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248:, and its tributaries, such as McDonald Creek and Lake Creek. These streams typically flow only during periods of heavy rainfall, when flash floods sweep through the area. The erosionally resistant sandstones of the peak's cap have protected underlying soils that have remained intact, while surrounding sediments have eroded away. As a result of this process, Duffy's Peak now stands out as a small but relatively prominent landmark that can be seen from a significant distance.
217:. Duffy's Peak extends less than 50 ft (15 m) above the river, yet despite its small size, it served as an important landmark for early surveyors of the region and is said to be named for a member of the original survey team who died and was buried nearby in the late 1870s.
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Duffy's Peak is located in the rolling plains to the south and east of the
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Rolling Plains of West Texas
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98:33.35806°N 101.34222°W
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103:33.35806; -101.34222
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274:Mount Blanco
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145:Location in
139:Duffy's Peak
29:Duffy's Peak
501:Justiceburg
488:communities
439:County seat
347:Anonymous.
314:November 2,
303:Anonymous.
174:Age of rock
163:Cap Rock SE
101: /
89:101°20′32″W
76:Coordinates
543:Categories
496:Close City
290:References
284:Kiowa Peak
179:Cretaceous
147:West Texas
86:33°21′29″N
66:Prominence
21:Duffy Peak
506:Southland
209:near the
114:Geography
56:Elevation
42:Salt Fork
263:See also
230:mesquite
183:Triassic
159:Topo map
242:grasses
224:of the
168:Geology
240:, and
334:(PDF)
238:cacti
234:yucca
207:butte
195:Butte
464:Post
456:City
446:Post
360:2017
316:2012
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Text is available under the Creative Commons Attribution-ShareAlike License. Additional terms may apply.