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Eaton Canyon Field Presentation

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Aaron Chiang
Aaron Chiang

Eaton Canyon is located within the San Gabriel Mountains near Los Angeles, California. The canyon and mountains contain various igneous and metamorphic rocks, including diorite, granodiorite, and granite pegmatite, which formed from the subduction of the Farallon plate underneath the North American plate. These mountains were later disrupted by movement along the San Andreas Fault and related faults. Today, Eaton Canyon is home to plants like prickly pear cactus and animals such as coyotes, with its waterfall providing a water source. The surrounding mountains further the region's ecosystems by blocking hot and dry air from the Mojave Desert.

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Eaton Canyon and the San Gabriel Mountains By Aaron Chiang
Background information Eaton canyon is the main emphasize, but the canyon itself is a small part of the San Gabriel Mountains Eaton Canyon itself doesnt have specific history, but is just part of San Gabriel Mountains history
What types of rocks are present? (Eaton Canyon) Diorite (right picture) Granidiorite (right picture) Granite Pegmatite (left picture)
Rocks: How they formed Oldest rock: Pelona Schist (not seen on the trip there) (Nourse, 2002) Thought to have formed from the subduction of the now destroyed Farallon plate underneath the North American plate during the Paleocene. (Nourse, 2002) The San Gabriel Mountains contain mainly igneous and metamorphic rocks that were disrupted and broken by faults that delineate the boundary between the North American and Pacific plate. (Nourse, 2002) The boundary between these two plates started forming in the late Cenozoic, particularly the Miocene. This fault is the famous San Andreas fault (Nourse, 2002)
Rocks: How they formed (cont.) San Gabriel Mountains are bounded by the San Andreas fault (right-lateral) to the north and the Sierra Madre-Cucamonga fault system (thrust) to the south (Nourse, 2002) The San Gabriel Mountains were formed because the San Andreas fault 'jogs' to the east along this area, creating tension between the southern block wanting to move northward and the north block moving south. In addition to this, the Sierra Madre-Cucamonga thrust fault exerts a compressional force against the rocks. The mountains are "currently experiencing a state of transpression" (Nourse, 2002, p. 175).
Rocks: How they formed (cont.) Through palinspastic reconstructions done by multiple geologists, it seems that the rocks in the San Gabriel Mountains were once connected to the rocks found in Orocopia and Chocolate Mountains in the south. When right- lateral movement was initiated through the birth of the San Andreas fault, it moved some of these rocks northward. (Nourse, 2002) San Gabriel Mountains:
Plants & Animals The prickly-pear cactus is "most common in disturbed areas such as land once cleared by man" (Vaughan, 1954). It serves as food for many animals like rats, mice, and rabbits. The coyote is the most dominant predator in Eaton Canyon, though it was not seen on the time of the visit (Vaughan, 1954) Evolution of animals and plants in this area are not widely documented in this area.
Ecosystems: Eaton Canyon is known for a waterfall at the end of its short trail. We can assume that animals go there for a drink of water or to cool off in the summer heat. Picture on the left are boulders right before the waterfall
Ecosystem (cont.) The mountains prevent cold ocean air from leaving the coastal basins, keeping them cool. In comparison, the Mojave desert, which is on the other side of the Mountains, receives the brunt of the heat and mostly stays dry. (Vaughan, 1954) The picture is part of a dry river bed along the Eaton Canyon path.
Ecosystems (cont.) The picture listed below shows how the mountains block the heat from the Mojave desert
Bibliography Nourse, J.A. (2002). Middle Miocene reconstruction of the central and eastern San Gabriel Mountains, southern California, with implications for evolution of the San Gabriel fault and Los Angeles basin, in Barth, A., ed., Contributions to Crustal Evolution of the Southwestern United States: Boulder, Colorado, Geological Society of America Special Paper 365, p. 161185. Vaughan, T.A. (1954, November 15). Mammals of the San Gabriel Mountains of California. Naturespace, 7. Retrieved from http://www.naturespeace.org/sangabrielmammals1954.b.htm [San Gabriel Mountains]. Retrieved August 1st, 2013 Fromhttp://kimandgeoff.com/wp-content/gallery/san-gabriel- skiing/p4123190.jpg [San Gabriel Mountain Wind Patterns]. Retrieved August 1st, 2013 From http://latimesblogs.latimes.com/.a/6a00d8341c630a53ef0153929a1b65970b- pi

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Eaton Canyon Field Presentation

  • 1. Eaton Canyon and the San Gabriel Mountains By Aaron Chiang
  • 2. Background information Eaton canyon is the main emphasize, but the canyon itself is a small part of the San Gabriel Mountains Eaton Canyon itself doesnt have specific history, but is just part of San Gabriel Mountains history
  • 3. What types of rocks are present? (Eaton Canyon) Diorite (right picture) Granidiorite (right picture) Granite Pegmatite (left picture)
  • 4. Rocks: How they formed Oldest rock: Pelona Schist (not seen on the trip there) (Nourse, 2002) Thought to have formed from the subduction of the now destroyed Farallon plate underneath the North American plate during the Paleocene. (Nourse, 2002) The San Gabriel Mountains contain mainly igneous and metamorphic rocks that were disrupted and broken by faults that delineate the boundary between the North American and Pacific plate. (Nourse, 2002) The boundary between these two plates started forming in the late Cenozoic, particularly the Miocene. This fault is the famous San Andreas fault (Nourse, 2002)
  • 5. Rocks: How they formed (cont.) San Gabriel Mountains are bounded by the San Andreas fault (right-lateral) to the north and the Sierra Madre-Cucamonga fault system (thrust) to the south (Nourse, 2002) The San Gabriel Mountains were formed because the San Andreas fault 'jogs' to the east along this area, creating tension between the southern block wanting to move northward and the north block moving south. In addition to this, the Sierra Madre-Cucamonga thrust fault exerts a compressional force against the rocks. The mountains are "currently experiencing a state of transpression" (Nourse, 2002, p. 175).
  • 6. Rocks: How they formed (cont.) Through palinspastic reconstructions done by multiple geologists, it seems that the rocks in the San Gabriel Mountains were once connected to the rocks found in Orocopia and Chocolate Mountains in the south. When right- lateral movement was initiated through the birth of the San Andreas fault, it moved some of these rocks northward. (Nourse, 2002) San Gabriel Mountains:
  • 7. Plants & Animals The prickly-pear cactus is "most common in disturbed areas such as land once cleared by man" (Vaughan, 1954). It serves as food for many animals like rats, mice, and rabbits. The coyote is the most dominant predator in Eaton Canyon, though it was not seen on the time of the visit (Vaughan, 1954) Evolution of animals and plants in this area are not widely documented in this area.
  • 8. Ecosystems: Eaton Canyon is known for a waterfall at the end of its short trail. We can assume that animals go there for a drink of water or to cool off in the summer heat. Picture on the left are boulders right before the waterfall
  • 9. Ecosystem (cont.) The mountains prevent cold ocean air from leaving the coastal basins, keeping them cool. In comparison, the Mojave desert, which is on the other side of the Mountains, receives the brunt of the heat and mostly stays dry. (Vaughan, 1954) The picture is part of a dry river bed along the Eaton Canyon path.
  • 10. Ecosystems (cont.) The picture listed below shows how the mountains block the heat from the Mojave desert
  • 11. Bibliography Nourse, J.A. (2002). Middle Miocene reconstruction of the central and eastern San Gabriel Mountains, southern California, with implications for evolution of the San Gabriel fault and Los Angeles basin, in Barth, A., ed., Contributions to Crustal Evolution of the Southwestern United States: Boulder, Colorado, Geological Society of America Special Paper 365, p. 161185. Vaughan, T.A. (1954, November 15). Mammals of the San Gabriel Mountains of California. Naturespace, 7. Retrieved from http://www.naturespeace.org/sangabrielmammals1954.b.htm [San Gabriel Mountains]. Retrieved August 1st, 2013 Fromhttp://kimandgeoff.com/wp-content/gallery/san-gabriel- skiing/p4123190.jpg [San Gabriel Mountain Wind Patterns]. Retrieved August 1st, 2013 From http://latimesblogs.latimes.com/.a/6a00d8341c630a53ef0153929a1b65970b- pi