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The San Juan structural basin is generally the east portion of the San Juan River Watershed of 24,600 sq mi (64,000 km 2) which extends farther west into Utah and Arizona. [1] The San Juan Basin is a geologic structural basin located near the Four Corners region of the Southwestern United States.
Radar cross-section (RCS), denoted σ, also called radar signature, is a measure of how detectable an object is by radar. A larger RCS indicates that an object is more easily detected. A larger RCS indicates that an object is more easily detected.
The byway parallels the San Juan River east and north of Mexican Hat, once again crossing Comb Ridge and intersecting with U.S. 191 and Utah State Route 162 near Bluff. The byway continues through the San Juan valley , passing through Montezuma Creek, UT and Aneth, UT before reentering the Ute Mountain Ute Indian Reservation in Colorado and ...
Juana Lopez refers to both the uppermost member of the Carlile Shale formation and to the environment that caused it to form. The Juana Lopez Member is calcareous sandstone dated to the Turonian age of the Upper Cretaceous and is exposed in the southern and western Colorado, northern and central New Mexico, [1] and northeastern Utah. [2]
Vertical cross-section through a supercell showing the BWER. The bounded weak echo region, also known as a BWER or a vault, is a radar signature within a thunderstorm characterized by a local minimum in radar reflectivity at low levels which extends upward into, and is surrounded by higher reflectivities aloft, forming a kind of dome of weak echoes.
The San Juan Basin is a distinct area of the San Juan River watershed; it is a geologic structural basin known for its abundant fuel resources. The San Juan Basin is roughly coterminous with the southeast quadrant of the San Juan River watershed in northwest New Mexico and southwest Colorado. [32]
The Pictured Cliffs Formation is a Campanian geologic formation in the San Juan Basin of New Mexico. [1] Dinosaur remains are among the fossils that have been recovered from the formation, although none have yet been referred to a specific genus .