UNITED STATES DEPARTMENT OF THE INTERIOR GEOLOGICAL … · 2010-11-19 · united states department...
Transcript of UNITED STATES DEPARTMENT OF THE INTERIOR GEOLOGICAL … · 2010-11-19 · united states department...
UNITED STATES DEPARTMENT OF THE INTERIOR
GEOLOGICAL SURVEY
MAP SHOWING LANDSLIDES AND RELATIVE SLOPE STABILITY OF QUATERNARY
DEPOSITS OF THE LOWER SKAGIT AND BAKER VALLEYS, NORTH CASCADES
WASHINGTON
By
Paul L. Heller
Open-File Report
79-963
This report is preliminary and
has not been edited or reviewed
for conformity with Geological
Survey standards or nomenclature
MAP SHOWING LANDSLIDES AND RELATIVE SLOPE STABILITY OF QUATERNARY
DEPOSITS OF THE LOWER SKAGIT~AND BAKER VALLEYS, NORTH CASCADES,
WASHINGTON
by Paul L. Heller
Appendix A Landslide Data
Data for landslides lettered on the.landslide location map is given in the following table. Landslides are listed sequentially by the six characters used to locate the slides on the landslide location map (example: 36-8-15A
36 = 36 North
8 = Range 8 East
15 = Section 15
A = label found on landslide in section 15).
Information given includes:
SLIDE TYPE
DATA SOURCE - codes are:
FLIGHT CODE SCALE YEAR OWNER
1
2
3
= CWD-R
= NW-69
= NW-C-76
1:20000
1:12000
1 : 24000
1956
1969
1976
Agricultural Stability and Conservation Service (USDA)
Washington State Department of Natural Resources
Washington State Department ofNatural Resources
4 = On site investigation 1976-1977
WIDTH - width at widest part of slide (usually slide's head) in meters.
LENGTH - slide length in meters. * denotes slide and fTowage length combined.
SLOPE - in degrees. Codes are: A = estimated from air photo (within 5 )
B - measured on site
C = estimated on site (within 5 )
D = minimum slope angle
VRT = near vertical slope
Appendix A (Cont.)
AREA - minimum area which failed in square meters. If length is * then value equals the minimum area which failed plus the minimum area damaged by slide debris.
CAUSES - factors contributing towards slope failure, presented in order of decreasing importance. Codes are:
A » ground water perched at impermeable boundary
B = steep slope angle
C = stream undercut
D = failure of previous landslide debris
E = loading
F = road construction, cutting and filling
6 » deforestation
DAMAGE - damage done to:
D = drainage
R = road
P = property
SLIDE I.n.
SLIDE
DATA
WIDTH
LENGTH
SLOPE. AREA
CAUSES
DAMAGE
TYPE
> 35-5-11 -A
DEBRTS
1 2?
*159FLOW
'1 '
B
1 35-5-13-A
DSBRJ8
1 45
?2 27
| '
FLO'*!
. '
1 .
L B
> 35-5-13-A
DEBRIS
* 15
30 22
D -
FLOW
ii '
'' -
- B
i 35-5-13-0
SLUMP 4
20 5
26
i
P
35-5-13-C
DEBRIS
1 <<$
45
30 FLOW
t
3510
IMAYUE NOT A
SLIDE.
510 R
SEE OH
SITE
INVESTIGATION.
CROWN AT
OLD ROAO.
750 A,D,F
R,d
2 OLD SLIDES HAVE
TAKEN PLACE MERE.
OLD ROAD DEBRIS IN
SLIDE.
F R
DEBITS SPILLS O^
TO PT.
20 . WOAO
AT GROWN OF
SLIDE.
1S30
CROWN AT
POWER
LINE CUT.
35-5-14-A SLUMP
FLOWV*
830
60 F.A
DIRT ROAD /ABOVE
SLIDE CKQWN.
AUIQW HORE WATER
TO SATURATE SLIDE
AREA.
i '
i)i *.., . «
|!i ' lr-
5! ai
SL2.OCJ
u> C5<£ 2.<c0
COUJCO
<c u
1!
! < ! UJQl<T
1 U.1 £. i ^_i __
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<i
COO
143
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~^-c^ -»»^5UlQ
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fOra
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a. 2:^30_J_J</JU_
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149
1mi*7
oz i - 4tCTl/> UJC-ZQtCCtujf- JcoXt/7
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\ t- ox0*-
«al<.00flfoJt-a*."3 .
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od
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u.
otoow
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.>-*3C
>
cO fU
?
"5
<n.»-*ut ao
S3O07
-*1 ^
143
1mP>
SLTOF T.n.
SI.IHF OATA
WIDTH LFvniH
sLOpr AREA
CAUSES DAMAGE
COWFA/T FYPF
SOURCE
&35-6- 23-A
DEBRIS' 3
85 99
40 5180
8,C SLIDE
35-6-23-B
HEBRTSl
3 l 85
31 ?080
B,C SL1.DE
|f
1 0
35-6-23-C
DEBRIS
3 ?5
31 40
780 B,C
SLIDE
D 35-6-27-A
DEBRIS 1
61 ??
40 1390
8.C SLIDE
i onjnrw; ROAD AT
HEAD OF SLIDE.
DAMAGED IF
FUTURE
FAILURE.
I QGHTMr; PQAD AT
HEAD OF SLIDE.
. DAMAGED IF
FUTURE
FAILURE.
i i
UNDERCUT BY
STREAM.
35-6-28-A
DEBRIS
SLIDE1
1i45200
6.CUNDERCUT BY
STREAM. SLIOE AT
EDGE. OF TERRACE.
SLIDE i.o.
SLT.DF DATA
WIDTH LENGTH
SLOPE AREA
CAUSES DAMAGE
COMMENTTYPE
SOURCE
D 35-6-2Q-B
DEBRIS
? 192
56 45
6960
B.C
AVALANCHE
35-7-01-A
DEBRIS
j ,»
45 91
3600
SLIDER
35-7-02-A
DEBRIS
1 1 llf
22
35
2600
* SLIDE
3S-7-02-8
DEBRIS
1 91
6&
5^0
B,C
SLIDE
ii
i
B 35-7-02-B
DEBRIS
^
50
C.8
SLIDE
UNDERCUT. BY
STREAM. SLIDE AT
EDGE OF TERRACE.
LANDSLIDE A/H.A.
DATA FOR A
SINGLE
/MEMBER.
J LANDSLIDE ARFA
JUST BELOW TERRACE
EDGE. CAUSFD BY
ROAD CUT ?
a SMALL RECENT
SLIDES WITHIN THIS
LANDSLIDE AREA
UNDERCUT BY
STREAM.
STREAM UNDERCUTS
BANK, MATERIAL
SPALLS OFF.
,..,>
301
is
v IO
N a9
Avtf
on
n i
MO
ldd.
wms
v-9o
-z-S
f
NV
N
Qd
iQ
Naa
nsoN
viV
flQd
VIV
O9
09
60
1
Off
99
a3Q
11S
51^9
30
9--h
O-A
-bf
Ban
sN
V ^ V
ION
NV
lV
l\/a
i O
SS
tl
Ot7
(6a
3Q
HS
S
Idfl3
CJ
Oft
ahns
JO
QV
3Hxv
\f3
ui
aans
aiM
Vl
3H3N
V1V
AV
30V
WV
OH1
0N31
H
i.om
vi
va3d
Ai
sons
a'i
san
s
SLTDF T.D
SLIDETYPE
DMA
SOURCE
W]D
SLOPE
AREA
CAUSES
DAMAGE
COMMENT
35-7-09-A
3550
35A,B
RUYLE SLIDE.
DEBRIS AVALANCHt
r?) AT
TERRACE
EDGE. SLUMP BLOCKS
f?1 ALSO.
35-7. 10-A
SLIDE8
4I6
3?15060
6LNDSLIDE AKEA
35-7-2?. A
/H7?0
F,B
35-7-24-A
DEBRIS
SLIDE
9tA
50 ^0
32X0
DATA ON
LARGEST OF
4- SLIDES AT
LOCATION.
DEBRIS
SLIDE
D34
30750
APEA MAY HAVE BEFAl
PREVIOUSLY LOGGED.
35-8-02-A
SLUMP
30070
35 !'
C'F.A
P.RLOWER BAKEP DAM
SLIDE.
POWEP
MOUSE DESTROYED.
TREMENDOUS
**i > p»»
SLIDE T.D.
SLIOF
OAIA
VTDTH
IFMRTM
SI OPE
APFA
CAUSFS
DA^AGF. .
. TYPF
SOMRCF
35-8-03-A
35-8-05-A
35-8-05-0
35-8-07-A
35-a-U-A
DEBRIS 1
91 68
40 SLIDE
UNKNOWN 1
« t
, «
DEBRIS 1
SLIDE
' *
D DEBRIS
2 27
48 20
FLOW
B SLUMP
I 4
90 90
36
FLOW
. r-
8 LANDSLIDE AREA AT
VERY STEFP HEAD OF
STREAM GULLY.
2 SMALL
RECEHT
! j
SLIDES WITHIN THIS
' LANDSLIDE.
AREA-
t030 MAYBE SOME OTHEH
/ TYPE.
OF LANDSLIDE.
'
A.F R
FLOWED ON TO ROAD
QELQW.
35-8-11-8FLOW
1120
590 A
AL FLOWED
STREAK
GULLIES.
SLIDE 1.0.
SLIDF
TYPF
HATA
VI1DTH
LFMRTM
S1.HPF SOURCE
ARFA
CAUSES
35-8-1 1-C
35-8-1 1-D
35-8-1 i-A
35-8-ia-B
35-8-1 a-C
D MUD
3 57
71 25
FLOW
MUD
3 28
37
* D
MUD
1 fc
6ft 20
FLOW
A DEBRIS
1 30
FLOW
* A
SLUMP
3 85
1\15 30
FLOW
M
28-10 A
D
520
A D
270
MATERIAL FLOWED
DOWN STREAM
r '. GULLIES.
i
LANDSLIDE AREA.
SFFM TQ BE
, /"UDFLOWS.
>
30160
A R.D
WUD FLQV«E.O
ON TO
RT. 20 SEVERAL
TIMES DURIMG HEAVY
RAINS IN
1976.
35-8-13-ASLIDE
1550 B
UNDERCUT BY
STREAM.
' &
SLIDE I.D.
SI.IDF '
TYPF
DATA
WIDTH
LENfUH
SLOPF
AREA
SOURCE
CAUSES
DAMAGE
35-8-16-A
DEBRIS SLIQE
250VRT
10900
DATA FOR LANDSLIDE
ARFA. AN
AR
TIF
TC
TA
l I. Y S
TfcT
P
SLO
PE
fQ
UA
RR
Y).
35-8-16-Afi
450S
LO
PE
H
AD
B
EE
N
DU
RIN
G
RO
AD
C
ON
ST
RU
CT
ION
.
CU
T
35-8
-16-B
D
EB
RIS
S
LID
E17
35AREA HAD OEEN
LOGGED. MAY BE
SIDE-CAST CPILL1
FAILURE.
]
35-8-16-C
QFRRTS
SLIDE
35AT
VFRY STEEP HEAD
OF STRFAM
, TW
PREVIOUSLY LOGGtD
AUFA.
35-8-16-D
SLUM-P FLOW
35
LANDSLIDE. AREA.
vmno
JO OVdH d33iS
OhU
MOld
V-ZI-0-SC
3HDNV1VAV
tOVH UUV
rJ33fU UVH VddV
Q
HO'U
3-91-9-SC
OVM
0 OSI7
9130
lib*
'U3U001
AlSOOlAddd W339
OVH V3dV 3
0ilb
' dO
OV3K IV
i iNfl
SN01V
b'O
b 02
30J.
1S
,Siti
H3
G3-9
1-8
-SC
S3
SII
VJ
Jd
U'lS
H
itJN
Jl
ViV
Uu*
i aa
ns
SLIDE T.D.
SLIDF
DATA
WIDTH
LFNRIH
SLMPF
ARFA
CAIISFS DAMAHF
TYPF
SOURCE
3S-8-17-B
35-8-1 7-C
35-8-17-D
35-8-31-A
35-8-P2-A
D DEBRIS
3 28
57
35
1600
B,C
FLOW
i i
»
DEBRIS^
3 30
B.C FLOW
, t
DEBRIS
1 45
B»F
R SLIDE
D DEORTS
2 128
1b ^0
2050
B,C
SLIDE
DEBRIS
Z
C.B
SLIDE
DERRIS FLO
1" AUE.A
AT HFAH OF
DRAINAGE..
I
MAYRF ONLY
A SIDE-CAST CFtLU
FAILURE.
UNDERCUT QY
STREAM.
LAWOSLIOE AKEAUNDERCUT 8Y
STREAM.
35-a-aa-B DEBRIS
i SLIDE.
91 sa
UNDERCUT BY
STREAM.
SUD
E i.o
. SLID
F HATA
WIDTH
LFNGTH
SLOPE. TYPF
SOHRCFCAHSFS
£>AMA(;E: CDNMFMT
35-8-H2-C
35-8-22-D
35-8-2^-A
35-8-23-A
35-8-33-8
35-8-23-C
DEBRIS
1 6
* 91
270
FLOW
DEBRIS
a
16 43
690SLIDE
', *
* D
DEBRIS
1 11
91 20
590
8,C
FLO*
B DEORTS
4
10 12
26 A
FLOW
ii B
DEBRIS
4
10 15
33 A
RFLHW
|»
BDEBRIS
a 128
136 42
M97Q
A.O AVALANCHE
FLOWED DOWN STREAM
GULLY.
ARFA HAD BEEN
LOfiGED AND HAD
SUSTAINED ROAD
CONSTRUCTION.
1 AVERAGE SIZE OF 4
SLIDES OCCURRING
IN THESF STREAM
GULLIES.
MANY OLD SLIDES AT
THIS SITE.
ORIGINATES AS A
DEBRIS-SLIDE OR
AVALANCHE, BECOMES
FLOW IN
STRHANV GULLY.
L3L3J&S
.35JSJB
aJR
B,«
JB e e
t
SLID
E
T.O
. STYPF
OATA W
IDTH LFM
GTH SLQ
Pf SOURCE
AR
FA
C
AIIS
FS
D
AM
AR
F.
,35-ft-2*-c
QEURTS 4
150A
VA
L.A
AIC
HL
42B.C
DATA FQW UANDSLTOfc.
AREA COMTATN1MG
BOTH DEBRIS-SLIDES
AMD DEQRTS FLOWS.
3S-S-23-D
OEBRTS,
SLI'OE *
8LAWDSLTOE AT
VLRV
STEEP HEAD OP
STREAM GUt.LY.
35-8-2"*-E
35-8-23-F
35-8-23-G
UNKNOWN
2.
DEQR1S
1 SLIDE
DEBRIS
1 ?
. FLHW;
, i
! LANOSLTDE ARFA AT
VEPY ST£EP HEAO OF
STREAM GULLY.
LANDSLIDE AKEA.
D 2
22 35
250 B,C
35-6-23-H
DEBRIS
FLOW
1 I500
a
>* It'
: T.O.
SLIDE QATA
WIDTH LENGTH
SLOPF AREA
CAUSES DAMAGE
COMMENT TYPE
SOURCE
35-8-33-1
DEGRTS
1 136
VRT F,B
SLIDE
35-A-P3-J
DEHRIS
1 1
22* 45
30 640
SLIDE »
ft
35-8-24-A
DEBRIS
1 91
91 5290
FLOW
8 35-ft-?4-A
SLUMP
a
9b 64
38
4100 A
FLOW
8 35-a-24-A
SLUMP 4
76 19
38 A.
FLOW
i--
LANOSL IDE AREA,
VEPTTCAI LY CUT
Cl 1FFS IN
SAND AND
GRAVEL.
AREA HAH RFFA1
LOGGED. CWO'^w
AT TERRACE EDGE.
i
CROWN TS
.AT A
DIRT
POAO.
CPOWN tSATAOIRT
^ ROAD.
35-8-E4-8
gFS51S
FL U"M
SLIDES ni
LANDSLIDE AREA.
MIGHT
BEL DEBRIS-SLIDES.
SL
IDE
T
.D.
SI.ID
K
TY
PF
DA
TA
IV
TD
TH
L'E
NO
TH
S
I HP
F
AR
FA
C
AIIS
FS
O
AM
AR
F
DE
BR
ISFLOW
32L 20-
58
0
35-8
-25-A
DE
UR
TS
S
LID
E76
MAY BE
IMTTTATE.D BY
LQAHTMG WITH
FTLL f?TDE CA
DEBRIS
1 AVALAMCHF
DE13R
TS 1
SLIDEV
RT
F.B
35.9,30-A
DEBRIS
SLIDE
TOP OF SLIDE
AT TERRACE
EDGE.
35-9.33-A
DEBRIS
to 10
60C
ULV
ER
T
AT
HE
.A&
O
F S
LID
E
CO
NC
EN
TR
AT
ES
V
*AT
EW
. R
OA
D
MA
Y
OE
D
AM
AG
ED
.
SHOP
T.I). SLTHF
DATA
VITDTH LENGTH
SLOPE
ARFA
CAUSES
DAMAGE
COMMENT
TYPF.
* A
36-7-31-A
SI UMp (.
1 qs
22 30
510FLOW
* '
* D
36-7-33-A
DFRRTSfl 1
129 91
40 8480
SLIDE ,.
* .!
36-7-33-8
DEBRTS
1 91
SLIDE
3f»-7-33-C DEBRIS
1 342
34 11700
SLIDE
i1A
36-7-35-A
DEBRIS
1 273
40 B.C
SLIDE
;
A36-7-36-A
DEBRTS
' t
27 91
40 2^60
B SLIDE
*
CROWN JUST BELOrt
TERRACE LIP.
UNDERCUT BY
STREAM.
i,MAYBF MOT
A SLIDE.
i.lNDKRCMT (?).
BYSTREAM.
>LANDSLIDE ARFA
UNDERCUT BY
STREAM.
UNDERCUT BY
STREAM. SLIDE AT
EDGE OF
TFRRACF.
3 LANDSLIDES
|N AREA STEEPENED BY
STREAM. AREA
DEEM PREVIOUSLY
LUGGED.' b
SLIDE T.D.
SLiriF DATA
WIDTH
LENGTH
SLOPF
AREA
TYPF
SONRCF
36-7-36-B
UNKNOWN
2 4.0
30 1090
f
3&-7-3h-C
DFBPTS
1 £
k SLIDE
|
3fr-8-01-A DEBRIS
1 6&
66 3080
FLOW
(3 3*-8-01-A
SLUMP
2 208
192 27
36860
FLOW
1 8
36-8-Dt-A
SLUMP
.4 304
60 27
! Fl O
W
3^-Q-OI-B
QE8RTS
2 48
48 ISaO
FLOW
CAUSES
DAMAGE
COMMENT
,i >
'
LANDSLIDE ARFA
WHICH HAD Of EN
PREVIOUSLY LOOfoEO.
1 .
'A
' : ! LATER FAILED BY
SLUMPING (?).
SMALL DEBRIS FLOW
NEXT TO THIS ONE.
A D
APEA HAD BEEN
PREVTOUSl Y
LOGGED.
A,C
D ARE A
HAD BEEM
PREVIOUSLY LOGGED
FLOWED DDWN STRE.^^A
GULLY.
i
OS
SLIDE 1.0.
SLIDE
DATA
WIDTH
LENGTH
SLOPE
TYPE
SOURCE
36-8-01-C
DEBRIS .8
16 64
SLIDE
'
, 1
' 36-8-01-0
SLUMP
;; 4
f FLOW
.
C 36-8-01-E
DEURTS
4
15 35
30 SLIDE
1
36-8-01-F
DERPTS
i 1.
91 91
FLOW ;
1 '
-D 'i
! 36-8-02-A
DEBRIS
1 159
91 35
SLIDE
i -
AREA
CAUSES
DAMAGE
COMMENT
t . .
770
MAYBF SOME OTHFfc
TYPE OF
LANDSLIDE.
AREA HAD BEEN
PREVIOUSLY LOGGED.
A AREA HAD BEEN
LOGGED AMD HAD
SUSTAINED ROAD
CONSTRUCTION.
1
E.G,A
LANDSLIDE AREA,
SQME SLUMPS f?).
DATA FOR
AVERAGE: i
DEBRIS-SLIDE.
/
6300
A
10850
B.C
FLOWED OONN STREAM
CULLY TO
LAKE.
SLIDE l.D.
SLIDE
DATA
WIDTH
LENGTH
SLOPE
AREA
CAUSES
DAMAGE
COMMENT
TYPE
SOURCE
36-8-02-8
36-8-1 1-A
36-8-12-A
36-8-12-A
36-8-12-Q
DEBRIS
1FLOW
i; '
B UNKNOWN'
4 35
MAYBE NOT
A SLIDE.
i
1 !
iD
DEBRIS
2 56
40 20
2080 NEW
SLIDE BUT AN
FLOW OLD SCAR
is ALSO
VISIBLE.
j
DEBRIS
1 4-5
34
1150FLOW
i
UNKNOWN
'2
16 16
' 260
OLD SCAR
VISIBLE. IN
LOGGED AREA.
36-8-12-C
DEBRIS
FLOW
3 22
25 35
280 A,G
AREA HAD BE'EK1
LOGGED PRIOR TO
SLIDE.
SLID
E
1.0
. S
UD
E
DA
TA
W
IDT
H
LE
NG
TH
S
LO
PE
T
YP
EAREA
CAUSES
DAMAGE
COMMENT
1 36-&-1Z-C DEOKIS
£ FLOW
\.. -
~T~~f ------------------------------------------------ """
c36-S-13-A
SLUMP
<(. 150
18 35
?700 A.U
FLOW
36-8-13-Q
DEBRIS
1 FLOW
36-8-13-C
DEBRTS
1 1iq.
91 7E50
SLIDE
A 36-8-13-D
DEBRIS
1 20
20 45
390
SLIDE
ARFA MAY HAVE BEEN
ARKA HAD BEEN
LOGGED AMD HAD
SUSTAINED ROAU
(CONSTUUCT1QN.
MAYBE ONLY
A 4
jo SIDC-CAST (FILL>
/ A
FAILURE.
UNDERCUT OY
STREAM, (^AYQE
SOME
OTHER LAMOSLTOE.
TYPE.
UNDERCUT RY
STREAM.
SLIDE T.D.
SLIDE
DATA
WIDTH
LENGTH
SLOPF
AREA
TYPE
SOURCE
CAUSES
DAMAHE
COMMENT
SLUMP
320
17656330
C,B
UNDERCUT BY
STREAM. SLIDE AT
EDGE OF
T6RKACE.
36-8-13-F
UNKNOWN
* 1
LANDSLIDE AREA
' *'
VERY STEEP MEAD
STREAM GULI.Y.
AT OF
C '
.' '
36-8-1<l-A SLUMP
4 IE
5 30
A.Q.G
'OTMFP SIMILAR
FLOW
LANDSLIDES NEAR
BY, AREA MAY HAVE
BEEN PREVIOUSLY
LOGGED.
i
DEBRIS
1 FLOW
7930
8870LANDSLIDE AT
LAKE
LEVEL. MAY HAVE
FORMERLY BEEN
UNDERCUT BY
STREAM.
36-8-14-C
UNKMOWN
LANDSLIDE AREA,
1 t*
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SLIDE J.D.
SI IDE AT
WT0
LENGTH
SLOPE
AREA CAUSES
DAMAGE
COMMFNT
,I Y
t,
36-8-23-C
UNKNOWN,, 1
LANDSLID
f
36-8-23-D
DEBRIS
* 2
VRT
POSSIBLY
SLIDE. *
SLIDE. M
CUT. .
* i i
D !
! 36-8-2<l-A
DEBRIS
1 182
57 35
10370
B.A
FORMERLY
SLIDE
CHANNEL.
IS LAKE
36-a-2<l-B UNKNOWN
1 .22
,57 1250
E AREA.
NOT A
IGHT OE
A
A STREAM
PRESENTLY
36.8-2M-C
SLUMP FLOW
25OCCURS AT
LAKE
LEVLL. WATER
PERCHED BY
LAKE ?
36-6-24-D
UNKNOWN
; 2
12& 128
13310LOGGING ROAD AT
HEAD OF
SLIDE,
DAMAGED IF
FUTUWE. FAILURE.
SLIDE T.D. SLIDE.
DATA WIDTH
LENGTH SLOPE
AREA CAUSES
DAMAGE COMMENT
TYPE.. SOURCF.
36-8-2q-E
DEBRIS '*
2 16
16 260
SL IDE, *
^ '
36-8-26-A
DEBRIS
1
68 22
780 B.C
SLIDE
t
* A
36-8-26-B
DEBRIS
1 68
68 25
3860
A FLOW
'
'
36-8-26-C
DEBRIS
2SLIDE
,i D
36-8-26-D
DEBRIS
2 96
32 30
2^30 G,C
SLIDE
1 i
! '
' '
R
1 36-8-28-A
DEBRIS ^
50 65
40 F'A.B
!/
SLIDE
FAILURE OCCUR«ED
ALONG POWER LIME
CUT.
UNDERCUT BY
STREAM.
OCCURS AT
LAKE
LEVEL . WATER
PERCHED OY
LAKE ?
LANDSLIDE AREA
WHICH HAD BEEN
PREVIOOSU L06G£b.'
UNDERCUT
liY STWEAM.
ROAD AT
HEAD.
SIDE-CAST (FILL)
FAILURE MAY HAVE.
TRIGGERED SLIDE.
1| SLIDE T.O.
SLIDE
DATA
WIDTH
LENGTH
SLQPfe 1
. TYPE
SOURCE,
3f>-8-31-A DEBRIS,
1 j
SLIDE /
I *
,
36-8-31-B
DEBRIS
2. 272.
80 40
SLIDE/
'
C 3&-8.3q./y
DEBRIS
4
US 600
50 SLIDE
j 36-8-34-B
DEBRIS
1 159
91 SLIDE.
1
36-B-34-C
DEBRIS
! 1
a? 50
\
SLIDE
i ".'
36-8-34-D
DEBRIS
1 114
1H
SLIDE
AREA
CAUSES
DAMAGE
COMMENT
i > »
F f\
LANDSLIDES IN
AREA STEEPENED BY
ROAD CUT.
*
1 1200
8 LANDSLIDE ARFA
AIH1CH HAD RFFN
I !
20000
C.a
0 DATA FOR LANDSLIDE
AHEA AT VEOY ST^EP
HEAD OF STRtAM
GULLY.
0*
7aso 8
1350
13000
DATA FOR
A LANDSLIDE AREA,
NQT FOR AW
INDIVIDUAL SLIDE.
SLIDE l.D.
SLIDE
DATA
WIDTH
LENGTH
Sl.OPt AREA
CAUSES
DAMAGE
COMMENT
TYPE
, SOURCE
' .( a
36-8-35-A
DEBRIS
4 30
bO 30
G.B
SLIDE
S6-a-35-8
DESR1S
3 SLIDE.
-i
36-9-06-A
DEBRIS
1 AVALANCHE
j 36-9-07-A
DEBRIS
Z a«8
?5 4010
B.FLOW
t
u
36-9-07-8
DEBRIS
a 3a
64
t020
6 FLOW
TRO^JM IS
AT
TERWACE EDGE. AREA
HAD BEEM
PREVIOUSLY LOGG&O.
AREA MAY HAVE B£EN
PREVIOUSLY LOGG&O.
LANDSLIDE AREA
WHICH HAH KEEN
i PREVIOUSLY LOC<i£C>.
/
DATA FOR
LANDSLIDE AREA,
AtOVER
STEEPENED HEAD
OF STREAM
GULLY.
OCCURS INSIDE AREA
SLIDE T.D.
SLTHE
DATA WIDTH
LENGTH
SLOPE
TYPE SOURCE
AREA CAUSES
DAMAGE
COMMENT
36-9-18-A
36-9-18-0
37-9-31-A
A ' f
DEBRIS
£ 16
48 560
FLOW
* i
/
' D
DEBRIS
2 96
64 40
5630
B SLIDE
'. '
1
DEBRIS
Z lia
FLOW
MAYBE SOME OTHER
TYPE OF LANOSL TOE.
AREA HAD BEtM
PREVIOUSLY LOGGED.
LOGGING ROAD AT
HEAD OF SLIDE,
DAMAGED IF
FUTURE
FAILURE.