scholarly journals Supplemental Material: Redefining the age of the lower Colorado River, southwestern United States

2021 ◽  
Author(s):  
Ryan Crow ◽  
et al.

Additional details on methods, summary of previous Ar/Ar dating relevant to the timing of Colorado River integration, sample locations, and full analytical results.<br>

2021 ◽  
Author(s):  
Ryan Crow ◽  
et al.

Additional details on methods, summary of previous Ar/Ar dating relevant to the timing of Colorado River integration, sample locations, and full analytical results.<br>


Author(s):  
Laura M. Norman ◽  
Michael Gishey ◽  
Leila Gass ◽  
Brian Yanites ◽  
Edwin Pfeifer ◽  
...  

Geology ◽  
2021 ◽  
Vol 49 (9) ◽  
pp. e532-e533
Author(s):  
R.S. Crow ◽  
J. Schwing ◽  
K.E. Karlstrom ◽  
M. Heizler ◽  
P.A. Pearthree ◽  
...  

Geology ◽  
2021 ◽  
Vol 49 (9) ◽  
pp. e531-e531
Author(s):  
Rebecca J. Dorsey ◽  
Gary J. Axen ◽  
Martin J. Grove ◽  
Bernard A. Housen ◽  
George Jefferson ◽  
...  

Geology ◽  
2021 ◽  
Author(s):  
R.S. Crow ◽  
J. Schwing ◽  
K.E. Karlstrom ◽  
M. Heizler ◽  
P.A. Pearthree ◽  
...  

Sanidine dating and magnetostratigraphy constrain the timing of integration of the lower Colorado River (southwestern United States and northern Mexico) with the evolving Gulf of California. The Colorado River arrived at Cottonwood Valley (Nevada and Arizona) after 5.24 Ma (during or after the Thvera subchron). The river reached the proto–Gulf of California once between 4.80 and 4.63 Ma (during the C3n.2r subchron), not at 5.3 Ma and 5.0 Ma as previously proposed. Duplication of section across newly identified strands of the Earthquake Valley fault zone (California) probably explains the discrepancy. The data also imply the start of focused plate motion and basin development in the Salton Trough (California) at 6–6.5 Ma and relative tectonic stability of the southernmost part of the lower Colorado River corridor after its integration. After integration, the Colorado River quickly incised through sediment-filled basins and divides between them as it also likely excavated Grand Canyon (Arizona). The liberated sediment from throughout the system led to deposition of hundreds of meters of Bullhead Alluvium downstream of Grand Canyon after 4.6 Ma as the river adjusted to its lower base level.


2008 ◽  
Vol 41 (3) ◽  
pp. 322-335 ◽  
Author(s):  
Edward P. Glenn ◽  
Kate Hucklebridge ◽  
Osvel Hinojosa-Huerta ◽  
Pamela L. Nagler ◽  
Jennifer Pitt

<em>Abstract.</em>—The lower Colorado is among the most regulated rivers in the world. It ranks as the fifth largest river in volume in the coterminous United States, but its flow is fully allocated and no longer reaches the sea. Lower basin reservoirs flood nearly one third of the river channel and store 2 years of annual flow. Diverted water irrigates 1.5 million ha of cropland and provides water for industry and domestic use by 22 million people in the southwestern United States and northern Mexico. The native fish community of the lower Colorado River was among the most unique in the world, and the main stem was home to nine freshwater species, all of which were endemic to the basin. Today, five are extirpated, seven are federally endangered, and three are being reintroduced through stocking. Decline of the native fauna is attributed to predation by nonnative fishes and physical habitat degradation. Nearly 80 alien species have been introduced, and more than 20 now are common. These nonnative species thrived in modified habitats, where they largely eliminated the native kinds. As a result, the lower Colorado River has the dubious distinction of being among the few major rivers of the world with an entirely introduced fish fauna.


2012 ◽  
Vol 430 ◽  
pp. 237-245 ◽  
Author(s):  
Tammy L. Jones-Lepp ◽  
Charles Sanchez ◽  
David A. Alvarez ◽  
Doyle C. Wilson ◽  
Randi-Laurant Taniguchi-Fu

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