347:. The center of the valley has CCC Reservoir (south, about the north-south valley center); the center-north contains Cow Camp Well and Electric Fence Reservoir. Cow Camp and Electric Fence are in the sinks region at the north terminus of Pine Valley Wash. Adjacent just north are the Pine Valley Hardpan, which has washes feeding it from the northwest (Tunnel Springs Mtns), and northeast; and from the alluvial fan washes southwest, Pine Valley Wash, south, and other washes from the east and southeast (Wah Wah Mtns).
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Pine Valley is about a 50-mile (80 km) long valley. The valley narrows in the south to about 3 miles (4.8 km) wide, where Pine Valley Wash originates. The valley is a north-south valley, but the southern 10 miles (16 km) turns southeasterly, paralleling a mountain ridgeline stretch of
328:. Steamboat Mountain, 8,588 feet (2,618 m), is west, south of the Indian Springs, but a northeasterly stretch of peaks, ridges, and hills form the southern border of the two ranges. The northeast mountainous stretch is also a part of the northwest border of the
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The north terminus of Pine Valley also narrows; here, the Tunnel
Springs Mountains are the west border, and a lower stretch of mountains and hills trend northwest from the north Wah Wah Mountains to form the eastern border.
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390:(SR‑21). A local road section of Pine Valley Road transits north from SR‑21, a due-north, straight stretch that borders the east of the
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bordered to the west. The south terminus of Pine Valley is at the merge point of the southeast Indian
Springs and
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The paved highway, Pine Valley Road, traverses from the south Pine Valley terminus to its north center, east of
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CCC Reservoir, at Pine Valley Wash (east side), (approx north-south valley center), lat-long.com (coordinates)
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Numerous unimproved roads access surrounding mountain foothills and many mountain canyons or washes.
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counties; the extreme south of the valley arises in two mountain range regions in northwestern
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The low point of the valley is probably Pine Valley
Hardpan or the Pine Valley Wash sinks.
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crosses the central-north section of Pine Valley; the route transits east to
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U.S. Geological Survey
Geographic Names Information System: Pine Valley
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that trends northeasterly off the center and southeast flank of the
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Valley in
Millard, Beaver, and Iron counties in Utah, United States
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The northwest of Pine Valley contains a 12-mile (19 km) long
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The center of Pine Valley has a 7-mile (11 km) long
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is a 50-mile (80 km) long valley in southwestern
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Utah DeLorme Atlas & Gazetteer, pp. 40-41, 48-49.
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556:Endorheic basins of the United States
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541:Valleys of Millard County, Utah
90:50 mi (80 km) N-S
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546:Valleys of Iron County, Utah
21:Pine Valley (disambiguation)
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551:Valleys of the Great Basin
503:Utah DeLorme Atlas, p. 40.
494:Utah DeLorme Atlas, p. 48.
485:Utah DeLorme Atlas, p. 40.
40:North Pine Valley and the
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396:Tunnel Springs Mountains
374:. The highway starts at
362:Looking northwest along
309:Tunnel Springs Mountains
191:Tunnel Springs Mountains
448:List of valleys of Utah
98:13 mi (21 km)
75:Pine Valley within the
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248:38.41750°N 113.68722°W
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378:at the south of the
322:Indian Springs Range
253:38.41750; -113.68722
19:For other uses, see
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364:Utah State Route 21
345:Mountain Home Range
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130:Great Basin Desert
380:Wah Wah Mountains
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372:Five Points
315:Description
291:Iron County
275:Pine Valley
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239:113°41′14″W
226:Coordinates
168:Five Points
164:Communities
69:Pine Valley
29:Pine Valley
525:Categories
454:References
236:38°25′03″N
174:Borders on
44:, May 2010
298:endorheic
103:Geography
426:See also
413:Garrison
137:Counties
417:Milford
287:Millard
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150:Millard
108:Country
354:Access
283:Beaver
145:Beaver
126:Region
87:Length
265:River
116:State
95:Width
376:Lund
320:the
285:and
279:Utah
180:List
155:Iron
120:Utah
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