Navajo section
The Navajo Section is a physiographic section of the larger Colorado Plateaus Province, which in turn is part of the larger Intermontane Plateaus physiographic Division.[1]
Geography
The Navajo Section is located in northeastern Arizona and northwestern New Mexico. It is named for the Navajo Nation, with about half of the area of the section on the Navajo Reservation.
The section is characterized by broad rolling plains on easily eroded and carved rocks, with cuestas (ridges) and tablelands capped by gently dipping resistant sandstone beds. One of the most prominent landform features of the Navajo Section is Shiprock, a Script error: No such module "convert". monadnock formation near the town of Shiprock, New Mexico.
Elevations
The lowest point in the Navajo Section is about Script error: No such module "convert"., near the Four Corners area. The boundary between this section and the Canyon Lands Section is nearby, in the San Juan River basin. The highest point of the Navajo Section is Script error: No such module "convert". at Chromo Mountain on the Continental Divide near Chama, New Mexico.[2]
Adjacent
Adjacent to the Navajo Section are the:
- Canyon Lands Section to the north.
- Rio Grande rift of the Basin and Range Province to the east.
- Acoma-Zuni Section to the south.
- Grand Canyon Section to the west
Geology and physiography
The area is predominantly generally horizontal sandstone beds with some shale sequences of late Cretaceous and early Cenozoic age. A few areas of the section also have abundant volcanic necks and buttes, but due to the arid weather and soft sandstone, many of the rock formations of the area have eroded to form distinctive features of long cuestas, shallow canyons and valleys, narrow fan terraces, undulating plateaus, isolated mesas, steep hills, and some shale badlands.[2]
- San Juan Basin
Near the Four Corners area is a steeply tilted monocline known as The Hogback, which trends southwestward from where the San Juan River enters the area. Here the San Juan River flows into an area known as the San Juan Basin, where the western San Juan Basin is typified by exposures of the Fruitland and Menefee Formations. A stepped sequence of high stream terraces, present above the San Juan River and its tributaries, represents abandoned Pleistocene flood plains.[3]
See also
References
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External links
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