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Coordinates: 33°57′27″N 111°11′12″W / 33.95750°N 111.18667°W / 33.95750; -111.18667
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{{Short description|Mountain range in Gila County, Arizona}}
The '''Sierra Ancha''' (“broad range” in [[Spain|Spanish]]) is a [[mountain range]] in [[Gila County, Arizona|Gila County]], in central [[Arizona]]. It lies between [[Theodore Roosevelt Lake|Roosevelt Lake]] to the south, the [[Tonto Basin]] to the west, Cherry Creek to the east, and [[Pleasant Valley, Arizona|Pleasant Valley]] to the north. The range is one of several, including the [[Bradshaw Mountains]], [[Mingus Mountain]], and the [[Mazatzal Mountains]], which form a transitional zone between the lowland [[desert]]s of southern Arizona and the [[Colorado Plateau]] of northeastern Arizona. The highest point in the range is Aztec Peak, at an elevation of 2345 m (7694 ft). This summit is the site of a [[United States Forest Service|U.S. Forest Service]] fire lookout once staffed by noted Arizona essayist and novelist [[Edward Abbey]].
[[Image:Grantham-peak.jpg|thumb|right|300px|Grantham Peak (6,591 ft) as seen from [[Arizona State Route 288]], the main road leading into the Sierra Ancha mountains from the south.]]


The '''Sierra Ancha''' ("broad range" in [[Spain|Spanish]], in [[Western Apache language|Western Apache]]: '''Dził Nteel''' - "Wide Flat Mountain") is a [[mountain range]] in [[Gila County, Arizona|Gila County]], in central [[Arizona]]. It lies between [[Theodore Roosevelt Lake|Roosevelt Lake]] to the south, the [[Tonto Basin]] to the west, Cherry Creek to the east, and Pleasant Valley to the north. The range is one of several, including the [[Bradshaw Mountains]], [[Mingus Mountain]] of the [[Black Hills (Arizona)|Black Hills]], and the [[Mazatzal Mountains]], which form a ''[[Arizona transition zone|transitional zone]]'' between the lowland [[desert]]s of southern Arizona and the [[Colorado Plateau]] of northeastern Arizona. The highest point in the range is Aztec Peak, at an elevation of 2345 m (7694 ft).
[[Image:sierra_ancha1.jpg|thumb|300px|right|Parker Canyon in the Sierra Ancha, Arizona, from State Route 288. Camera station at approximately 5000 feet elevation. Photo by Joe Schallan, Oct. 2, 2005.]]


The Sierra Ancha is penetrated by few improved roads, and the range is cut by numerous deep, spectacular [[canyon]]s, particularly on its eastern flank. Little agricultural, commercial, or residential development has taken place, though in the past [[asbestos]] mining was carried out at a mine between Asbestos and Zimmerman Points. Cattle ranching is still practiced in the area. Nearby communities include [[Roosevelt, Arizona|Roosevelt]], [[Tonto Basin, Arizona|Tonto Basin]], [[Punkin Center, Arizona|Punkin Center]], and [[Young, Arizona|Young]], Arizona. The Sierra Ancha lies completely within Arizona's [[Tonto National Forest]].
The Sierra Ancha is penetrated by few improved roads, and the range is cut by numerous deep, spectacular [[canyon]]s, particularly on its eastern flank. Little agricultural, commercial, or residential development has taken place, though in the past [[asbestos]] mining was carried out at a mine between Asbestos and Zimmerman Points. Cattle ranching is still practiced in the area. Nearby communities include Roosevelt, [[Tonto Basin, Arizona|Tonto Basin]], [[Punkin Center, Arizona|Punkin Center]], and [[Young, Arizona|Young]], Arizona. The Sierra Ancha lies completely within Arizona's [[Tonto National Forest]].


[[Image:Aztec-peak-lookout-tower.jpg|thumb|left|150px|The summit of Aztec peak is the site of a [[United States Forest Service|U.S. Forest Service]] fire lookout once staffed by noted Arizona essayist and novelist [[Edward Abbey]].]]
Two [[U.S. Wilderness Area]]s lie within the Sierra Ancha — the [[Salome Wilderness]], encompassing Salome Creek and its canyon on the southern edge of the range, and the [[Sierra Ancha Wilderness]], protecting the high peaks and deep canyons of the eastern flank of the range. The range also includes the U.S. Forest Service's Sierra Ancha Experimental Forest, a tract on which research on the characteristics of [[Southwestern United States|Southwestern U.S.]] [[drainage basin|watershed]]s has been conducted.


Two [[U.S. Wilderness Area]]s lie within the Sierra Ancha — the [[Salome Wilderness]], encompassing [[Salome Creek]] and its canyon on the southern edge of the range, and the [[Sierra Ancha Wilderness]], protecting the high peaks and deep canyons of the eastern flank of the range. The range also includes the U.S. Forest Service's Sierra Ancha Experimental Forest, a tract on which research on the characteristics of [[Southwestern United States|Southwestern U.S.]] [[drainage basin|watershed]]s has been conducted.
The Sierra Ancha includes abundant [[archaeology|archaeological]] remains, especially in the form of [[cliff-dwelling|cliff dwellings]] in the rugged canyons opening eastward toward Cherry Creek. The identity of the [[Native Americans in the United States|Native American]] builders of these structures remains uncertain, but the sites show characteristics of both the Salado and [[Mogollon culture|Mogollon]] cultures. [[Dendrochronology|Tree-ring dating]] of roof beams from the sites suggests that construction began in the late 1280s AD, and that the structures were abandoned by 1350 AD.

The Sierra Ancha includes abundant [[archaeology|archaeological]] remains, especially in the form of [[cliff-dwelling|cliff dwellings]] in the rugged canyons opening eastward toward Cherry Creek. The identity of the American Indian builders of these structures remains uncertain, but the sites show characteristics of both the [[Salado culture|Salado]] and [[Mogollon culture|Mogollon]] cultures. [[Dendrochronology|Tree-ring dating]] of roof beams from the sites suggests that construction began in about 1280 AD, and that the structures were abandoned by 1350 AD.


==Ecology==
==Ecology==
Prominent streams within the Sierra Ancha are [[Workman Creek]] and [[Salome Creek]]. The classic [[Sonoran Desert]] floristic community of [[saguaro]], [[palo verde]], and [[creosote bush]] can be found in the southern foothills above Roosevelt Lake (650-1000 m / 2133-3281 ft), while in the range's middle elevations (1200-1800 m / 3937-5906 ft) [[oak]] scrub and [[juniper]] predominate. Above 6000 feet (1829 m), the Sierra Ancha has extensive stands of [[ponderosa pine]], with [[Douglas-fir]] on the highest, coolest slopes. The Sierra Ancha hold a [[disjunctive population]] of [[Coastal woodfern]], '''[[Dryopteris arguta]]'',<ref>C. Michael Hogan. 2008</ref> which is typically found closer to the Pacific Ocean.<ref>''Jepson Manual''. 1993</ref>
Prominent streams within the Sierra Ancha are [[Workman Creek]] and [[Salome Creek]]. The classic [[Sonoran Desert]] floristic community of [[saguaro]], [[Parkinsonia|palo verde]], and [[creosote bush]] can be found in the southern foothills above Roosevelt Lake (650–1000 m / 2133–3281&nbsp;ft), while in the range's middle elevations (1200–1800 m / 3937–5906&nbsp;ft) [[oak]] scrub and [[juniper]] predominate. Above 6000 feet (1829 m), the Sierra Ancha has extensive stands of [[ponderosa pine]], with [[Douglas-fir]] on the highest, coolest slopes. The Sierra Ancha holds a [[disjunctive population]] of coastal woodfern, ''[[Dryopteris arguta]]'',<ref>C. Michael Hogan. 2008</ref> which is typically found closer to the Pacific Ocean,<ref>''Jepson Manual''. 1993</ref> owing to the relatively humid climate of the upper elevations of the range.

{{Weather box
|location = Sierra Ancha, Arizona<br/>Altitude: {{convert|5100|ft|m|-1}}
|single line = N
|Jan record high F = 76
|Feb record high F = 79
|Mar record high F = 84
|Apr record high F = 91
|May record high F = 97
|Jun record high F = 105
|Jul record high F = 104
|Aug record high F = 103
|Sep record high F = 103
|Oct record high F = 96
|Nov record high F = 83
|Dec record high F = 78
|year record high F = 105
|Jan high F = 53.0
|Feb high F = 56.7
|Mar high F = 61.6
|Apr high F = 69.9
|May high F = 78.1
|Jun high F = 88.5
|Jul high F = 91.5
|Aug high F = 89.0
|Sep high F = 85.2
|Oct high F = 75.0
|Nov high F = 62.9
|Dec high F = 54.9
|year high F = 72.2
|Jan low F = 30.3
|Feb low F = 32.6
|Mar low F = 35.6
|Apr low F = 41.7
|May low F = 48.5
|Jun low F = 57.7
|Jul low F = 62.6
|Aug low F = 61.7
|Sep low F = 58.3
|Oct low F = 48.4
|Nov low F = 37.6
|Dec low F = 31.8
|year low F = 45.6
|Jan record low F = 0
|Feb record low F = 10
|Mar record low F = 11
|Apr record low F = 16
|May record low F = 22
|Jun record low F = 30
|Jul record low F = 34
|Aug record low F = 38
|Sep record low F = 29
|Oct record low F = 20
|Nov record low F = 12
|Dec record low F = 2
|year record low F = 0
|precipitation colour=green
|Jan precipitation inch = 3.29
|Feb precipitation inch = 2.57
|Mar precipitation inch = 2.78
|Apr precipitation inch = 1.24
|May precipitation inch = 0.53
|Jun precipitation inch = 0.45
|Jul precipitation inch = 2.95
|Aug precipitation inch = 3.46
|Sep precipitation inch = 2.10
|Oct precipitation inch = 1.96
|Nov precipitation inch = 1.90
|Dec precipitation inch = 3.29
|Jan snow inch = 7.1
|Feb snow inch = 4.2
|Mar snow inch = 3.5
|Apr snow inch = 0.7
|May snow inch = 0.5
|Jun snow inch = 0.0
|Jul snow inch = 0.0
|Aug snow inch = 0.0
|Sep snow inch = 0.0
|Oct snow inch = 0.0
|Nov snow inch = 0.6
|Dec snow inch = 3.8
|Jan precipitation days = 7
|Feb precipitation days = 6
|Mar precipitation days = 6
|Apr precipitation days = 3
|May precipitation days = 2
|Jun precipitation days = 2
|Jul precipitation days = 9
|Aug precipitation days = 10
|Sep precipitation days = 6
|Oct precipitation days = 4
|Nov precipitation days = 4
|Dec precipitation days = 6
|unit precipitation days = 0.01 in
|source 1 = WRCC<ref>
{{cite web
| url = http://www.wrcc.dri.edu/cgi-bin/cliMAIN.pl?az7876
| title = SIERRA ANCHA, ARIZONA (027876)
| publisher = Western Regional Climate Center
| access-date = 2010-02-27
}}</ref>
|date=December 2011
}}

==Geology==
[[Image:South Fork Parker Canyon, Sierra Ancha, Arizona.jpg|thumb|300px|right|South fork of upper Parker Canyon in the Sierra Ancha, Arizona. Camera station on Arizona State Route 288, at approximately {{convert|1500|m|-3|abbr=on}}. The prominent cliffs topping the canyon at left, at approximately {{convert|2120|m|-2|abbr=on}}, have been formed from erosion-resistant quartzite.]]
The Sierra Ancha features significant exposures of the [[Apache Group (geology)|Apache Group]], a complex consisting of [[Proterozoic]] [[conglomerate (geology)|conglomerate]], [[shale]], dolomitic [[limestone]], and [[quartzite]], with large-scale [[intrusion]]s of [[diabase]]. The purplish [[Dripping Spring Quartzite]] and white-pinkish Troy Quartzite are much more resistant to [[weathering]] than the surrounding [[stratum|strata]] and form the Sierra Ancha's spectacular cliffs. In lower Parker Canyon, on the range's south face, the Dripping Springs Quartzite forms precipices with a {{convert|200|m|-2|abbr=on}} vertical drop. The light-colored cliffs topping upper Parker Canyon have been formed from the Troy Quartzite. The [[Basement (geology)|basement]] (lowest) rock throughout the range consists of the Proterozoic Ruin [[Granite]]. The top of Aztec Peak is capped with a coarse-grained, brown, [[Cambrian]] [[sandstone]] analogous to the [[Tapeats Sandstone]] of the [[Grand Canyon]]. The Tapeats Sandstone lies on an [[unconformity]] at {{convert|850|m|abbr=on}} in the Grand Canyon, whereas at Aztec Peak it appears at about {{convert|2350|m|abbr=on}}, a vertical displacement from which can be inferred about {{convert|1500|m|abbr=on}} of ancient [[tectonic uplift|uplift]], implying that the Sierra Ancha once stood at least 1500 m higher than the range does today, and that the [[Paleozoic]] strata which overlie the Tapeats in the Grand Canyon have been removed in the Sierra Ancha through [[erosion]]. Gravels consistent with erosional removal and deposition can be found on top of the [[Colorado Plateau]] to the north of the Sierra Ancha.<ref>Ivo Lucchitta. 2001</ref>


==References==
==References==
* C. Michael Hogan. 2008. [http://www.globaltwitcher.com/artspec_information.asp?thingid=88976 ''Coastal Woodfern (Dryopteris arguta}'', GlobalTwitcher, ed. N. Stromberg]
* C. Michael Hogan. 2008. [https://web.archive.org/web/20110711102430/http://www.globaltwitcher.com/artspec_information.asp?thingid=88976 ''Coastal Woodfern (Dryopteris arguta)'', GlobalTwitcher, ed. N. Stromberg]
* ''Jepson Manual''. 1993. [http://ucjeps.berkeley.edu/cgi-bin/get_JM_treatment.pl?19,27,28 ''Dryopteris arguta'', University of California Press, Berkeley, California]
* ''Jepson Manual''. 1993. [http://ucjeps.berkeley.edu/cgi-bin/get_JM_treatment.pl?19,27,28 ''Dryopteris arguta'', University of California Press, Berkeley, California]
* Ivo Lucchitta. 2001. ''Hiking Arizona's Geology'', The Mountaineers Books, Seattle, Wash., pp.&nbsp;145–149.


==Line notes==
==Line notes==
{{reflist}}
{{Reflist}}


== External links ==
== External links ==
{{Commons category|Sierra Ancha}}
*[http://www.topoquest.com/map.asp?z=12&n=3741401&e=508499&s=100&size=l&datum=nad83&layer=DRG100 Topographic map from TopoQuest]
*[http://www.topoquest.com/map.asp?z=12&n=3741401&e=508499&s=100&size=l&datum=nad83&layer=DRG100 Topographic map from TopoQuest]
*[http://www.fs.fed.us/r3/tonto/wilderness/wilderness-sierra_ancha-index.shtml Tonto National Forest—Sierra Ancha Wilderness]
*[http://www.fs.usda.gov/detail/tonto/specialplaces/?cid=fsbdev3_018738 Tonto National Forest—Sierra Ancha Wilderness]
*[http://www.fs.fed.us/r3/tonto/wilderness/wilderness-salome-index.shtml Tonto National Forest—Salome Wilderness]
*[http://www.fs.usda.gov/detail/tonto/specialplaces/?cid=fsbdev3_018737 Tonto National Forest—Salome Wilderness]
*[http://gorp.away.com/gorp/resource/us_wilderness_area/az_sierr.htm Sierra Ancha Wilderness at GORP]
*[http://www.gorp.com/parks-guide/travel-ta-tonto-national-forest-arizona-sidwcmdev_069079.html Sierra Ancha Wilderness at GORP]
*[http://gorp.away.com/gorp/resource/us_wilderness_area/az_salom.htm Salome Wilderness at GORP]
*[http://www.gorp.com/parks-guide/travel-ta-tonto-national-forest-arizona-sidwcmdev_069076.html Salome Wilderness at GORP]
*[http://www.fs.fed.us/rm/main/expfor/sierra.html Sierra Ancha Experimental Forest (USFS)]
*[http://www.fs.fed.us/rmrs/experimental-forests/sierra-ancha-experimental-forest/ Sierra Ancha Experimental Forest (USFS)]

*[http://ag.arizona.edu/OALS/watershed/sierraancha/sadescription.html Sierra Ancha Experimental Forest (University of Arizona)]
{{Mountains of Arizona}}
*[http://www.fs.fed.us/r3/tonto/wilderness/wilderness-facts/s_a-ruins.pdf Sierra Ancha Cliff Ruins (USFS)]
{{Authority control}}
{{Coord|33|57|27|N|111|11|12|W|display=title}}


[[Category:Arizona transition zone mountain ranges]]
[[Category:Archaeological sites in Arizona]]
[[Category:Mountain ranges of Gila County, Arizona]]
[[Category:Mountain ranges of Arizona]]
[[Category:Mountain ranges of Arizona]]
[[Category:Tonto National Forest]]

Latest revision as of 22:37, 8 February 2022

Grantham Peak (6,591 ft) as seen from Arizona State Route 288, the main road leading into the Sierra Ancha mountains from the south.

The Sierra Ancha ("broad range" in Spanish, in Western Apache: Dził Nteel - "Wide Flat Mountain") is a mountain range in Gila County, in central Arizona. It lies between Roosevelt Lake to the south, the Tonto Basin to the west, Cherry Creek to the east, and Pleasant Valley to the north. The range is one of several, including the Bradshaw Mountains, Mingus Mountain of the Black Hills, and the Mazatzal Mountains, which form a transitional zone between the lowland deserts of southern Arizona and the Colorado Plateau of northeastern Arizona. The highest point in the range is Aztec Peak, at an elevation of 2345 m (7694 ft).

The Sierra Ancha is penetrated by few improved roads, and the range is cut by numerous deep, spectacular canyons, particularly on its eastern flank. Little agricultural, commercial, or residential development has taken place, though in the past asbestos mining was carried out at a mine between Asbestos and Zimmerman Points. Cattle ranching is still practiced in the area. Nearby communities include Roosevelt, Tonto Basin, Punkin Center, and Young, Arizona. The Sierra Ancha lies completely within Arizona's Tonto National Forest.

The summit of Aztec peak is the site of a U.S. Forest Service fire lookout once staffed by noted Arizona essayist and novelist Edward Abbey.

Two U.S. Wilderness Areas lie within the Sierra Ancha — the Salome Wilderness, encompassing Salome Creek and its canyon on the southern edge of the range, and the Sierra Ancha Wilderness, protecting the high peaks and deep canyons of the eastern flank of the range. The range also includes the U.S. Forest Service's Sierra Ancha Experimental Forest, a tract on which research on the characteristics of Southwestern U.S. watersheds has been conducted.

The Sierra Ancha includes abundant archaeological remains, especially in the form of cliff dwellings in the rugged canyons opening eastward toward Cherry Creek. The identity of the American Indian builders of these structures remains uncertain, but the sites show characteristics of both the Salado and Mogollon cultures. Tree-ring dating of roof beams from the sites suggests that construction began in about 1280 AD, and that the structures were abandoned by 1350 AD.

Ecology

[edit]

Prominent streams within the Sierra Ancha are Workman Creek and Salome Creek. The classic Sonoran Desert floristic community of saguaro, palo verde, and creosote bush can be found in the southern foothills above Roosevelt Lake (650–1000 m / 2133–3281 ft), while in the range's middle elevations (1200–1800 m / 3937–5906 ft) oak scrub and juniper predominate. Above 6000 feet (1829 m), the Sierra Ancha has extensive stands of ponderosa pine, with Douglas-fir on the highest, coolest slopes. The Sierra Ancha holds a disjunctive population of coastal woodfern, Dryopteris arguta,[1] which is typically found closer to the Pacific Ocean,[2] owing to the relatively humid climate of the upper elevations of the range.

Climate data for Sierra Ancha, Arizona
Altitude: 5,100 feet (1,550 m)
Month Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec Year
Record high °F 76 79 84 91 97 105 104 103 103 96 83 78 105
Mean daily maximum °F 53.0 56.7 61.6 69.9 78.1 88.5 91.5 89.0 85.2 75.0 62.9 54.9 72.2
Mean daily minimum °F 30.3 32.6 35.6 41.7 48.5 57.7 62.6 61.7 58.3 48.4 37.6 31.8 45.6
Record low °F 0 10 11 16 22 30 34 38 29 20 12 2 0
Average precipitation inches 3.29 2.57 2.78 1.24 0.53 0.45 2.95 3.46 2.10 1.96 1.90 3.29 26.52
Average snowfall inches 7.1 4.2 3.5 0.7 0.5 0.0 0.0 0.0 0.0 0.0 0.6 3.8 20.4
Record high °C 24 26 29 33 36 41 40 39 39 36 28 26 41
Mean daily maximum °C 11.7 13.7 16.4 21.1 25.6 31.4 33.1 31.7 29.6 23.9 17.2 12.7 22.3
Mean daily minimum °C −0.9 0.3 2.0 5.4 9.2 14.3 17.0 16.5 14.6 9.1 3.1 −0.1 7.6
Record low °C −18 −12 −12 −9 −6 −1 1 3 −2 −7 −11 −17 −18
Average precipitation mm 84 65 71 31 13 11 75 88 53 50 48 84 673
Average snowfall cm 18 11 8.9 1.8 1.3 0.0 0.0 0.0 0.0 0.0 1.5 9.7 52.2
Average precipitation days (≥ 0.01 in) 7 6 6 3 2 2 9 10 6 4 4 6 65
Source: WRCC[3]

Geology

[edit]
South fork of upper Parker Canyon in the Sierra Ancha, Arizona. Camera station on Arizona State Route 288, at approximately 1,500 m (5,000 ft). The prominent cliffs topping the canyon at left, at approximately 2,120 m (7,000 ft), have been formed from erosion-resistant quartzite.

The Sierra Ancha features significant exposures of the Apache Group, a complex consisting of Proterozoic conglomerate, shale, dolomitic limestone, and quartzite, with large-scale intrusions of diabase. The purplish Dripping Spring Quartzite and white-pinkish Troy Quartzite are much more resistant to weathering than the surrounding strata and form the Sierra Ancha's spectacular cliffs. In lower Parker Canyon, on the range's south face, the Dripping Springs Quartzite forms precipices with a 200 m (700 ft) vertical drop. The light-colored cliffs topping upper Parker Canyon have been formed from the Troy Quartzite. The basement (lowest) rock throughout the range consists of the Proterozoic Ruin Granite. The top of Aztec Peak is capped with a coarse-grained, brown, Cambrian sandstone analogous to the Tapeats Sandstone of the Grand Canyon. The Tapeats Sandstone lies on an unconformity at 850 m (2,790 ft) in the Grand Canyon, whereas at Aztec Peak it appears at about 2,350 m (7,710 ft), a vertical displacement from which can be inferred about 1,500 m (4,900 ft) of ancient uplift, implying that the Sierra Ancha once stood at least 1500 m higher than the range does today, and that the Paleozoic strata which overlie the Tapeats in the Grand Canyon have been removed in the Sierra Ancha through erosion. Gravels consistent with erosional removal and deposition can be found on top of the Colorado Plateau to the north of the Sierra Ancha.[4]

References

[edit]

Line notes

[edit]
  1. ^ C. Michael Hogan. 2008
  2. ^ Jepson Manual. 1993
  3. ^ "SIERRA ANCHA, ARIZONA (027876)". Western Regional Climate Center. Retrieved 2010-02-27.
  4. ^ Ivo Lucchitta. 2001
[edit]

33°57′27″N 111°11′12″W / 33.95750°N 111.18667°W / 33.95750; -111.18667