California River

The river originated in the North American Cordillera of California{{efn|

The California River is named after its headwaters.{{sfn|Wernicke|2009|p=33}}}}{{sfn|Wernicke|2009|p=33}} in the Mojave{{sfn|Ingersoll|Spafford|Jacobson|Grove|2018|p=446}}/Alisitos arc,{{sfn|Davis|Dickinson|Gehrels|Spencer|2010|p=931}} between the Nevadaplano farther north and the Mexicoplano farther south.{{sfn|Ingersoll|Spafford|Jacobson|Grove|2018|p=446}} It then flowed east-northeastward between the Sevier fold-and-thrust belt to the north and the Maria fold-and-thrust belt to the south. It continued northeastward between the Kaibab and the Circle Cliffs uplift and eventually turned due north between the Uncompahgre and San Rafael swells.{{sfn|Davis|Dickinson|Gehrels|Spencer|2010|p=931}} The course of the river extended over {{convert|1000|km}}.{{sfn|Davis|Dickinson|Gehrels|Spencer|2010|p=932}} Ancestral Little Colorado River was a tributary, and the ancestral Mogollon Highlands also drained in this river system.{{sfn|Beard|Karlstrom|Young|Billingsley|2011|p=120}}

The river ended in the Uinta Basin{{sfn|Cather|Chapin|Kelley|2012|p=1181}}{{efn|

This is unlike drainages in the southeastern half of the Colorado Plateau which formed river deltas on the western shore of the Western Interior Seaway and the area of the Gulf of Mexico. Other rivers drained into closed basins.{{sfn|Cather|Chapin|Kelley|2012|p=1181}}}} and Lake Uinta in present-day Utah{{sfn|Smith|Carroll|Scott|2015|p=72}} roughly where the Green River exits the basin,{{sfn|Wang|Plink-Björklund|2019|p=911}} forming a river delta that today comprises the voluminous Colton Formation{{sfn|Davis|Dickinson|Gehrels|Spencer|2010|p=931}} and with its sediment covering an area of over {{convert|3000|km2}}.{{sfn|Foreman|Rasmussen|2016|p=1352}} The so-called "Sunnyside Delta" has also been interpreted as a product of the California River.{{sfn|Wang|Plink-Björklund|2019|p=895}}

In the Paleocene, this river system may have formed the headwater of river systems that ended in the Gulf of Mexico{{sfn|Pettit|Blum|Pecha|McLean|2019|p=284}} through a paleo-Platte River{{sfn|Pecha|Blum|Gehrels|Sundell|2022|p=285}} and before that it may have drained into the Arctic Ocean.{{sfn|Sharman|Covault|Stockli|Wroblewski|2017|p=189}} A drainage through the Little Colorado River valley towards the San Juan Basin is also possible but there is no evidence,{{sfn|Karlstrom|Crossey|Embid|Crow|2017|p=55}} and petrological information on sediments excludes that the Piceance Creek Basin as an endpoint of California River waters.{{sfn|Foreman|Rasmussen|2016|p=1353}}

This river system was of similar scale to the present-day Colorado River-Green River system, but with opposite direction.{{sfn|Beard|Karlstrom|Young|Billingsley|2011|p=80}} Analogies have been drawn between the California River and the present-day Ili River in Central Asia, both in terms of its geomorphology and the sizes and shapes of their deltas and terminal lakes.{{sfn|Wang|Plink-Björklund|2019|p=913}}

The river had a high{{sfn|Wernicke|2009|p=33}} but variable discharge, which has been documented from the delta deposits.{{sfn|Wang|Plink-Björklund|2019|p=913}}

The age of the Western Grand Canyon is controversial, with evidence both of an old Mesozoic and a young Neozoic age. In the former case,{{sfn|Flowers|Farley|Ketcham|2015|p=430}} it is possible that the river created an early Grand Canyon during the Campanian{{sfn|Wernicke|2009|p=33}} or the Paleocene.{{sfn|Gehrels|2014|p=138}}

The California River has been proposed to explain the origin of the deltaic Colton Formation, as it has a high volume and similar source rocks are rare in the area of the Uinta Basin. Rock formations of similar origin occur in southeastern California and southwestern Arizona{{sfn|Davis|Dickinson|Gehrels|Spencer|2010|p=932}} and may have been located along the same drainage.{{sfn|Davis|Dickinson|Gehrels|Spencer|2010|p=933}} Eroded material from the Kaiparowits Formation probably did not contribute much to the formation of the Colton Formation.{{sfn|Dickinson|Lawton|Pecha|Davis|2012|p=869}} The existence of the California river and whether the river that formed the deltaic Colton Formation and the early Grand Canyon were the same are subject to debate.{{sfn|Karlstrom|Jacobson|Sundell|Eyster|2020|p=1448}}

A similar, but more north-northeasterly drainage to the present-day Kaiparowits Plateau may have existed during the Turonian.{{sfn|Primm|Johnson|Stearns|2018|p=267}} During the Cretaceous and Paleogene, the beginning Laramide orogeny disrupted drainages in what today are the western United States, forming several closed basins where drainage ponded from as far as California.{{sfn|Foreman|Rasmussen|2016|p=1345}} The California River existed in the Paleocene and Eocene.{{sfn|Birgenheier|Berg|Plink-Björklund|Gall|2020|p=584}} During the Paleocene, the collapse of the continental borderland and the Laramide orogeny reversed the course of the California River.{{sfn|Wernicke|2009|p=33}} In the Eocene, the drainage divide migrated northeastward.{{sfn|Ingersoll|Spafford|Jacobson|Grove|2018|p=446}}

{{notelist}}

{{Reflist}}

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• {{cite web|last1=Beard|first1=L.S.|last2=Karlstrom|first2=K.E.|last3=Young|first3=R.A.|last4=Billingsley|first4=G.H.|year=2011|title=CRevolution 2—Origin and evolution of the Colorado River system, workshop abstracts: U.S. Geological Survey Open-File Report 2011–1210|url=https://pubs.usgs.gov/of/2011/1210/}}
• {{cite journal |last1=Birgenheier |first1=L. P. |last2=Berg |first2=M. D. Vanden |last3=Plink-Björklund |first3=P. |last4=Gall |first4=R. D. |last5=Rosencrans |first5=E. |last6=Rosenberg |first6=M. J. |last7=Toms |first7=L. C. |last8=Morris |first8=J. |title=Climate impact on fluvial-lake system evolution, Eocene Green River Formation, Uinta Basin, Utah, USA |journal=GSA Bulletin |date=1 March 2020 |volume=132 |issue=3–4 |pages=562–587 |doi=10.1130/B31808.1 |s2cid=197586166 |url=https://pubs.geoscienceworld.org/gsa/gsabulletin/article/132/3-4/562/571754/Climate-impact-on-fluvial-lake-system-evolution |language=en |issn=0016-7606}}
• {{cite journal |last1=Cather |first1=Steven M. |last2=Chapin |first2=Charles E. |last3=Kelley |first3=Shari A. |title=Diachronous episodes of Cenozoic erosion in southwestern North America and their relationship to surface uplift, paleoclimate, paleodrainage, and paleoaltimetry |journal=Geosphere |date=1 December 2012 |volume=8 |issue=6 |pages=1177–1206 |doi=10.1130/GES00801.1 |language=en|doi-access=free }}
• {{cite journal |last1=Davis |first1=Steven J. |last2=Dickinson |first2=William R. |last3=Gehrels |first3=George E. |last4=Spencer |first4=Jon E. |last5=Lawton |first5=Timothy F. |last6=Carroll |first6=Alan R. |title=The Paleogene California River: Evidence of Mojave-Uinta paleodrainage from U-Pb ages of detrital zircons |journal=Geology |date=1 October 2010 |volume=38 |issue=10 |pages=931–934 |doi=10.1130/G31250.1 |s2cid=129376203 |url=https://pubs.geoscienceworld.org/gsa/geology/article/38/10/931/130122/The-Paleogene-California-River-Evidence-of-Mojave |language=en |issn=0091-7613}}
• {{cite journal |last1=Dickinson |first1=William R. |last2=Lawton |first2=Timothy F. |last3=Pecha |first3=Mark |last4=Davis |first4=Steven J. |last5=Gehrels |first5=George E. |last6=Young |first6=Richard A. |title=Provenance of the Paleogene Colton Formation (Uinta Basin) and Cretaceous–Paleogene provenance evolution in the Utah foreland: Evidence from U-Pb ages of detrital zircons, paleocurrent trends, and sandstone petrofacies |journal=Geosphere |date=1 August 2012 |volume=8 |issue=4 |pages=854–880 |doi=10.1130/GES00763.1 |language=en|doi-access=free }}
• {{cite journal |last1=Flowers |first1=Rebecca M. |last2=Farley |first2=Kenneth A. |last3=Ketcham |first3=Richard A. |title=A reporting protocol for thermochronologic modeling illustrated with data from the Grand Canyon |journal=Earth and Planetary Science Letters |date=15 December 2015 |volume=432 |pages=425–435 |doi=10.1016/j.epsl.2015.09.053 |language=en |issn=0012-821X|doi-access=free }}
• {{cite journal |last1=Foreman |first1=Brady Z. |last2=Rasmussen |first2=Dirk M. |title=Provenance Signals In the Piceance Creek Basin: Unroofing of the Sawatch Range and Extent of the Early Paleogene California River System (Colorado, U.S.A.)B.Z. FOREMAN AND D.M. RASMUSSENPROVENANCE OF THE WASATCH FORMATION (PICEANCE CREEK BASIN, COLORADO, U.S.A.) |journal=Journal of Sedimentary Research |date=1 December 2016 |volume=86 |issue=12 |pages=1345–1358 |doi=10.2110/jsr.2016.81 |url=https://pubs.geoscienceworld.org/sepm/jsedres/article/86/12/1345/257124 |language=en |issn=1527-1404}}
• {{cite journal |last1=Gehrels |first1=George |title=Detrital Zircon U-Pb Geochronology Applied to Tectonics |journal=Annual Review of Earth and Planetary Sciences |date=30 May 2014 |volume=42 |issue=1 |pages=127–149 |doi=10.1146/annurev-earth-050212-124012|doi-access=free }}
• {{Citation|last1=Ingersoll|first1=Raymond V.|title=Provenance, paleogeography, and paleotectonic implications of the mid-Cenozoic Sespe Formation, coastal southern California, USA|date=2018|url=https://pubs.geoscienceworld.org/books/book/2118/chapter/115921132|work=Tectonics, Sedimentary Basins, and Provenance: A Celebration of the Career of William R. Dickinson|publisher=Geological Society of America|language=en|doi=10.1130/2018.2540(20)|isbn=978-0-8137-2540-6|access-date=2020-10-05|last2=Spafford|first2=Claire D.|last3=Jacobson|first3=Carl E.|last4=Grove|first4=Marty|last5=Howard|first5=Jeffrey L.|last6=Hourigan|first6=Jeremy|last7=Pedrick|first7=Jane}}
• {{cite journal |last1=Karlstrom |first1=K. E. |author-link2= Laura J. Crossey |last2=Crossey |first2=L. J. |last3=Embid |first3=E. |last4=Crow |first4=R. |last5=Heizler |first5=M. |last6=Hereford |first6=R. |last7=Beard |first7=L. S. |last8=Ricketts |first8=J. W. |last9=Cather |first9=S. |last10=Kelley |first10=S. |title=Cenozoic incision history of the Little Colorado River: Its role in carving Grand Canyon and onset of rapid incision in the past ca. 2 Ma in the Colorado River System |journal=Geosphere |date=1 February 2017 |volume=13 |issue=1 |pages=49–81 |doi=10.1130/GES01304.1 |language=en|doi-access=free }}
• {{cite journal |last1=Karlstrom |first1=Karl E. |last2=Jacobson |first2=Carl E. |last3=Sundell |first3=Kurt E. |last4=Eyster |first4=Athena |last5=Blakey |first5=Ron |last6=Ingersoll |first6=Raymond V. |last7=Mulder |first7=Jacob A. |last8=Young |first8=Richard A. |last9=Beard |first9=L. Sue |last10=Holland |first10=Mark E. |last11=Shuster |first11=David L. |last12=Winn |first12=Carmen |author-link13= Laura J. Crossey |last13=Crossey |first13=Laura |title=Evaluating the Shinumo-Sespe drainage connection: Arguments against the "old" (70–17 Ma) Grand Canyon models for Colorado Plateau drainage evolution |journal=Geosphere |date=1 December 2020 |volume=16 |issue=6 |pages=1425–1456 |doi=10.1130/GES02265.1 |language=en|doi-access=free |hdl=2440/135048 |hdl-access=free }}
• {{Citation |last1=Pecha |first1=Mark E. |title=Linking the Gulf of Mexico and Coast Mountains batholith during late Paleocene time: Insights from Hf isotopes in detrital zircons |date=2022-05-03 |url=https://pubs.geoscienceworld.org/gsa/books/edited-volume/2332/chapter/132965445/Linking-the-Gulf-of-Mexico-and-Coast-Mountains |work=Tectonic Evolution of the Sevier-Laramide Hinterland, Thrust Belt, and Foreland, and Postorogenic Slab Rollback (180–20 Ma) |pages=265–292 |editor-last=Craddock |editor-first=John P. |access-date=2023-04-05 |publisher=Geological Society of America |language=en |doi=10.1130/2021.2555(10) |isbn=978-0-8137-2555-0 |last2=Blum |first2=Michael D. |last3=Gehrels |first3=George E. |last4=Sundell |first4=Kurt E. |last5=Karlstrom |first5=Karl E. |last6=Gonzales |first6=David A. |last7=Malone |first7=David H. |last8=Mahoney |first8=J. Brian |editor2-last=Malone |editor2-first=David H. |editor3-last=Foreman |editor3-first=Brady Z. |editor4-last=Konstantinou |editor4-first=Alexandros|via=ResearchGate}}
• {{cite journal |last1=Pettit |first1=Bridget S. |last2=Blum |first2=Mike |last3=Pecha |first3=Mark |last4=McLean |first4=Noah |last5=Bartschi |first5=Nicolas C. |last6=Saylor |first6=Joel E. |title=Detrital-Zircon U-Pb Paleodrainage Reconstruction and Geochronology of the Campanian Blackhawk–Castlegate Succession, Wasatch Plateau and Book Cliffs, Utah, U.S.A. |journal=Journal of Sedimentary Research |date=11 April 2019 |volume=89 |issue=4 |pages=273–292 |doi=10.2110/jsr.2019.18 |s2cid=146547554 |url=https://pubs.geoscienceworld.org/sepm/jsedres/article/89/4/273/570026/Detrital-Zircon-U-Pb-Paleodrainage-Reconstruction |language=en |issn=1527-1404}}
• {{cite journal |last1=Primm |first1=Jonathan W. |last2=Johnson |first2=Cari L. |last3=Stearns |first3=Michael |title=Basin-axial progradation of a sediment supply driven distributive fluvial system in the Late Cretaceous southern Utah foreland |journal=Basin Research |date=April 2018 |volume=30 |issue=2 |pages=249–278 |doi=10.1111/bre.12252|s2cid=133822007 }}
• {{cite journal |last1=Sharman |first1=Glenn R. |last2=Covault |first2=Jacob A. |last3=Stockli |first3=Daniel F. |last4=Wroblewski |first4=Anton F.-J. |last5=Bush |first5=Meredith A. |title=Early Cenozoic drainage reorganization of the United States Western Interior–Gulf of Mexico sediment routing system |journal=Geology |date=1 February 2017 |volume=45 |issue=2 |pages=187–190 |doi=10.1130/G38765.1 |url=https://pubs.geoscienceworld.org/gsa/geology/article/45/2/187/195291/early-cenozoic-drainage-reorganization-of-the |language=en |issn=0091-7613}}
• {{Citation|last1=Smith|first1=Michael Elliot|title=Stratigraphic Expression of Climate, Tectonism, and Geomorphic Forcing in an Underfilled Lake Basin: Wilkins Peak Member of the Green River Formation|date=2015|url=http://link.springer.com/10.1007/978-94-017-9906-5_4|work=Stratigraphy and Paleolimnology of the Green River Formation, Western USA|volume=1|pages=61–102|editor-last=Smith|editor-first=Michael Elliot|place=Dordrecht|publisher=Springer Netherlands|doi=10.1007/978-94-017-9906-5_4|isbn=978-94-017-9905-8|access-date=2020-10-04|last2=Carroll|first2=Alan R.|last3=Scott|first3=Jennifer Jane|series=Syntheses in Limnogeology |editor2-last=Carroll|editor2-first=Alan R.}}
• {{cite journal |last1=Wang |first1=Jianqiao |last2=Plink-Björklund |first2=Piret |title=Stratigraphic complexity in fluvial fans: Lower Eocene Green River Formation, Uinta Basin, USA |journal=Basin Research |date=October 2019 |volume=31 |issue=5 |pages=892–919 |doi=10.1111/bre.12350|s2cid=135391382 }}
• {{cite conference|url=https://gsa.confex.com/gsa/2009AM/webprogram/Paper163056.html|last=Wernicke|first=B.|year=2009|title=The California River and its role in carving Grand Canyon|conference=Geological Society of America Abstracts with Programs|volume=41|issue=7|page=33}}

{{refend}}

• {{Cite thesis|title=Probabilistic source-to-sink analysis of the provenance of the California paleoriver : implications for the early Eocene paleogeography of western North America|url=https://mountainscholar.org/handle/11124/170973|publisher=Colorado School of Mines. Arthur Lakes Library|date=2017|degree=Thesis|first=Evan Rhys|last=Jones|ref=none}}

Category:Former rivers

Category:Cretaceous North America

Category:Paleogene North America

Category:Natural history of Utah

Category:Natural history of California