Introduction: Written in the RocksLike pages in a book, the rock layers present in the upper Black Canyon and Curecanti tell a story of past environments, ancient animals, and dynamic processes of change. Geologic TimeOne spin of the Earth on its axis is a day, and one trip around the sun is a year. While this concept seems rather straightforward now, scholars sought for centuries to understand time and its relationship to the age of the Earth. For the purpose of understanding the length of each era, chapter pages are listed out of a 1,000 page "book" covering all of Earth's history. Chapter 1: PrecambrianPages: 1–880 The Precambrian accounts for Earth's history from its very beginning up until about 540 million years ago. This era reveals a time of harsh and drastic changes in the Earth and show little to no signs of life. It is difficult for geologists to interpret what Colorado may have looked like during this time. Most of the region's Precambrian-age rocks have been highly altered by extreme heat and pressures. Precambrian rocks are often called basement rocks, since they are buried deep beneath the surface. They only become exposed under special circumstances where the overlying younger rocks have been stripped away. Most exposures of these ancient rocks are found in the cores of mountain ranges or in deeply eroded canyons like the Black Canyon. Chapter 2: Paleozoic EraPages: 881–955 Chapter 3: Mesozoic EraPages: 956–987 The Morrison Formation is one of the most widespread and easily recognized rock formations in the Southern Rocky Mountain and Colorado Plateau regions. Its strata (beds or layers) contain iron oxide and other minerals responsible for the red and green colors, which makes the Morrison Formation so easy to identify. The sandstones and mudstones that characterize the Morrison Formation were deposited in shallow lakes and by streams and rivers that would occasionally flood the surrounding lowlands. Fossilized remains of dinosaurs and other Mesozoic life provide important clues which help us understand the environment and the creatures that lived near these ancient lakes and streams. Above the Morrison Formation is a more resistant sedimentary rock called Dakota Sandstone. This buff-colored, Cretaceous rock forms prominent outcrops in the roadcuts along U.S. Highway 50, just west of Elk Creek. The Dakota Sandstone was deposited along the shore of an ancient inland sea. When this sandstone was being deposited, the area was coastal with beaches, sand dunes, marshes, and mudflats. Over the next several thousand years, the inland sea deepened and expanded, swallowing Colorado and much of the Southwest. Near-shore beach deposits gave way to offshore marine deposits of soft, black mud. This mud accumulated to great thicknesses. Chapter 4: Cenozoic EraPages: 988–1000 The beginning of the Tertiary Period coincides with the birth of the Rocky Mountains. The event is known as the Laramide Orogeny (orogeny means "mountain building"). The cause of the Laramide Orogeny reaches back more than 200 million years. At the end of the Triassic period, the great supercontinent known as Pangea began to break apart, and North America began to separate from Europe. Far to the west, the North American crustal plate began colliding with and over-riding the Pacific-Farallon Plate. The collision between the two plates caused the crust to buckle and fold. This folding started in California and gradually moved its way eastward, finally reaching Colorado about 60 million years ago. The stresses caused by the colliding plates to the west forced several Precambrian crustal "wedges" upwards, forming the Colorado Front Range and the Southern Rocky Mountains. In some areas, the mountain building was accompanied by volcanic eruptions and magma emplacement. Tertiary VolcanismVolcanic processes during the Tertiary Period are responsible for one of the most notable geologic features in Curecanti. The Dillon Pinnacles tower above the northern shore of Sapinero Basin in Blue Mesa Reservoir. West Elk Breccia (pronounced bretch'-yuh) is the rock that makes up these pinnacles. It formed from a huge volcanic mud flow of ash and volcanic debris that spewed from violent eruptions in the West Elk Mountains about 30 million years ago. The West Elk Breccia contains a jumble of angular rock fragments that vary in size and shape. These fragments are imbedded in a matrix of fine volcanic ash and mud. Many of the larger clastic fragments are more resistant to the effects of erosion and weathering than the soft, mud-ash matrix. These larger rock fragments provide protection against the elements, sheltering the rock beneath it. The result is spire-like pinnacles. About 28 million years ago, a series of volcanic ash flows that originated from the San Juan Mountains blanketed much of southern Colorado. The tremendous caldera eruptions of the San Juans were characterized by turbulent, flowing clouds of hot incandescent ash, gasses and tiny shards of volcanic glass. As the turbulent ash clouds settled out, the burning-hot ash and glass shards welded together to form a dense, erosion-resistant rock called welded tuff. The various layers of welded tuff serve as cap rocks that protect the softer rocks beneath them and give the mesas surrounding Curecanti their flat "tops." From Past to PresentThe uplift and volcanism of the early to mid-Tertiary (Cenozoic Era) established the highland that would serve as the headwaters for the Gunnison River. Snowmelt from the Sawatch Range to the east, the West Elk Mountains to the north, and the San Juans to the south provided an ample supply of water to what would eventually become the Gunnison Basin. Geologists believe that the modern Gunnison River became established in its current course about 10 to 15 million years ago, just after the last eruptions in the San Juans and West Elks. This coincides with a period of rapid uplift of the Great Basin and Colorado Plateau provinces that lie between the Rocky Mountains and the Sierra Nevadas in California. Additional ResourcesEdwards, Lucy E. and Pojeta, Jr., John, n.d. Fossils, Rock, and Time. https://pubs.usgs.gov/gip/fossils/ |
Last updated: August 11, 2024