Jump to content

Pasadena orogeny

From Wikipedia, the free encyclopedia

This is an old revision of this page, as edited by OAbot (talk | contribs) at 19:56, 12 April 2020 (Open access bot: doi added to citation with #oabot.). The present address (URL) is a permanent link to this revision, which may differ significantly from the current revision.

Geography of Southern California

Pasadena orogeny is a mountain building event. Conventionally it refers to the formation of mountains in mainly Southern California during the Pleistocene and lasting until the present day; originally it referred to the uplift of the San Gabriel Mountains.

The Pasadena orogeny is a major Late Quaternary[1]-modern event[2] of mountain formation,[1] which took place in the middle or perhaps late Pleistocene[3] or to the present-day.[4] It is also known as the "Coast Ranges orogeny"[3] or considered to be part of the Cascadian orogeny[5] or Alpide Orogeny.[6] Finally, the term "Pasadena orogeny" is sometimes applied to all very recent orogenies around the Pacific Ocean.[7] The type location is close to Pasadena, California in the Transverse Ranges,[8] and originally referred to the fast rise of the San Gabriel Mountains recorded there.[9]

During this orogeny mountain ranges such as the San Bernardino Mountains, San Gabriel Mountains, San Jacinto Mountains, Santa Monica Mountains, Santa Ynez Mountains[10] and the Transverse Ranges grew,[11] as did the northern Channel Islands,[10] the Kettleman Hills anticline in the San Joaquin Valley[12] and the Palos Verdes Hills.[13] Sometimes the concept is limited to the uplift of the Transverse Ranges.[14]

The general uplift of mountains over a length of over 400 kilometres (250 mi) is caused by the collision of the North American Plate with other geologic structures that are attached to the Pacific Plate.[10] This orogeny has resulted in the uplift of mostly north-south trending mountain chains, although some east-west trending uplifts are also found such as the Channel Islands and the Transverse Ranges;[12] much of the uplift took place at the edge of basins.[15] The Pasadena orogeny is accompanied by earthquake activity, which includes tsunami hazards.[16]

Folding accompanying the uplift of the Coast Ranges in Southern California,[3] folding farther north at Morro Bay[17] and the structure of the Santa Barbara Basin[1] and Ventura Basin are consequences of the Pasadena orogeny.[4] The city of Long Beach, California lies within the affected region.[2]

References

  1. ^ a b c Marsaglia, K.M.; Rimkus, K.C.; Behl, R.J. (October 1995), "Provenance of Sand Deposited in the Santa Barbara Basin at Site 893 during the Last 155,000 Years" (PDF), Proceedings of the Ocean Drilling Program, 146 Part 2 Scientific Results, Proceedings of the Ocean Drilling Program, vol. 146–2, Ocean Drilling Program, doi:10.2973/odp.proc.sr.146-2.274.1995, retrieved 2018-11-20
  2. ^ a b Bohannon & Gardner 2004, p. 261.
  3. ^ a b c Davis, W. M. (1932). "Glacial Epochs of the Santa Monica Mountains, California". Proceedings of the National Academy of Sciences of the United States of America. 18 (11): 659–665. Bibcode:1932PNAS...18..659D. doi:10.1073/pnas.18.11.659. JSTOR 85970.
  4. ^ a b Scott, Edward W. (1983). "Petroleum potential of wilderness lands in California; petroleum potential of wilderness lands in the Western United States". Circular: D4. doi:10.3133/cir902D. ISSN 2330-5703.
  5. ^ Bandy, Orville L. (1970). Radiometric Dating and Paleontologic Zonation. Geological Society of America. p. 191. ISBN 9780813721248.
  6. ^ Stille 1936, p. 875.
  7. ^ Stille 1936, p. 849.
  8. ^ Blakey & Ranney 2017, p. 186.
  9. ^ Blakey & Ranney 2017, p. 183.
  10. ^ a b c Blakey & Ranney 2017, p. 31.
  11. ^ Wright, Tom (1987). "Geologic Evolution of the Petroleum Basins of Southern California". Petroleum Geology of Coastal Southern California: 7. {{cite journal}}: Cite journal requires |journal= (help)
  12. ^ a b Stille 1936, p. 869.
  13. ^ HANER, BARBARA E. (1971). "Morphology and Sediments of Redondo Submarine Fan, Southern California". Geological Society of America Bulletin. 82 (9): 2413. Bibcode:1971GSAB...82.2413H. doi:10.1130/0016-7606(1971)82[2413:MASORS]2.0.CO;2.
  14. ^ Blakey & Ranney 2017, p. 197.
  15. ^ Blakey & Ranney 2017, p. 181.
  16. ^ Bohannon & Gardner 2004, p. 262.
  17. ^ Blakey & Ranney 2017, p. 184.

Sources