The Aspen anomaly coincides with the highest region of the Rocky Mountains (such as the San Juan Mountains and the Sawatch Range[6]) and divergent drainages (Arkansas River, Colorado River and Gunnison River) which have cut deep gorges. This region underwent significant uplift during the Cenozoic[3] starting from 10-5 million years ago and was subsequently eroded by the Colorado River.[7] Ongoing present-day uplift of the San Juan Mountains may be linked to the Aspen anomaly.[5]
River knickpoints in Gore Canyon and Black Canyon may mark the point at which the rivers pass through the edge of the region above the anomaly.[8] The Colorado River may be influenced by the anomaly all the way to Lees Ferry, Arizona.[9]
In seismic tomography images, the Aspen anomaly is characterized by a northwards tilted low seismic velocity anomaly.[12] The anomaly is one among several low velocity anomalies beneath the western United States, although unlike the others known as the Jemez, Yellowstone and St. George it does not have a northeastward throw.[2] Other structures that may be related to the Aspen anomaly are the Lester Mountain zone, the Colorado mineral belt and the Rio Grande Rift.[13] The Aspen anomaly has been compared with the Yellowstone hotspot,[3] but it lacks a volcanic caldera that Yellowstone has.[5]
Origin
The Aspen anomaly has been interpreted in several ways.
It may be a mantle plume, but the steep tilt angle is unusual for a mantle plume.[12]
It may be a lithospheric melt zone, but the lithosphere is not thick enough to contain such a structure.[14]
It may be a Proterozoic structure, maybe the leftover of a subduction zone.[13] Prolonged subduction would have enriched a segment of mantle with water and thus lowered its melting point.[15]
^ abcCoblentz, D.D.; van Wijk, J. (December 2007). "Mechanisms of Topographic Uplift for the Southern Rocky Mountains". AGU Fall Meeting Abstracts. 2007: T11C–0723. Bibcode:2007AGUFM.T11C0723C.
^Reiter, Marshall (1 March 2008). "Geothermal anomalies in the crust and upper mantle along Southern Rocky Mountain transitions". GSA Bulletin. 120 (3–4): 439. doi:10.1130/B26198.1. ISSN0016-7606.
^E., Karlstrom, K.; D., Coblentz, D.; B., Ouimet, W.; E., Kirby; W., van Wijk, J.; B., Schmandt; J., Crossey, L.; R., Crow; S., Kelley (December 2009). "Dynamic uplift of the Colorado Rockies and western Colorado Plateau in the last 6 Ma driven by mantle flow and buoyancy: Evidence from the Colorado River region". AGU Fall Meeting Abstracts. 2009: T51F–04. Bibcode:2009AGUFM.T51F..04K.{{cite journal}}: CS1 maint: multiple names: authors list (link)
^A., Darling; K., Karlstrom; E., Kirby; W., Ouimet; D., Coblentz; A., Aslan (2008). "Evaluating Neogene Uplift and Denudational History of the Colorado Rockies Using River Profiles and Incision Records". AGU Fall Meeting Abstracts. 2008: T11C–1893. Bibcode:2008AGUFM.T11C1893D.
^M., Sandoval; D., Coblentz; K., Karlstrom; A., Sussman (2005). "Connecting Topographic Analysis With Colorado River Incision History: Sensitive Gauges of Neotectonics in the Rocky Mountains". AGU Fall Meeting Abstracts. 2005: T23C–0580. Bibcode:2005AGUFM.T23C0580S.
^ abcK., MacCarthy, J.; C., Aster, R.; M., Hansen, S.; C., Stachnik, J.; G., Dueker, K.; E., Karlstrom, K. (2009). "Joint inversion of teleseismic body wave residuals and Joint Inversion of Teleseismic Body Wave Residuals and Bouguer Gravity Data to Constrain the Origin of the Colorado Rockies". AGU Fall Meeting Abstracts. 2009: S13B–1745. Bibcode:2009AGUFM.S13B1745M.{{cite journal}}: CS1 maint: multiple names: authors list (link)
Karlstrom, Karl E.; Whitmeyer, Steven J.; Dueker, Ken; Williams, Michael L.; Bowring, Samuel A.; Levander, Alan R.; Humphreys, E. D.; Keller, G. Randy; Group, CD-ROM Working (2005). "Synthesis of results from the CD-ROM Experiment: 4-D image of the lithosphere beneath the Rocky Mountains and implications for understanding the evolution of continental lithosphere". The Rocky Mountain Region: An Evolving Lithosphere Tectonics, Geochemistry, and Geophysics. Geophysical Monograph Series. Vol. 154. American Geophysical Union (AGU). pp. 421–441. doi:10.1029/154gm31. ISBN978-0-87590-419-1. {{cite book}}: |last9= has generic name (help)