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Garden of the Gods and Pikes Peak, Colorado Springs --- The red Lyons Formation sandstone layers were uplifted vertically when the Rocky Mountains were uplifted. The 14,000 foot Pikes Peak in the background is a lone Precambrian granite intrusion.
Mt. Sopris, Carbondale --- The granitic magma that solidified to form this mountain was intruded below sedimentary layers that have since been eroded away on top, but still remain tilted upwards along the edges.
El Peñón de Guatapé is a granitic monolith that rises about 200 m above the surrounding landscape, in the Antioquia region of NW Colombia. These isolated landforms are also known as "inselbergs" and are typical of granitic rocks in tropical regions.