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Deer Creek, Nevada County, CA
The total length of Deer Creek is approximately 34 miles.
At 3100 feet elevation, the North and South Forks of Deer Creek meet. It flows into Scotts Flat Reservoir at 3069 feet. Deer Creek travels through Nevada City, (2300′) then drops down into Lake Wildwood (1200′). From there, it descends 1100 feet where it converges with the Yuba River below Englebright Dam.
Sixteen Locations Along Deer Creek
- North & South Forks Deer Creek – PDF
- Scotts Flat Reservoir & Spillway – PDF
- Lower Scotts Flat Lake & Spillway – PDF
- Below Lower Scotts Flat Lake – (private land not open to the public) – PDF
- Willow Valley Road – PDF
- Pine Street Bridge in Nevada City – PDF
- Tribute Trail – PDF
- Champion Mine / Newtown Ditch area – PDF
- Little Deer Creek Lane (creek banks are private land not open to the public) – PDF
- Bitney Springs Road and Newtown Road (private land not open to the public) – PDF
- Deer Creek Falls (private land not open to the public) – PDF
- Below Deer Creek Falls (private land not open to the public) – PDF
- Deer Creek entrance to Lake Wildwood (community membership required for access) – PDF
- Lakewildwood Spillway – PDF
- Mooney Flat Road below Lakewildood (private land not open to the public) – PDF
- Mooney Flat Road Bridge & Black Swan Preserve – PDF
Entire length of Deer Creek – PDF
Formation of Deer Creek
The story of Deer Creek begins with the formation of the continent. It was during this phase of geologic time that gold was created.
About 160 million years ago, the ocean floor of the Farallon oceanic plate began sinking below the North American Plate. Tremendous subduction forces heated and drove mineral-rich water through cracks where the two land masses folded. Gold and other minerals cooled in the Smartville Complex, the heart of the Gold Rush in the Sierra Nevada Mountains.
Donner Summit rides at the top of the Smartville batholith, a twenty-five thousand square mile section of solid granite that is mostly under the surface of the Sierra Nevada Mountains.
AAPG – Smartville Terrain
Assembling California, John McPhee
Book: Crow’s Range; An Environmental History of the Sierra Nevada by David Beesley
California in 10 Million Years Lecture – Graham Kent, Scripps Institution of Oceanography
Live Science – ‘Lost’ Tectonic Plate Found Beneath California (2013)
Sci News – Scientists Find Remains of Ancient Tectonic Plate Beneath California (2013)
Smartville Complex – Northern California Geologic Society field trip video series led by Dr. Eldridge M. Moores, Distinguished Professor Emeritus, University of California, Davis
Geological Society of America Abstract
The Smartville Complex comprises a north-trending submarine intrusive-extrusive (ophiolitic) complex, approximately 100km long by 40km wide in the northwestern Sierra Nevada Foothills. Generally from bottom to top, rocks comprise serpentinite (a few exposures), olivine gabbro, and layered gabbro, varitextured massive pyroxene and hornblende gabbro, plagiogranite, massive diabase, sheeted diabase, pillow lava, and volcaniclastic sediments. A few massive sulfide deposits are present in the volcaniclastic sediments. Rocks range from nearly undeformed–perhaps the best-preserved sheeted dikes and pillow lavas in North America–to highly schistose. Structure is complex, but rocks describe approximately a north-trending antiform that structurally overlies mélange and associated sediments of the Central Belt of the Sierra Nevada. Dikes intrude both igneous rocks and here and there Central Belt sedimentary rocks. Dikes are mostly north-trending, but curve to NE-trending towards the N. In places (Stanfield Hill, Marysville Road) the dikes are nearly undeformed, trending NNW and dipping steeply E. In other places, e.g. in Auburn, Oroville Dam south abutment, and along the E. side of the complex, dikes and other rocks are highly foliated.
Volcanic rocks compositionally are mostly island-arc tholeiites and oceanic andesites, although MORB compositions have been reported in a few places. Tectonic relations with underlying rocks include a tectonic window near Higgins Corner, a half-window north of Lake Oroville and the high-angle Wolf Creek Fault zone and continuations on the eastern side. On the west, the Smarville and associated rocks are covered by Great Valley deposits and/or intruded by subsequent granitic plutons. Associated ophiolitic rocks include the older Lake Combie Complex, east of SR 49, and the approximately 200 Ma Jarbo Gap and Slate Creek Complexes N and NE of the Smartville complex.
The Smartville complex and associated ophiolites may have been emplaced by collision of one or more west-dipping subduction zones with the North American Continental Margin (or with the western margin of the “Rubia” ribbon continent” of Hildebrand, 2009 GSA Sp. Pap. 457.
Following is part of an Introduction to Physical Geology video course from the City College of San Francisco (Katryn Wiese). Videos below discuss how to identify minerals (formed by organic debris or volcanic glass) igneous (formed by lava), sedimentary (formed by compaction), and metamorphic (formed by pressure & temperature) rocks.
More About Minerals
Identifying Igneous Rock
Identifying Sedimentary Rock
Identifying Metamorphic Rock