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Areas of Landslides Sikes Dam Quadrangle, North DakotalsQ ls Qls Qls Qls Qls Qls Qls Qls ls Qls Qls...

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Qls Qls Qls Qls Qls Qls Qls Qls Qls Qls Qls Qls Qls Qls Qls Qls Qls Qls Qls Qls Qls Qls Qls Qls Qls Qls Qls Qls Qls Qls Qls Qls Qls Qls Qls Qls Qls Qls Qls Qls Qls Qls Qls Qls Qls Qls Qls Qls Qls Qls Qls Qls Qls Cartographic Compilation: E. L. Kadrmas & S.S. Kranich 102 o 30 ' 00 " 48 o 15 ' 00 " 102 o 22 ' 30 " 102 o 22 ' 30 " 102 o 30 ' 00 " 48 o 07 ' 30 " 48 o 07 ' 30 " 48 o 15 ' 00 " Areas of Landslides Sikes Dam Quadrangle, North Dakota (STANLEY) (STANLEY SE) (ROS S) (RAT LAKE SE) (BELDEN SE) (ROB INS ON LA KE) (BELDEN SW) (BELDEN) North Dakota Geological Survey 24K: SksD - l Edward C. Murphy, State Geologist Lynn D. Helms, Director Dept. of Mineral Resources Geologic Symbols Known contact between two geologic units. UNIT DESCRIPTIONS QUATERNARY SYSTEM RECENT/PLEISTOCENE Geology Undifferentiated T. 155 N. T. 154 N. Other Features Unpaved Road MN 1981 Magnetic North Declination at Center of Sheet 12 o R. 91 W. R. 92 W. 0 0.5 1 Miles 1:24,000 Scale Standard Parallels 48 o 07 ' 30 " an d 48 o 15 ' 00 " USGS 7.5 Min ute Topo graph ic Map Co ntour Interval 1 0 Feet Lambert Conformal Conic Projection 1927 North American Datum NGVD 1929 Road Layer Rectified to 2003 NAIP Digital Orthophoto Sikes Dam Quadrangle, North Dakota Edward C. Murphy 2011 Variable mixture of strata and deposits that have slid to the base of steep slopes of the Little Knife River Valley and tributaries. Landslide Deposits Qls Landslides identified on this quadrangle were mapped from stereo pairs, black and white 1:20,000 scale aerial photographs flown between 6-6-58 and 9-7-58. As a result these maps can be used to identify areas that are vulnerable to slope failure, but are not an up to date assessment of all landslides for the area.
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Page 1: Areas of Landslides Sikes Dam Quadrangle, North DakotalsQ ls Qls Qls Qls Qls Qls Qls Qls ls Qls Qls Qls Qls Qls Qls Qls Qls Qls Qls Qls Qls Qls!(8 Cartographic Compilation: E. L. Kadrmas

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Cartographic Compilat ion: E. L. Kadrmas & S.S. Kran ich

102o 30' 00"

48o 15' 00"

102o 22' 30"

102o 22' 30"102o 30' 00"48o 07' 30" 48o 07' 30"

48o 15' 00"

Areas of LandslidesSikes Dam Quadrangle, North Dakota

(STANLEY) (STANLEY SE

)

(ROSS)

(RAT LAKE SE) (BELDEN SE)

(ROB

INSO

N LA

KE)

(BELDEN SW)

(BEL

DEN)

North Dakota Geological Survey24K: SksD - l

Edward C. Murphy, State GeologistLynn D. Helms, Director Dept. of Mineral Resources

Geologic Symbols

Known contact between two geologic units.

UNIT DESCRIPTIONS

QUATERNARY SYSTEM

RECENT/PLEISTOCENE

Geology Undifferentiated

T. 155 N.

T. 154 N.

Other Features

Unpaved Road

MN

1981 Magnetic North Declinat ion at Center of Sheet

12o

R. 91 W.R. 92 W.

0 0.5 1Miles

1:24,000Scale

Stand ard Paral lels 4 8o 07' 30" an d 48o 15' 00"

USGS 7.5 Min ute Topo graph ic Map Co ntour Interval 1 0 Feet

Lambert Conformal Conic Projection1927 No rth American Datum NGVD 1929

Road Layer Rectified to 2 003 NAIP Digi tal Orth ophotoSikes Dam Quadrangle, North Dakota

Edward C. Murphy2011

Variable mixture of strata and deposits that have slid to the base ofsteep slopes of the Little Knife River Valley and tributaries.

Landslide DepositsQls

Landslides identified on this quadrangle were mapped from stereopairs, black and white 1:20,000 scale aerial photographs flownbetween 6-6-58 and 9-7-58. As a result these maps can be usedto identify areas that are vulnerable to slope failure, but are not anup to date assessment of all landslides for the area.

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