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  • Yellow summer wildflowers frame the Middle Falls of the Genesee River in Letchworth State Park, New York. The Middle Falls of the Genesee River has a height of 107 feet (33 meters) and is about twice that wide. The area was once submerged under an inland sea, which left deposits that formed sandstone and shale. The eroded the river bed forming the Letchworth Gorge, which is 22 miles (35 km) long and as much as 550 feet (168 meters) deep.
    NY_Letchworth_MiddleFalls_Wildflower...jpg
  • Several layers of Berea sandstone are visible near the top of Brandywine Falls, a 60-foot (18-meter) waterfall located in the Cuyahoga Valley National Park, Ohio. Brandywine Falls drops overs over three different types of rock: Berea sandstone at the top, Bedford shale in the middle and Cleveland shale at the bottom. The newest rock is about 320 million years old; the oldest is about 400 million. The layers were exposed and the waterfall was formed about 10,000 years ago when the last glaciers retreated from the area.
    OH_Cuyahoga-Valley-NP_Brandywine-Fal...jpg
  • Brandywine Falls drops 65 feet (20 meters) into a lush gorge in Cuyahoga Valley National Park, Ohio. Brandywine Falls drops overs over three different types of rock: Berea sandstone at the top, Bedford shale in the middle and Cleveland shale at the bottom. The newest rock is about 320 million years old; the oldest is about 400 million. The layers were exposed and the waterfall was formed about 10,000 years ago when the last glaciers retreated from the area. The top Berea sandstone layer is the hardest and protects the softer layers below from the erosive force of the falling water.
    OH_Cuyahoga-Valley-NP_Brandywine-Fal...jpg
  • The Genesee River cascades over a drop in the eroded river bed in Letchworth State Park, New York. The area was once submerged under an inland sea, which left deposits that formed sandstone and shale. The Genesee River eroded the river bed, forming small drops like this, as well as the Letchworth Gorge, which is 22 miles (35 km) long and as much as 550 feet (168 meters) deep.
    NY_Letchworth_GeneseeRiver_Curve_889...jpg
  • Colorful layers of siltstone, mudstone and shale are visible in the badlands near the Blue Mesa in Petrified Forest National Park, Arizona. The layers contain iron and manganese, which provide the pigments for the brilliant and varied colors.
    AZ_Petrified-Forest_Badlands_Painted...jpg
  • The Genesee River cascades over a drop in the eroded river bed in Letchworth State Park, New York. The area was once submerged under an inland sea, which left deposits that formed sandstone and shale. The Genesee River eroded the river bed, forming small drops like this, as well as the Letchworth Gorge, which is 22 miles (35 km) long and as much as 550 feet (168 meters) deep.
    NY_Letchworth_GeneseeRiver_Curve_890...jpg
  • A rainbow stretches across the sky above the Vermilion Cliffs near Page, Arizona. The Vermilion Cliffs, which rise as much as 3,000 feet (914 meters), are the second step in the five-step Grand Staircase of the Colorado Plateau, which stretches from northern Arizona to southern Utah.  The cliffs are made up of sedimentary rocks, primarily sandstone, siltstone, limestone, and shale, that have eroded over millions of years. The Vermilion Cliffs were designated as the Vermilion Cliffs National Monument in 2000.
    AZ_VermilionCliffs_Rainbow_8507.jpg
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