Pedestal rock, or hoodoo, at Stud Horse Point. These hoodoos form when erosion occurs around but not underneath a more resistant caprock that sits atop of the hoodoo spire. Stud Horse Point is a spectacular viewpoint on a mesa overlooking the Arizona / Utah border.
Location: Page, Arizona
Image ID: 37778
Pedestal rock, or hoodoo, at Stud Horse Point. These hoodoos form when erosion occurs around but not underneath a more resistant caprock that sits atop of the hoodoo spire. Stud Horse Point is a spectacular viewpoint on a mesa overlooking the Arizona / Utah border.
Location: Page, Arizona
Image ID: 37780
Hoodoos in Goblin Valley State Park, aerial panorama. The "goblins" are technically known as hoodoos, formed through the gradual erosion of Entrada sandstone deposited 170 millions years ago. Aerial panoramic photograph.
Location: Goblin Valley State Park, Utah
Image ID: 37957
Hoodoos in Goblin Valley State Park. The "goblins" are technically known as hoodoos, formed through the gradual erosion of Entrada sandstone deposited 170 millions years ago.
Location: Goblin Valley State Park, Utah
Image ID: 38066
Hoodoos in Goblin Valley State Park. The "goblins" are technically known as hoodoos, formed through the gradual erosion of Entrada sandstone deposited 170 millions years ago.
Location: Goblin Valley State Park, Utah
Image ID: 38183