•
<br /> _ i - T
<br /> i o 0 0 `� �
<br /> , r \
<br /> ' o
<br /> ,
<br /> i ✓ r�
<br /> ,
<br /> � �
<br /> ,
<br /> S 26000IL
<br /> 1 /
<br /> r? X
<br /> r
<br /> LI ' OF 4 G C N ERPR ATION
<br /> 7300
<br /> u
<br /> ,
<br /> yF K w#I %
<br /> S 27000 S 2700
<br /> -___ _ __..__ _-__..- - _-_. .- _ __�-- a.._ ♦ - . ..f. _� _ .•-. V - -. ._ .- ... .. - Imo- r a-. + - .. . �- •"
<br /> 2053
<br /> Kwft •
<br /> I
<br /> o ' al wft
<br /> • 111 _
<br /> J
<br /> • I • K wff (�
<br /> s 2e000 �0 Kwft I - - - - --- - -- - - S 28006
<br /> Oil
<br /> / Jv��✓ � r rlilil�a � I..
<br /> i
<br /> I 11 1 1
<br /> . ��� I • .� 100
<br /> 2083
<br /> / ° �l)� Kwf wf11 t
<br /> AYVf Kwf1 < A III IIIII �h o�
<br /> i
<br /> � P
<br /> S 29000 1 I l !•♦ ••• `�� ie� f/ . . ' ; _ - - _ - - - -- S 29000
<br /> 7000 \
<br /> Qal _ 4 p
<br /> Kwfl. Glal f �e°� - 1 F/
<br /> 1000 10 �9S
<br /> KwfJ -_
<br /> 3151
<br /> Qal ,ISO 1
<br /> �� 1'O U W ©0 Ill�ll(11j1 o 7450
<br /> S 30000 / ,`o -- - --
<br /> J�
<br /> -- --- 1 I� Kwfl � F --1-
<br /> i
<br /> - 9 ai I'I I 11I S 30000
<br /> 3181 Q3
<br /> All,,11 1 1"11111111�
<br /> (C K wf l /
<br /> �11 111111�
<br /> �t1 11111( 1550
<br /> 6950 1 QSq P, �f1111 IIIIIIII
<br /> °
<br /> 3 y L I 111111111111 /
<br /> � r � 11 I I I i 1
<br /> Al
<br /> S 31000f � s .. f + --- QU- 32° /. 1 . �. • ♦ +•� .+sias• • ♦ ♦ , . / _
<br /> i
<br /> S 31000
<br /> 6 / - - Kw
<br /> 9 fl - r .
<br /> D -- _
<br /> i
<br /> f1 d � _ �v v�o 2055
<br /> 7
<br /> g
<br /> 6 i fl o
<br /> \ I
<br /> K w w � 4+13
<br /> 7100
<br /> -
<br /> �� - I I i _���� � �-_ � 300•- �2065
<br /> S 3200 i _ _ ;
<br /> rf � S 32000
<br /> ,
<br /> 2085 7p r -
<br /> 50
<br /> W,
<br /> h
<br /> ,
<br /> S 3300 S 33000Kill
<br /> 3153
<br /> Kwfl
<br /> �J
<br /> e ��s I � r � G� fly r '1- � ,�'� � • - s \
<br /> J
<br /> S 34000 I yt � - 7�5p ' ` Kwfl ��- - � ^- _ � 34000 -
<br /> t1-cB3 I 9to
<br /> -
<br /> 1 /-
<br /> -
<br /> •
<br /> ti
<br /> 700
<br /> \' o" cos - - / eVfl
<br /> S 3I �� S 35000
<br /> \ I
<br /> t 9 p -- C + f E 0 .G � ♦ 1
<br /> i
<br /> �v 's
<br /> r - �� •♦♦♦ �_ S 9 ���' 1�� i 1 I 1 4 Sll�dl/T I o �/ �.
<br /> pill
<br /> ,p, Ug
<br /> I 1) 77
<br /> i
<br /> f II
<br /> •
<br /> --- - _
<br /> S 36000 � e j
<br /> -J 1
<br /> rr�R TATIOI✓�
<br /> T
<br /> i
<br /> — • - _._ ._ . J-. - - -
<br /> 1
<br /> []RAGE y ° O° - �= __ -v • - _�.
<br /> 7Jsp / 6 g 04 \_
<br /> 00 _
<br /> 1�
<br /> S 3900 �� o OP -� \ ��� « S 39000
<br /> 7300 _ �- - 4263
<br /> i
<br /> 7200
<br /> S 4000 4293 S 4000
<br /> III I
<br /> � J•, ', I � � � i }_�
<br /> 7050
<br /> S 4100
<br /> "sO
<br /> 381
<br /> S 4200 5371
<br /> -� � 5351 ( 4 S 42024
<br /> 00
<br /> 21 /
<br /> i
<br /> > <ro j 1 ZS
<br /> • � � � DSO o � f -� I ! _�---� `l v ��� � i./ �� :�_ ,o / I
<br /> S 43000 __ S 43000
<br /> I VS
<br /> r4295 � l / 1
<br /> \, 7250
<br /> s 44000
<br /> '
<br /> �� 7950 s
<br /> S 45000 --- r - - -----
<br /> _ asoo
<br /> 1400 If
<br /> � 7900 _ 3950
<br /> DICffAL PHOTOGRAMMETRY BY AERO-GRAPHICS, INC.-SALT LAKE CITY, UTAH '
<br /> m; EXPLANATION 1
<br /> 313 QUATERNARY SYSTEM .�
<br /> S 6 T 6 U 6 m l Y 6 Z 6 Permit Number < 7 ri p Z o S
<br /> mlm Alluvium. Stream deposits including primarily clay- to fine class: ermit Vo17 �{•{F�d.r„f_73-3Q ja^ '., q/// - Z
<br /> S7 T 7 U 7 tr I Y 7 Z 7 - Section/Exhibit: ,-. - --_ _ -_-_,_-_-_,
<br /> Qal- sa wed fractions with fragments of sandstone u to four to -.-._.-._._..._
<br /> P ---.�----------;
<br /> six inches in maximum dimension. Locally, sandstone fractions class:[]Revision '
<br /> R B S8 T8 UB I Y8 ZB AA8 are larger, particularly in the northwestern part of the area LEGEND REVISIONS TyDer$ea —_ _ __ _— _ _ —
<br /> _ _ _-_- _-_-_ _ _ -_-_ - _-______-_. -----:
<br /> It991� FR„„FO>ED YEAR MINED - Class O Report 13 Hydro[]General
<br /> xB
<br /> beneath cliffs of the Twentymile Sandstone. I- _ _ ('1'7^r SMALL AREA EXEMPTION ^K°o�� SURFACE CONTOUR DocT e
<br /> .-- 1 CHK�D DATE DESCRIPTION YD
<br /> slluvial Fan.
<br /> Deposits
<br /> rs sandstone primarily
<br /> detto rital
<br /> silt
<br /> I 1 1 1 STOCKPILE -- r �' DRAINAGE DApplication(Coal only) 13 Bond 0 Enforcement []inspection
<br /> OIL WELL DISTURBANCE AREA -
<br /> - Qf P P P Y t1_'-•._ - - ---- PROPERTY LINE
<br /> R S9 T9 U9 V W9 X9 Y9 �( .-r�T.-,-, J1.L1 TOPSOIL
<br /> R 0 SIO T 10 U 10 V 0 Wp X 10 Y 10 Z IO maximum dimension. o o-- POWER LINE R.J.G. A/23/9' viK Rf5P
<br /> RII SII TII UII V I WIII XII YII Z11 Potentially Unstable Ground. Occurs primarily in sections of FACILITR:S PAVED ROAD R.J.G. 7/wsii PR, RESP.
<br /> Qpug lower part of the WTTliams Fork Formation where marine shale is _-- RAMP T..lW 2/18/92 the predominant rock type. Characteristics on the aerial o o < x FENCE LINE SENECA II- 1IY`A,
<br /> MINE
<br /> S12 T12 U12 V 2 W121 Xi2 Y12 • photographs, field observation and topographic slope indicate a °o°o° POND EXCAVATION WAGTF STCCKPILE ♦♦♦♦♦♦♦
<br /> Icy PERMIT BOUNDARY
<br /> ' potential for this material t0 move. PEABODV COAL COMPANY 1300 S.YALE FLAGSTAFF,ARIZONA 86001 -
<br /> S13 T13 U13 V13 , _ �'•, " EXISTING HAUL ROAD W/GRADE
<br /> I Unstable Ground. Ground that is moving or has moved recently. 4l� TEMPORARY OVERBURDEN STOCKPIL: PROPOSED HAUL ROAD W/GRAD DESIGNED BY P.C.C. SCALE I" = 400'
<br /> S14 T14 U14 V14 QUg Areas of this ground are classified generally as earth flows. 77 DRAWN BY: P.C.C. DRAWING DATE: 11-06-90
<br /> ' and all occur within the lower part of the Williams Fork. LIGHT USE ROAD
<br /> Formation where marine shale is the predominant rock t e — -J PROPOSE[] TOPSOIL STOCKPILE %.-�'�i, PROPOSED DEADHEAD ROUTE CHECKED BY R.J.G. PHOTO DATE 7-1-89
<br /> T5-N I �' P - 1 -
<br /> T-4-N � � Characteristics on the aerial photographs are typical landslide ` — CONTOUR INTERVAL' 10
<br /> 01i and slump features that can be confirmed on the ground.
<br /> Headscarps, slope scarps, hummocky ground, and related earth
<br /> flow features are common.
<br /> Stabilized Ground. Ground that appears primarily from study of FOR :
<br /> QSg aerial photographs to have experienced previous movement, but LEGEND PEABODY COAL COMPANY
<br /> to be essentially stabilized. Areas of this ground occur9 in
<br /> the lower part of the Williams Fork Formation which consists Contact between map units
<br /> primarily of marine shales.
<br /> CRETACEOUS SYSTEM „ Strike and direction of dip from aerial photographs
<br /> Williams Fork Formation- •, F F Fault, downthrown side indicated
<br /> �' — SENECA II-W MINE
<br /> _ `Moil, Scarps, variable in magnitude
<br /> Twentymile Sandstone and Above. This map .trRit •i" e
<br /> K wft Will
<br /> Fork Formation from the base of t
<br /> Sandstone to the 'tap of. t6afa .,, REGIONAL GEOLOGY -
<br /> consist of interbedded sandstone, Ale an , ' �-,
<br /> Lower Units. This map unit includes the Williams Fork
<br /> 'dl&- K wfl Torma an rom the base of the Twentymile Sandstone downward to
<br /> the base of the Formation. That part of the Lower Unit
<br /> 4: immediately below the Twentymile Sandstone is primarily marine r
<br /> shale. GEOLOGY JOI APPROVED DRAFTING:
<br /> Note: More complete descriptions of the map units are included
<br /> in the text of the accompanying report.
<br /> DATE: SCALE: DRAWING NO.:
<br /> J
<br /> F
<br /> -2s-s2 i r,=floor 9111 -2
<br />�$�-�.. a--.. _- : • - _. `� _..� --- _ - _ - --- ----- _ - -- - __ --�-- _- _ - - — -
<br /> I1111111 Hill llltllllllllllllllllllllllll
<br />
|