thermochronology pushes the age of Colorado Plateau uplift back to the latest Cretaceous, with a kilometer-scale elevation gain over the south-western part of the plateau (Flowers et al., 2008; Fig. Most recent uplift phase started 10-5 m.y.a. The uplift was facilitated by reactivation of pre-existing faults and accompanied by tilting of the plateau toward the north. The most popular models of uplift can be divided into crustal, lithospheric and sub-lithospheric categories. In the Colorado Plateau, 1.3 km of Cenozoic uplift remain unex - plained, and on the Great Plains, there is … The way in which the uplift of the Colorado Plateau occurred is puzzling. I thought some sort of uplift must have formed the Bookcliffs. The uplift history of the Colorado Plateau has been debated for over a century with still no unified hypotheses for the cause, timing, and rate of uplift. Lithospheric density models reveal evidence for Cenozoic uplift of the Colorado Plateau and Great Plains by lower-crustal hydration 2A). Because of this uplift, it is not correct to say the Grand Canyon was carved down through the rock by the Colorado River. When the entire Colorado Plateau was uplifted at the same time as the Rockies, The Colorado River … The river stayed in the same place while the surrounding land pushed up higher than the river, but the rise was so slow that the river maitnationed its position by eroding the gradually rising rock-- the Colorado Plateau is a geologic marvel. The first uplift of the Defiance Plateau occurred in Laramide time. In essence The Laramide Orogeny is the birth of The Colorado Plateau. The Colorado Plateau is a major tectonic and physiographic province in the southwestern United States which has been relatively stable during the Phanerozoic, but has been epeirogenically uplifted about 2 km in the Cenozoic. and Morgan, 1990), they account for ~300–350 m of uplift of the Colorado Pla-teau relative to the eastern Great Plains and 400–500 m in the western Great Plains (Fig. Zion is located along the edge of a region called the Colorado Plateau. With support from the Grand Canyon Trust and the Landscape Conservation Initiative, the first Uplift Conference in the spring of 2015 engaged nearly 100 young people. Enjoy the videos and music you love, upload original content, and share it all with friends, family, and the world on YouTube. They decided to call the gathering “Uplift,” inspired by the geologic process that led to the rise of the Colorado Plateau. Tectonic Setting of the Colorado Plateau and Previous Paleoaltimetry 2.1. While the adjacent Basin and Range province and Rio Grande rift province underwent Cenozoic shortening followed by extension, the plateau experienced approximately 2 km of rock uplift without significant internal deformation. Uplift, tilting, and erosion of rock layers formed a feature called the Grand Staircase, a series of colorful cliff s stretching between Bryce Canyon and the Grand Canyon. The eastern boundary of the uplift was a monocline near the present Arizona / New Mexico border. GSA TODAY, AUGUST 2002 5 Isostatic response to the erosional ex-humation of the plateau over the middle-late Cenozoic should itself result in sig-nificant rock uplift, but this has not been adequately considered in evaluating the Even though the plateau is a distinct physiographic unit today (e.g., Spencer, 1996), whether it was uplifted as an individual block, As the plateau, erosion took the more recent rocks off, leaving the more resistant sandstone. With the arrival of the flat-lying Farallon slab, dynamic subsidence swept from west to east over the plateau and reached a maximum ca. Two stages of uplift followed the removal of the Farallon slab below the plateau: one in the latest Cretaceous and the other in the Eocene with a cumulative uplift … The Colorado Plateau is a massive feature with a series of relatively flat-bedded tablelands, made steplike by faulting action and intruded by domes of igneous rocks. The Colorado Plateau is an arid region that developed as a stable crustal block. The plateau, with an average elevation of 9,500 feet (2,900 m), rises from the Colorado River 4,600 ft (1,400 m) to Horsefly Peak 10,300 ft (3,100 m). At the Uplift Climate Conference, we connect, train, and support young people to act for climate justice. Mechanisms Driving Plateau Uplift and Existing Paleoelevation Constraints [5] The Colorado Plateau is a 2 km high, roughly 337,000 km 2 physiographic region bounded by the Rocky Mountains, Rio Grande Rift, and Basin and Range provinces in the southwestern United States . Uplift of the Colorado Plateau was a key step in the eventual formation of Grand Canyon. The action of plate tectonics lifted the rocks high and flat, creating a plateau through which the Colorado River could cut down. A classic example is the Colorado Plateau, for which the starting and ending points are well known: The region was at sea level in the Late Cretaceous, and now, the deeply eroded land surface is at ~2 km. Colorado Plateau uplift and erosion evaluated using GIS. We are currently in a period of structural and financial transition to have more capacity to meet the needs of the regional movement for climate justice. The Uncompahgre uplift is a northwest-trending Laramide structure bordered on its southwestern and northeastern flanks by faulted monoclines (Williams, 1964; Cashion, 1973). The regional uplift of the Colorado Plateau began about 6 million years ago. The bottom layer of rock Huntington, K. W., Wernicke, B. P. & Eiler, J. M. Influence of climate change and uplift on Colorado Plateau paleotemperatures from carbonate clumped isotope thermometry. This blocked the southwest to northeast drainage from Arizona to Wyoming and helped form the ancestral Little Colorado River. It was not significantly affected by either the compressional forces that gave rise to the Rockies or by the Cenozoic extensional forces that produced the Basin and Range. Uplift is a climate justice conference created for - and by - young people. Uncompahgre uplift of Colorado and Utah and along major fault blocks along the flanks of the uplift, which partly coincides with the geomorphic Uncompahgre Plateau. Upwelling may be related to movement of the slab gap (we talked about this earlier) under the plateau between 10 and 5 million years. Uncompahgre is a Ute word that describes the water: "Dirty Water" or "Rocks that make Water Red".. • Geophysical data reveals there is mantle upwelling under the plateau. 86 Ma. Uplift connects, trains, and supports young people (ages 18-30) to take climate action across the Colorado Plateau and greater Southwest. The Uncompahgre Plateau in western Colorado is a distinctive large uplift part of the Colorado Plateau. tion has focussed on the Colorado Plateau, which sits in the middle of the southern half of the uplifted zone (Figure 1). These results reconcile the long-standing controversy between interpretations of ancient vs. recent uplift by providing an uplift history curve for the Colorado Plateau. We amplify stories from frontline communities and build relationships to support grassroots movements across the Colorado Plateau and greater Southwest. Approximately 5 million years ago the Colorado Plateau was uplifted some 1,000 to 1,500m. On the Colorado Plateau, uplift was facilitated by reactivation of preexisting faults and accompanied by tilting of the plateau toward the north. This type of uplift which does not involve deformation is termed epeirogenic uplift. Our initial investigation does not resolve the details of differential uplift between different parts of the plateau, but subsequent sampling of young flows (<9 Ma) may reveal the extent of internal plateau deformation. This type of uplift which does not involve deformation and effects a large area is termed epeirogenic uplift. Its slow rate of uplift was matched by the steady downcutting of the Colorado River and its tributaries, producing the… This phase of uplift and erosion is responsible for nearly all the magnificent landscape features on the Colorado Plateau. The timing of both Colorado plateau uplift and formation of the GrandCanyonremainunresolved,withvariouslinesofevidencesug-gesting episodes of uplift in the Laramide11,12, mid-Cenozoic3,13 and late Cenozoic8,14,15. Well, partly. 1B). Since 10 Ma, the center of uplift continued northeastward from the southwestern rim of the plateau consistent with a young Grand Canyon model and eastward sweep of magmatism in the western Colorado Plateau. The forces that drove rock uplift of the low-relief, high-elevation, tectonically stable Colorado Plateau are the subject of long-standing debate. • Crust beneath the plateau not thick enough to explain its uplift based upon isostatic uplift. plateau were invaded by basaltic magmas6 whose Nd and Sr isotopes indicate an increasingly undepleted mantle source7,10. entire Rocky Mountains and Colorado Plateau were uplifted 4,000 to 6,000 feet. Study of the interaction between uplift and erosion is a major theme of our science, but our understanding of their interplay is often limited by a lack of quantitative data. As for Levander et al, “The timing of both Colorado plateau uplift and formation of the Grand Canyon remain unresolved,” the first line of their paper admitted. Uplift of the Colorado Plateau Paul Withers Introduction to the Colorado Plateau: [2] The Colorado Plateau is a relatively coherent uplifted crustal block surrounded on three sides by the extensional block-faulted regime of the Basin and Range Province and the Rio Grande rift. The uplift increased the stream gradient in the region, and stream downcutting followed. The Laramide Orogeny is a geologic event that occured over the course of 30 million years in the Late Cretacous /Early Tertiary Periods that uplifted the Colorado Plateau from the Cretatous Sea. 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