<?xml version='1.0' encoding='utf-8'?>
<oai_dc:dc xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd">
  <dc:contributor>W. Kenneth Hamblin</dc:contributor>
  <dc:contributor>Jessica L. Wellmeyer</dc:contributor>
  <dc:contributor>Stephanie L. Dudash</dc:contributor>
  <dc:creator>George H. Billingsley</dc:creator>
  <dc:date>2001</dc:date>
  <dc:description>The geologic map of part of the Uinkaret Volcanic Field is one product of a cooperative project between the&#13;
U.S. Geological Survey, the National Park Service, and the Bureau of Land Management to provide geologic&#13;
information about this part of the Grand Canyon-Parashant Canyon National Monument of Arizona. The Uinkaret&#13;
Volcanic Field is a unique part of western Grand Canyon where volcanic rocks have preserved the geomorphic&#13;
development of the landscape. Most of the Grand Canyon, and parts of adjacent plateaus have already been mapped.&#13;
This map completes one of the remaining areas where uniform quality geologic mapping was needed. A few dozen&#13;
volcanoes and lava flows within the Grand Canyon are not included in the map area, but their geologic significance to&#13;
Grand Canyon development is documented by Hamblin (1994) and mapped by Billingsley and Huntoon (1983) and&#13;
Wenrich and others (1997). The geologic information in this report may be useful to resource managers of the Bureau&#13;
of Land Management for range management, biological, archaeological, and flood control programs.&#13;
The map area lies within the Shivwits, Uinkaret, and Kanab Plateaus, which are subplateaus of the Colorado&#13;
Plateaus physiographic province (Billingsley and others, 1997), and is part of the Arizona Strip north of the Colorado&#13;
River. The nearest settlement is Colorado City, Arizona, about 58 km (36 mi) north of the map area (fig. 1). Elevations&#13;
range from about 2,447 m (8,029 ft) at Mount Trumbull, in the northwest quarter of the map area, to about 732 m (2,400&#13;
ft) in Cove Canyon, in the southeast quarter of the map area. Vehicle access is via the Toroweap and Mount Trumbull&#13;
dirt roads (fig. 1). Unimproved dirt roads traverse other parts of the area except in designated wilderness. Extra fuel,&#13;
two spare tires, and extra food and water are highly recommended for travelers in this remote area.&#13;
The U.S. Bureau of Land Management, Arizona Strip Field Office, St. George, Utah manages most of the area.&#13;
In addition, there are 12 sections belonging to the State of Arizona, about 12 sections are private land, and several&#13;
sections are within the Grand Canyon National Park and Lake Mead National Recreational Area (U.S. Department of&#13;
the Interior, 1993). The private land is in Potato Valley and Lake Valley, southwest and west of Mount Trumbull, and&#13;
in Whitmore Canyon and Toroweap (Tuweap) Valley. Portions of the Sawmill Mountains, Mount Logan, and Mount&#13;
Trumbull areas were originally established as part of the Dixie National Forest in 1904. In 1924, Dixie National Forest&#13;
land became part of the Kaibab National Forest. Then on February 13, 1974, management of this part of the Kaibab&#13;
National Forest was transferred to the Bureau of Land Management, Arizona Strip Field Office (personal commun.&#13;
Becky Hammond, Bureau of Land Management, 1997). Mount Logan and part of the Sawmill Mountains are now&#13;
designated as the Mount Logan Wilderness Area, and Mount Trumbull is designated as the Mount Trumbull Wilderness&#13;
Area. Most of the map area is now part of the new Grand Canyon-Parashant Canyon National Monument established&#13;
January 11, 2000.&#13;
Lower elevations within Hells Hollow, Whitmore Canyon, Toroweap Valley, and Cove Canyon support a&#13;
sparse growth of sagebrush, cactus, grass, and a variety of desert shrubs. Sagebrush, grass, cactus, cliffrose bush, pinion&#13;
pine, and juniper trees thrive at elevations above 1,830 m (6,000 ft). Ponderosa pine and oak forests thrive at higher&#13;
elevations in the Mount Trumbull and Mount Logan areas.&#13;
Surface runoff within the map area drains south towards the Colorado River through Hells Hole, Hollow,&#13;
Whitmore Canyon, Toroweap Valley, and Cove Canyon. Upper Toroweap Valley, upper Hells Hollow, and Whitmore&#13;
Canyon are part of the physiographic area of Grand Canyon, but are not within Grand Canyon National Park&#13;
(Billingsley and others, 1997). As of January 11, 2000, these areas are now part of the new Grand Canyon-Parashant</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.3133/mf2368</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>Geological Survey (U.S.)</dc:publisher>
  <dc:title>Geologic Map of Part of the Uinkaret Volcanic Field, Mohave County, Northwestern Arizona</dc:title>
  <dc:type>reports</dc:type>
</oai_dc:dc>