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Grand Prismatic Spring in Yellowstone National Park
Grand Loop road view, Calcite springs overlook and Yellowstone River in Yellowstone National Park, Wyoming, USA.
Artist Point on the Grand Canyon of the Yellowstone
Dead trees in the geothermal landscape of Norris Geyser Basin, Yellowstone National Park, Wyoming, USA. The mineral-rich hot springs have created a stark and surreal environment where trees stand bare against a bright blue sky. A powerful symbol of geology, climate, and nature’s raw forces, perfect for global buyers seeking unique science and travel imagery.
Close-up view of the textured, eroded canyon walls in Yellowstone National Park. The beige volcanic rock pillars and cliffs contrast with the green lodgepole pines and the river below in this iconic Wyoming landscape.
Travertine Cliff in a Steamy Background in Mammoth Hot Springs in Yellowstone National Park in Wyoming
Calcite Springs hydrothermal area. Yellowstone National Park, Wyoming. Springtime. Columnar basalt rock layers from a basalt flow.
Special landscapes made with film camera in USA
Lower Falls at Grand Canyon of the Yellowstone
West Thumb Geyser Basin has several different geothermal features in Yellowstone National Park.
Tiered colorful steaming pools of geologic and thermal activity in Yellowstone National Park near the North Entrance in Wyoming.  Beauty and awe of this rugged volcanic landscape.
Boulders on mountain top in beautiful landscape. Grand Canyon of the Yellostone. Overlook of the Lower Falls. Canyon and river. Beautiful landscape in Yellowstone National Park.\nWaterfall, river, forests, mountains, sky. USA
A dead tree on the white mineral ground of a geothermal area in Yellowstone National Park, Wyoming, USA. The stark contrast between the lifeless wood and the mineral-rich barren land highlights themes of survival, climate change, and the power of nature. A conceptual and striking landscape perfect for both travel and creative use.
Yellowstone River
Mammoth Hot Springs, yellow stone, US
Colorful walls of the Grand Canyon of the Yellowstone River. Yellowstone National Park, Wyoming. Springtime. The colors in the canyon are a result of hydrothermal alteration. The rhyolite in the canyon contains a variety of different iron compounds.  Exposure to the elements caused the rocks to change colors. The colors indicate the presence or absence of water in the individual iron compounds. Most of the yellows in the canyon are the result of iron present in the rock.
Closeup of Grand Prismatic Spring, Midway Geyser Basin, Yellowstone National Park, Wyoming, USA
Waterfall and canyon in the Yellowstone National Park, Wyoming, USA
This dramatic geological feature stretching about 20 miles long and reaching depths of up to 1,200 feet is carved by the Yellowstone River. It was first officially documented during the Washburn-Langford-Doane Expedition of 1870. The expedition was led by Henry D. Washburn, Nathaniel P. Langford, and Gustavus C. Doane.
The Yellowstone Canyon in Yellowstone National Park, Wyoming
Geyser in grand prismatic spring Basin in Yellowstone National Park in Wyoming
Background of wall in the Grand Canyon of Yellowstone, Wyoming, USA
Geyser in the distance at Mammoth Falls, Yellowstone National Park.
Geysers at Midway Geyser Basin Trailhead, Yellowstone National Park.
Canyon wall with volcanic basalt stones in Yellowstone
Close-up view of bright white and ochre-colored rock formations illuminated by sunlight along the Grand Canyon of Yellowstone. The rugged textures and mineral-rich surfaces stand out sharply against the canyon walls in the background. Below, the Yellowstone River carves through the narrow gorge, visible as a ribbon of turquoise water. The image highlights geological contrast, erosion patterns, and the natural artistry of volcanic stone shaped over millennia. Captured in daylight, emphasizing texture, color, and topographical depth.
Vibrant mineral deposits cover the ground in this geothermal area of Yellowstone National Park. Steam rises from vents, showcasing the park's active geology under a clear sky.
Steamy land, Midway Geyser Basin, Yellowstone National Park, Wyoming, USA
Image of Detail of colorful Yellowstone pools of acidic sulfur
Rhyolite is a type of extrusive igneous rock characterised by its light color, high silica content, and fine-grained texture. It forms from the rapid cooling of magma on the Earth's surface and is often associated with volcanic eruptions. Rhyolite is rich in silica (SiO₂), typically containing more than 70% silica. It is composed mainly of quartz and feldspar, with minerals like biotite, hornblende, and pumice often present.
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