Dendora Valley
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Dendora Valley
The Dendora Valley is a small valley on the Gila River west of Painted Rock Dam and Reservoir, Arizona, United States. The valley is north of the river, and is the valley west of the north–south Painted Rock Mountains which form the western end of the Painted Rock Reservoir. The Dendora Valley is only about long. The Gila Bend Mountains form the northern border from east to west, of both Dendora Valley, and the Painted Rock Reservoir adjacent eastwards; this is the famous Gila Bend formed by the Gila River as it changes direction to south, then west entering the reservoir. Other small mountains and hills border the southwest, namely Oatman Mountain, at and the Face Mountain group with Montezuma Head, (peak) to the west. The easiest access route to the Dendora Valley is from Hyder in the Hyder Valley The Hyder Valley is a 20-mile (32 km) long valley section of the Gila River Valley west of Hyder on the Gila River. The valley is located north of Gila River in southwe ...
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Painted Rock Dam
The Painted Rock Dam is an earthfill embankment dam located west of Gila Bend, Arizona. It is primarily used for flood control purposes. Description The Painted Rock Dam was constructed during a 3-year period from 1957–1960 by the United States Army Corps of Engineers to help control seasonal floods on the lower reaches of the Gila River. The river had no significant impediments between the Colorado River and the Coolidge Dam hundreds of miles upstream. In this stretch the river receives several tributaries, including the Hassayampa, Agua Fria rivers, and most importantly the Salt River and its major tributary, the Verde River. Due to a relatively large watershed of , more than half of which is unregulated, the flood threat to small farming communities downstream on the Gila River is large, and seasonal flooding of these areas prior to the construction of the dam was significant. The area surrounding the dam has also hosted a number of historical events. The Butterfiel ...
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Gila Bend Mountains
The Gila Bend Mountains are a long mountain range of the north-central Sonoran Desert southwest of Phoenix, Arizona and in southwest Maricopa County. The Gila River of New Mexico and Arizona transects the entire state of Arizona, and the watershed covers about 65% of Arizona. The famous Gila Bend of the river changes the west-southwest flow to south-flowing, then back to west-flowing. Painted Rock Reservoir and the Dendora Valley are nestled at the south of the Gila Bend Mountains, the monolith which causes the diversion of the Gila Bend. Gila Bend, Arizona is located at the southeast of the bend, on Interstate 8. Centennial Wash borders the north of the range and has its junction with the Gila River in the Arlington State Wildlife Area. Peaks, and landforms The highest elevation in the mountains is Woolsey Peak at , in the range's center-east. Two peaks are slightly west. In the north-center, Signal Peak, at , anchors the center of the small Signal Mountain Wilderness. ...
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Painted Rock Reservoir
The Painted Rock Dam is an earthfill embankment dam located west of Gila Bend, Arizona. It is primarily used for flood control purposes. Description The Painted Rock Dam was constructed during a 3-year period from 1957–1960 by the United States Army Corps of Engineers to help control seasonal floods on the lower reaches of the Gila River. The river had no significant impediments between the Colorado River and the Coolidge Dam hundreds of miles upstream. In this stretch the river receives several tributaries, including the Hassayampa, Agua Fria rivers, and most importantly the Salt River and its major tributary, the Verde River. Due to a relatively large watershed of , more than half of which is unregulated, the flood threat to small farming communities downstream on the Gila River is large, and seasonal flooding of these areas prior to the construction of the dam was significant. The area surrounding the dam has also hosted a number of historical events. The Butterfield ...
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Painted Rock Mountains
The Painted Rock Mountains are a short long mountain range of the north-central Sonoran Desert southwest of Phoenix, Arizona and in southwest Maricopa County. The Gila River flows through the central-north end of the range. The famous Painted Rock Petroglyph Site lies at the northeast end of the range, adjacent the Painted Rock Reservoir, and the reservoir lies at the eastern end of the agricultural river valley that is locally named as the Lower Gila River Valley, extending approximately from the Colorado River at Yuma to the west and the reservoir at the east. The Gila River crosses all of southern Arizona from southwest New Mexico, and is the drainage for about 1/2 of Arizona (the south). Peaks, and landforms The highest elevation in the mountains is "unnamed" at , and is located at the central and east region of the range. (The range has many northwest-by-southeast ridgelines.) See also * List of mountain ranges of Maricopa County, Arizona A list of mountain ranges of ...
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Hyder Valley
The Hyder Valley is a 20-mile (32 km) long valley section of the Gila River Valley west of Hyder on the Gila River. The valley is located north of Gila River in southwest Arizona in the northwestern Sonoran Desert. The Park Valley, which crosses the Gila borders to the southwest; the Hyder Valley is the access route to the Dendora Valley northeast which is on the western border of the Painted Rock Dam and Reservoir. The Hyder Valley lies on the northwest side of the Gila River, and both trend southwest–northeast. The Palomas Mountains are on the west, and the Palomas Plain, which drains three other mountain ranges, and the eastern portion of the Kofa National Wildlife Refuge, lies to the north; Face Mountain and the Gila Bend Mountains are northeast. On the south side of the Gila River, to the southeast lies the Sentinel Plain The Sentinel Plain is an extensive northwest–southeast trending plain south of the Gila River Valley in southwestern Arizona, USA. It is centere ...
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Gila River
The Gila River (; O'odham ima Keli Akimel or simply Akimel, Quechan: Haa Siʼil, Maricopa language: Xiil) is a tributary of the Colorado River flowing through New Mexico and Arizona in the United States. The river drains an arid watershed of nearly that lies mainly within the U.S., but also extends into northern Sonora, Mexico. Indigenous peoples have lived along the river for at least 2,000 years, establishing complex agricultural societies before European exploration of the region began in the 16th century. However, European Americans did not permanently settle the Gila River watershed until the mid-19th century. During the 20th century, human development of the Gila River watershed prompted the construction of large diversion and flood control structures on the river and its tributaries, and consequently the Gila now contributes only a small fraction of its historic flow to the Colorado. The historic natural discharge of the river is around , and is now only . These engin ...
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Hyder, Arizona
The Camp Hyder was a sub camp of the US Army, Desert Training Center in Riverside County, California. The main headquarters for the Desert Training Center was Camp Young, this is where General Patton's 3rd Armored Division was stationed. Camp Hyder is miles south of Hyder, Arizona. The camp was just north of the Gila River. Camp Hyder is miles east of Yuma, Arizona, near Camp Horn. Camp Hyder was built at the site of an old 1890s military base. Trained at Camp Hyder, in 1943, for six months was the 77th Infantry Division from April 1943 to September 1943. Then the 104th Infantry Division moved in for training. Unlike the other camps, no large tank activity was done. The camp was built by The 369th Engineer Regiment. Camp Hyder had its own rail station at which most troops arrived. The train station at Sentinel, Arizona south of the camp was also used. Over 13,000 troops were trained at Camp Horn and Camp Hyder. Camp Hyder was built in August 1942. The Desert Training ...
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Valleys Of Arizona
A valley is an elongated low area often running between Hill, hills or Mountain, mountains, which will typically contain a river or stream running from one end to the other. Most valleys are formed by erosion of the land surface by rivers or streams over a very long period. Some valleys are formed through erosion by glacier, glacial ice. These glaciers may remain present in valleys in high mountains or polar areas. At lower latitudes and altitudes, these glaciation, glacially formed valleys may have been created or enlarged during ice ages but now are ice-free and occupied by streams or rivers. In desert areas, valleys may be entirely dry or carry a watercourse only rarely. In karst, areas of limestone bedrock, dry valleys may also result from drainage now taking place cave, underground rather than at the surface. Rift valleys arise principally from tectonics, earth movements, rather than erosion. Many different types of valleys are described by geographers, using terms th ...
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