing, it is
our opinion that the subject grading has been performed in
' general conformance with the recommendations contained in
Reference 4.
The grading and following foundation recommendations are not
intended to mitigate possible landslide associated ground
movements. The recommendations are intended to create a
residential addition and appurtenances which are consistent
' with the existing residence. Risk associated with possible
landsliding cannot be evaluated without further subsurface
work.
' 2. Foundation and Slab Recommendations
The proposed structure may be supported on conventional
' continuous /spread footings bearing in compacted fill soils.
Footings should extend to a minimum depth of 24- inches into
compacted fill. Footings located adjacent to utility trenches
' should extend below a 1:1 plane projected upward from the
inside bottom corner of the trench. Footings located adjacent
to sloping ground should be extended to a sufficient depth to
provide at least 10 feet of horizontal distance between the
' footing and the face of slope. Continuous footings should be
reinforced with a minimum of two #5 bars, one top and one
bottom.
' HETHERINGTON ENGINEERING INC.
AS- GRADED GEOTECHNICAL REPORT
' Project No. 626.1
October 31, 1991
Page 4
'
Footings bearing as recommended g q may be designed for a dead plus
live load bearing value of 1500 pounds per square foot. This
' value may be increased by one -third for loads including wind or
seismic forces. A lateral bearing value of 250 pounds per
square foot per foot of depth and a coefficient of friction
' between foundation soil and concrete of 0.4 may be assumed.
These values assume that footings will be poured neat against
the foundation soils. Footing excavations should be inspected
' by the Geotechnical Engineer prior to the placement of
reinforcing steel to ensure that they are founded in suitable
bearing materials.
' A 24 -inch deep grade beam should be placed across the garage
door opening and reinforced as for footings.
' On -grade floor slabs should be at least 4- inches thick and
reinforced with No. 3 bars spaced at 12- inches center to center
in two directions. Reinforcement should be placed on chairs so
that the reinforcement is in the center of the slab. Floor
' slabs should be underlain by 1 -inch of clean sand over a 6 -mil
visqueen moisture barrier over 4- inches of rounded gravel or
clean sand.
Slab subgrade soils should be presaturated to 5% over optimum
moisture content to a depth of 24- inches and verified by the
' Geotechnical Engineer prior to pouring concrete.
3. Retaining Walls
' Retaining walls free to rotate (cantilevered walls) should be
designed for an active pressure of 45 pounds per cubic foot,
equivalent fluid pressure, assuming level backfill consisting
' of the on -site soils. Walls with a 2:,1 (horizontal to
vertical) surcharge should be designed for an active pressure
of 60 pounds per cubic foot, equivalent fluid pressure,
respectively.
Walls restrained from movement at the top should be designed
for an additional uniform soil pressure of 8xH pounds per
' square foot where H is the height of the wall in feet. Any
additional surcharge pressure behind the wall should be added
to these values.
' Retaining wall footings may be founded in compacted fill and /or
terrace deposits and should be designed in accordance with the
' previous building foundation recommendations.
' HETHERINGTON ENGINEERING, INC.
1
' AS- GRADED GEOTECHNICAL REPORT
Project No. 626.1
October 31, 1991
Page 5
Retaining walls should be provided with adequate drainage to
prevent buildup of hydrostatic pressure and should be
adequately water - proofed.
4. Trench Backfill
' All trench backfill should be compacted to at least
P 90 percent
relative compaction and tested by the Geotechnical Engineer
' during placement.
5. Site Drainage
' The following recommendations are intended to minimize the
potential adverse effects of water on structures and
appurtenances.
a. Consideration should be given to providing structures with
roof gutters and downspouts;
' b. All site drainage should be directed away from structures
and not allowed to flow over slopes;
' C. No landscaping should be allowed against foundation
structures. Moisture accumulation or watering adjacent to
foundations can result in deterioration of wood /stucco and
' may effect foundation performance;
d. Irrigated areas should not be over - watered. Irrigation
1 should be limited to that required to maintain the
vegetation. Additionally, automatic systems should be
seasonally adjusted to minimize over - saturation potential
' particularly in the winter (rainy) season;
e. All slope, yard, and roof drains should be periodically
checked to verify they are not blocked and flow properly.
' This may be accomplished either visually or, in the case of
subsurface drains, placing a hose at the inlet and checking
the outlet for flow.
' HETHERINGTON ENGINEERING, INC.
' AS- GRADED GEOTECHNICAL REPORT
Project No. 626.1
October 31, 1991
' Page 6
' LIMITATIONS
Our testing and observation was performed using the degree of care
' and skill ordinarily exercised, under similar circumstances, by
reputable Geotechnical Consultants practicing in this or similar
localities. No other warranty, express or implied, is made as to
the conclusions and professional advice included in this report.
' If there are any questions regarding this report, please feel free
to call. We appreciate this opportunity to be of service.
' Very truly yours,
HETHE IN O G RING, INC.
,0 c M E ERI
D G PAUL A. BOGSETH A• Bp
' En r 80 10 # Certified Engine, Geologis� J 3
Geotechnic En "#$'7 c;,. (expires 6/30/ E.G. 11
(both expir ti /92)
Rio. 397 �P� Ea.o.____,_w_•
J
I '3
"_ �ql�. �✓ �
�➢ , y ,L' 4 '� CHRIS HOSKIN '`e•\�OF CALW �
r
� s � Staff Engineer
HETHERINGTON ENGINEERING, INC.
' REFERENCES
1) Landslide Hazards in the Rancho Santa Fe Quadrangle, CDMG OFR
' 86 -15LA, 1987.
2) "Report of Soil Investigation for APN 264- 160- 32...," by the
' Tri -City Engineers, dated January 4, 1982.
3) "Supplemental Geotechnical Evaluation, Proposed Two Lot
Residential Subdivision, 2920 Lone Jack Road.... 11 by Leighton
and Associates, Inc., dated June 25, 1990.
4) "Geotechnical Investigation, 2926 Lone Jack Road, Encinitas,
California," by Hetherington Engineering, Inc., dated
February 26, 1991.
5) "Preliminary Geotechnical Investigation, 2916 Lone Jack Road,
' Encinitas, California," by Ninyo & Moore, dated March 9,
1989.
' 6) "Grading Plan for Frost Residence," by James A. Laret, dated
March 13, 1991.
! 7) Aerial Photos Flight AXN, 1953 -1959
Flight SDPD, June 17, 1974
HETHERINGTON ENGINEERING, INC.
' TABLE I
SUMMARY OF FIELD DENSITY TESTS
(ASTM: D 1556)
' Comments and Moisture Dry Relative
Test Test Test Elevation Content Density Soil Compaction
No. Date (MSL) (-%) (-%) Test ( %)
1 9/23/91 153.5 19.9 103.5 2
90
2 9/23/91 154.5 17.1 109.5 1 94
' 3 9/24/91 157.0 15.7 116.5 3 91
4 9/25/91 165.0 19.4 107.7 3 92
5 9/26/91 163.0 16.4 104.6 3 90
6 9/26/91 167.0 14.1 105.1 1 90
7 9/26/91 170.0 15.4 104.3 3 90
8 10/10/91 170.0 16.2 101.0 2 88
(Failed)
' 9 10/10/91 170.0 16.3 103.4 2 90
(Retest of 8)
10 10/10/91 166.5 11.8 107.2 1 92
' 11 10/10/91 186.5 16.1 101.9 4 85
(Failed)
12 10/10/91 185.5 15.6 99.9 '4 83
' (Failed)
13 10/14/91 186.0 19.8 104.6 2 91
(Retest of 11 & 12)
14 10/14/91 189.0 17.0 110.3 1 92
' 15 10/15/91 190.0 12.1 100.0 1 85
(Failed)
16 10/15/91 170.0 18.5 107.1 1 92
17 10/16/91 171.5 16.4 104.5 3 90
18 10/16/91 F.G. 19.3 104.9 1 90
19 10/16/91 189.0 19.2 108.8 5 92
' 20 10/16/91 190.5 19.0 110.5 4 92
(Retest of 15)
21 10/18/91 F.G. 17.4 108.2 4 90
22 10/18/91 174.5 20.5 106.3 2 92
' 23 10/21/91 175.5 21.4 104.8 2 91
24 10/22/91 173.5 17.2 106.2 5 90
25 10/23/91 178.5 18.4 105.4 3 90
1
' TABLE II
Maximum Dry Density /Optimum Moisture Content Determinations
' (ASTM: D 1557A)
' Optimum
Maximum Dry Density Moisture Content
Soil Type Soil Description (pcf) (o)
1 Light red -brown silty sand 117.0 13.0
' 2 Gray -green silty clay 115.0 16.0
III' 3 Red -brown silty sand with 116.5 13.5
gray -green silty clay
4 Green and brown sandy clay 120.5 12.5
t 5 Red - orange slightly clayey 118.0 13.0
silty sand