Monocline Photos

Aerial Photo of Raplee Ridge near Mexican Hat, Utah. Raplee Ridge is a spectacular series of multicolored triangular flatirons near the San Juan River. Often called "the Raplee Anticline" the geologic structure is in fact better described as a monocline, according to the Utah Geological Survey
Aerial Photo of Raplee Ridge near Mexican Hat, Utah. Raplee Ridge is a spectacular series of multicolored triangular flatirons near the San Juan River. Often called "the Raplee Anticline" the geologic structure is in fact better described as a monocline, according to the Utah Geological Survey.
Location: Mexican Hat, Utah
Image ID: 39489  
Aerial photo of the San Rafael Reef at dawn. A fold in the Earth's crust leads to this inclined section of the San Rafael Reef, at the eastern edge of the San Rafael Swell. Clearly seen are the characteristic triangular flatiron erosion patterns that typical this formation. The colors seen here arise primarily from Navajo and Wingate sandstone
Aerial photo of the San Rafael Reef at dawn. A fold in the Earth's crust leads to this inclined section of the San Rafael Reef, at the eastern edge of the San Rafael Swell. Clearly seen are the characteristic triangular flatiron erosion patterns that typical this formation. The colors seen here arise primarily from Navajo and Wingate sandstone.
Location: Utah
Image ID: 39787  
Aerial Photo of Raplee Ridge near Mexican Hat, Utah. Raplee Ridge is a spectacular series of multicolored triangular flatirons near the San Juan River. Often called "the Raplee Anticline" the geologic structure is in fact better described as a monocline, according to the Utah Geological Survey
Aerial Photo of Raplee Ridge near Mexican Hat, Utah. Raplee Ridge is a spectacular series of multicolored triangular flatirons near the San Juan River. Often called "the Raplee Anticline" the geologic structure is in fact better described as a monocline, according to the Utah Geological Survey.
Location: Mexican Hat, Utah
Image ID: 39490  
Aerial photo of the San Rafael Reef at dawn. A fold in the Earth's crust leads to this inclined section of the San Rafael Reef, at the eastern edge of the San Rafael Swell. Clearly seen are the characteristic triangular flatiron erosion patterns that typical this formation. The colors seen here arise primarily from Navajo and Wingate sandstone
Aerial photo of the San Rafael Reef at dawn. A fold in the Earth's crust leads to this inclined section of the San Rafael Reef, at the eastern edge of the San Rafael Swell. Clearly seen are the characteristic triangular flatiron erosion patterns that typical this formation. The colors seen here arise primarily from Navajo and Wingate sandstone.
Location: Utah
Image ID: 39784  
Aerial View of the San Rafael Reef, Utah. This is a canyon-like section of the San Rafael Reef, photographed at sunrise. The "reef proper" is on the right, with its characteristic triangular flatiron erosion. The canyon in the center is a fold in the Earth's crust affiliated with the boundary of the San Rafael Swell. The colors seen here arise primarily from Navajo and Wingate sandstone
Aerial View of the San Rafael Reef, Utah. This is a canyon-like section of the San Rafael Reef, photographed at sunrise. The "reef proper" is on the right, with its characteristic triangular flatiron erosion. The canyon in the center is a fold in the Earth's crust affiliated with the boundary of the San Rafael Swell. The colors seen here arise primarily from Navajo and Wingate sandstone.
Location: Utah
Image ID: 39497  
Panorama dimensions: 4490 x 8439
Aerial View of the San Rafael Reef, Utah. This is a canyon-like section of the San Rafael Reef, photographed at sunrise. The "reef proper" is on the right, with its characteristic triangular flatiron erosion. The canyon in the center is a fold in the Earth's crust affiliated with the boundary of the San Rafael Swell. The colors seen here arise primarily from Navajo and Wingate sandstone
Aerial View of the San Rafael Reef, Utah. This is a canyon-like section of the San Rafael Reef, photographed at sunrise. The "reef proper" is on the right, with its characteristic triangular flatiron erosion. The canyon in the center is a fold in the Earth's crust affiliated with the boundary of the San Rafael Swell. The colors seen here arise primarily from Navajo and Wingate sandstone.
Location: Utah
Image ID: 39496  
Aerial photo of the San Rafael Reef at dawn. This is a canyon-like section of the San Rafael Reef, photographed at sunrise. The "reef proper" is on the right, with its characteristic triangular flatiron erosion. The canyon in the center is a fold in the Earth's crust affiliated with the boundary of the San Rafael Swell. The colors seen here arise primarily from Navajo and Wingate sandstone
Aerial photo of the San Rafael Reef at dawn. This is a canyon-like section of the San Rafael Reef, photographed at sunrise. The "reef proper" is on the right, with its characteristic triangular flatiron erosion. The canyon in the center is a fold in the Earth's crust affiliated with the boundary of the San Rafael Swell. The colors seen here arise primarily from Navajo and Wingate sandstone.
Location: Utah
Image ID: 39786  
Panorama dimensions: 4384 x 8521
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