Tag Archive for: Garfield County

Metate Arch is sculpted by weathering and differential erosion of two sandstone layers along the contact of the Gunsight Butte and overlying Cannonville Members of the Jurassic-age Entrada Sandstone. The arch is about 17 miles southeast of Escalante, just east of the Straight Cliffs. Metate Arch, Devils Garden Outstanding Natural Area, Garfield County, Utah Photographer: Ken Krahulec; © 2014

POTD 4-21-15 Devils Garden Metate Arch

Metate Arch, Devils Garden Outstanding Natural Area, Garfield County, Utah
Photographer: Ken Krahulec; © 2014

Bryce Canyon National Park, Garfield County, Utah Photographer: Danielle Lehle; © 2014

POTD 1-27-15 Bryce Canyon National Park, Garfield County

Bryce Canyon National Park, Garfield County, Utah
Photographer: Danielle Lehle; © 2014

Grand Staircase–Escalante National Monument, Garfield County, Utah
Photographer: Michael Vanden Berg; © 2013

Iron concretions from the Navajo Sandstone, Grand Staircase–Escalante National Monument, Garfield County

By: Robert F. Biek, John J. Anderson, Edward G. Sable, and Peter D. Rowley

The Haycock Mountain quadrangle lies in the central part of the Markagunt Plateau in southwest Utah and includes the eastern part of Panguitch Lake, a popular area of summer and winter recreational use. Despite the plateau’s relatively simple structure of a gently east-tilted fault block, the quadrangle contains scenic and instructive exposures of south-west Utah’s youngest basaltic lava flows, classic examples of inverted valleys capped by older lava flows, and the southern margin of the Markagunt Megabreccia, including newly identified, exceptionally instructive exposures of its basil slip surface. The Megabreccia is the debris of Utah’s largest catastrophic landslide deposit, which covers 1300 square miles (3400 km²) of the northern and central Markagunt Plateau.

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By: Robert F. Biek, John J. Anderson, Edward G. Sable, and Peter D. Rowley

The Panguitch Lake quadrangle lies in the central part of the Markagunt Plateau in southwest Utah and includes Panguitch Lake, a popular area of summer and winter recreational use. Despite the plateau’s relatively simple structure of a gently east-tilted fault block, the quadrangle contains scenic and instructive exposures of southwest Utah’s youngest basaltic lava flows, classic examples of inverted valleys capped by older lava flows, glacial deposits in the Castle Valley area, and the southern margin of the Markagunt Megabreccia. The Megabreccia is the debris of Utah’s largest catastrophic landslide deposit, which covers 1300 square miles (3400 km²) of the northern and central Markagunt Plateau.

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Bryce Canyon National Park from Rainbow Point, Garfield County, Utah
Photographer: Gregg Beukelman; © 2013

 

Waterpocket Fold, Capitol Reef National Park, Garfield County, Utah
Photographer: Adam Hiscock; © 2013

 

What a great photo to start the weekend with!

Bryce Canyon National Park, Garfield County, Utah
Photographer: Lance Weaver; © 2012

Dixie National Forest, Garfield County, Utah
Photographer: Robert F. Biek; © 2012

Colorful volcanic sandstone and mudstone of the Brian Head Formation record initiation of volcanic activity in southwest Utah about 36 million years ago. Here, Eocene-age Brian Head deposits form rugged badlands at the south end of the Sevier Plateau.

Henry Mountains, Garfield County, Utah
Photographer: Ken Krahulec; © 2012

Oligocene-age igneous intrusions exposed in the Henry Mountains, Garfield County.