A sandstone formation in the Valley of Fire Nevada State Park. The different colors in the rock result from different impurities in the sandstone, such as iron, sulfur, and magnesium.
Alex Demas (Former Employee)
Science and Products
A sandstone formation in the Valley of Fire Nevada State Park. The different colors in the rock result from different impurities in the sandstone, such as iron, sulfur, and magnesium.
A sandstone formation in the Valley of Fire Nevada State Park. The different colors in the rock result from different impurities in the sandstone, such as iron, sulfur, and magnesium.
A sandstone formation in the Valley of Fire Nevada State Park. The different colors in the rock result from different impurities in the sandstone, such as iron, sulfur, and magnesium.
A sandstone formation in the Valley of Fire Nevada State Park. The different colors in the rock result from different impurities in the sandstone, such as iron, sulfur, and magnesium.
A sandstone formation in the Valley of Fire Nevada State Park. The different colors in the rock result from different impurities in the sandstone, such as iron, sulfur, and magnesium.
A petrified log in the Valley of Fire Nevada State Park. Petrified wood occurs when a tree, or a plant similar to a tree, undergoes a kind of fossilization known as "permineralization," in which all the organic parts of the tree are replaced with minerals.
A petrified log in the Valley of Fire Nevada State Park. Petrified wood occurs when a tree, or a plant similar to a tree, undergoes a kind of fossilization known as "permineralization," in which all the organic parts of the tree are replaced with minerals.
A petrified log in the Valley of Fire Nevada State Park. Petrified wood occurs when a tree, or a plant similar to a tree, undergoes a kind of fossilization known as "permineralization," in which all the organic parts of the tree are replaced with minerals.
A petrified log in the Valley of Fire Nevada State Park. Petrified wood occurs when a tree, or a plant similar to a tree, undergoes a kind of fossilization known as "permineralization," in which all the organic parts of the tree are replaced with minerals.
A sandstone formation in the Valley of Fire Nevada State Park.
A sandstone formation in the Valley of Fire Nevada State Park.
A sandstone formation in the Valley of Fire Nevada State Park.
A sandstone formation in the Valley of Fire Nevada State Park.
A sandstone formation in the Valley of Fire Nevada State Park.
A sandstone formation in the Valley of Fire Nevada State Park.
A sandstone formation in the Valley of Fire Nevada State Park.
A sandstone formation in the Valley of Fire Nevada State Park.
A sandstone formation in the Valley of Fire Nevada State Park.
A sandstone formation in the Valley of Fire Nevada State Park.
A sandstone formation in the Valley of Fire Nevada State Park.
A sandstone formation in the Valley of Fire Nevada State Park.
A sandstone formation in the Valley of Fire Nevada State Park.
A sandstone formation in the Valley of Fire Nevada State Park.
A sandstone formation in the Valley of Fire Nevada State Park.
A sandstone formation in the Valley of Fire Nevada State Park.
A sandstone formation in the Valley of Fire Nevada State Park.
A sandstone formation in the Valley of Fire Nevada State Park.
A sandstone formation in the Valley of Fire Nevada State Park. The different colors in the rock result from different impurities in the sandstone, such as iron, sulfur, and magnesium.
A sandstone formation in the Valley of Fire Nevada State Park. The different colors in the rock result from different impurities in the sandstone, such as iron, sulfur, and magnesium.
A sandstone formation in the Valley of Fire Nevada State Park. The different colors in the rock result from different impurities in the sandstone, such as iron, sulfur, and magnesium.
A sandstone formation in the Valley of Fire Nevada State Park. The different colors in the rock result from different impurities in the sandstone, such as iron, sulfur, and magnesium.
A sandstone formation in the Valley of Fire, a Nevada state park.
A sandstone formation in the Valley of Fire, a Nevada state park.
A panorama of Hoover Dam and Lake Mead. Hoover Dam impounds Lake Mead and provides drinking water and hydroelectric power to the surrounding area. It was constructed between 1931 and 1936.
A panorama of Hoover Dam and Lake Mead. Hoover Dam impounds Lake Mead and provides drinking water and hydroelectric power to the surrounding area. It was constructed between 1931 and 1936.
A bronze statue watching over Hoover Dam.
A bronze statue watching over Hoover Dam.
Hoover Dam impounds Lake Mead and provides drinking water and hydroelectric power to the surrounding area. It was constructed between 1931 and 1936. The Intake Towers are where water enters to generate electricity.
Hoover Dam impounds Lake Mead and provides drinking water and hydroelectric power to the surrounding area. It was constructed between 1931 and 1936. The Intake Towers are where water enters to generate electricity.
Hoover Dam impounds Lake Mead and provides drinking water and hydroelectric power to the surrounding area. It was constructed between 1931 and 1936.
Hoover Dam impounds Lake Mead and provides drinking water and hydroelectric power to the surrounding area. It was constructed between 1931 and 1936.
Science and Products
A sandstone formation in the Valley of Fire Nevada State Park. The different colors in the rock result from different impurities in the sandstone, such as iron, sulfur, and magnesium.
A sandstone formation in the Valley of Fire Nevada State Park. The different colors in the rock result from different impurities in the sandstone, such as iron, sulfur, and magnesium.
A sandstone formation in the Valley of Fire Nevada State Park. The different colors in the rock result from different impurities in the sandstone, such as iron, sulfur, and magnesium.
A sandstone formation in the Valley of Fire Nevada State Park. The different colors in the rock result from different impurities in the sandstone, such as iron, sulfur, and magnesium.
A sandstone formation in the Valley of Fire Nevada State Park. The different colors in the rock result from different impurities in the sandstone, such as iron, sulfur, and magnesium.
A sandstone formation in the Valley of Fire Nevada State Park. The different colors in the rock result from different impurities in the sandstone, such as iron, sulfur, and magnesium.
A petrified log in the Valley of Fire Nevada State Park. Petrified wood occurs when a tree, or a plant similar to a tree, undergoes a kind of fossilization known as "permineralization," in which all the organic parts of the tree are replaced with minerals.
A petrified log in the Valley of Fire Nevada State Park. Petrified wood occurs when a tree, or a plant similar to a tree, undergoes a kind of fossilization known as "permineralization," in which all the organic parts of the tree are replaced with minerals.
A petrified log in the Valley of Fire Nevada State Park. Petrified wood occurs when a tree, or a plant similar to a tree, undergoes a kind of fossilization known as "permineralization," in which all the organic parts of the tree are replaced with minerals.
A petrified log in the Valley of Fire Nevada State Park. Petrified wood occurs when a tree, or a plant similar to a tree, undergoes a kind of fossilization known as "permineralization," in which all the organic parts of the tree are replaced with minerals.
A sandstone formation in the Valley of Fire Nevada State Park.
A sandstone formation in the Valley of Fire Nevada State Park.
A sandstone formation in the Valley of Fire Nevada State Park.
A sandstone formation in the Valley of Fire Nevada State Park.
A sandstone formation in the Valley of Fire Nevada State Park.
A sandstone formation in the Valley of Fire Nevada State Park.
A sandstone formation in the Valley of Fire Nevada State Park.
A sandstone formation in the Valley of Fire Nevada State Park.
A sandstone formation in the Valley of Fire Nevada State Park.
A sandstone formation in the Valley of Fire Nevada State Park.
A sandstone formation in the Valley of Fire Nevada State Park.
A sandstone formation in the Valley of Fire Nevada State Park.
A sandstone formation in the Valley of Fire Nevada State Park.
A sandstone formation in the Valley of Fire Nevada State Park.
A sandstone formation in the Valley of Fire Nevada State Park.
A sandstone formation in the Valley of Fire Nevada State Park.
A sandstone formation in the Valley of Fire Nevada State Park.
A sandstone formation in the Valley of Fire Nevada State Park.
A sandstone formation in the Valley of Fire Nevada State Park. The different colors in the rock result from different impurities in the sandstone, such as iron, sulfur, and magnesium.
A sandstone formation in the Valley of Fire Nevada State Park. The different colors in the rock result from different impurities in the sandstone, such as iron, sulfur, and magnesium.
A sandstone formation in the Valley of Fire Nevada State Park. The different colors in the rock result from different impurities in the sandstone, such as iron, sulfur, and magnesium.
A sandstone formation in the Valley of Fire Nevada State Park. The different colors in the rock result from different impurities in the sandstone, such as iron, sulfur, and magnesium.
A sandstone formation in the Valley of Fire, a Nevada state park.
A sandstone formation in the Valley of Fire, a Nevada state park.
A panorama of Hoover Dam and Lake Mead. Hoover Dam impounds Lake Mead and provides drinking water and hydroelectric power to the surrounding area. It was constructed between 1931 and 1936.
A panorama of Hoover Dam and Lake Mead. Hoover Dam impounds Lake Mead and provides drinking water and hydroelectric power to the surrounding area. It was constructed between 1931 and 1936.
A bronze statue watching over Hoover Dam.
A bronze statue watching over Hoover Dam.
Hoover Dam impounds Lake Mead and provides drinking water and hydroelectric power to the surrounding area. It was constructed between 1931 and 1936. The Intake Towers are where water enters to generate electricity.
Hoover Dam impounds Lake Mead and provides drinking water and hydroelectric power to the surrounding area. It was constructed between 1931 and 1936. The Intake Towers are where water enters to generate electricity.
Hoover Dam impounds Lake Mead and provides drinking water and hydroelectric power to the surrounding area. It was constructed between 1931 and 1936.
Hoover Dam impounds Lake Mead and provides drinking water and hydroelectric power to the surrounding area. It was constructed between 1931 and 1936.