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  2. Alluvial fan - Wikipedia

    en.wikipedia.org/wiki/Alluvial_fan

    Alluvial fans are common in the geologic record, such as in the Triassic basins of eastern North America and the New Red Sandstone of south Devon. Such fan deposits likely contain the largest accumulations of gravel in the geologic record. Alluvial fans have also been found on Mars and Titan, showing that fluvial processes have occurred on ...

  3. Northern Basin and Range ecoregion - Wikipedia

    en.wikipedia.org/wiki/Northern_Basin_and_Range...

    The Northern Basin and Range ecoregion is a Level III ecoregion designated by the United States Environmental Protection Agency (EPA) in the U.S. states of Oregon, Idaho, Nevada, Utah, and California. It contains dissected lava plains, rolling hills, alluvial fans, valleys, and scattered mountain ranges in the northern part of the Great Basin.

  4. Bridgeport Valley - Wikipedia

    en.wikipedia.org/wiki/Bridgeport_Valley

    Thus a major portion of the valley floor actually lies on a large alluvial fan formed by Robinson Creek sediment deposits to the southwest, where the creek exits out of the mountains into the Bridgeport Valley. The channels of the alluvial fan branch out towards the north, northeast and east creating a highly fertile and well-watered grassy region.

  5. Geology of the Death Valley area - Wikipedia

    en.wikipedia.org/wiki/Geology_of_the_Death...

    In this arid environment, alluvial fans form at the mouth of these streams. Very large alluvial fans merged to form continuous alluvial slopes called bajadas along the Panamint Range. [33] The faster uplift along the Black Mountains formed much smaller alluvial fans because older fans are buried under playa sediments before they can grow too large.

  6. Los Angeles Basin - Wikipedia

    en.wikipedia.org/wiki/Los_Angeles_Basin

    This bed sequence indicates an alluvial fan, meandering stream or braided stream origin. [11] Upward from the Sespe Formation toward the Vaqueros, the grains become finer and the beds become thinner; indicating a transition to a shallow marine environment. The Vaqueros Formation is marked by two sandstone, siltstone and shale units.

  7. Abyssal fan - Wikipedia

    en.wikipedia.org/wiki/Abyssal_fan

    Abyssal (or submarine) fans are formed from turbidity currents. These currents begin when a geologic activity pushes sediments over the edge of a continental shelf and down the continental slope, creating an underwater landslide. A dense slurry of muds and sands speeds towards the foot of the slope, until the current slows. The decreasing ...

  8. Certified Unified Program Agency - Wikipedia

    en.wikipedia.org/wiki/Certified_Unified_Program...

    California Uniform Fire Code: Hazardous Material Management Plans and Hazardous Material Inventory Statements - Office of the State Fire Marshal (CAL FIRE-OSFM) [2] The mission of the Unified Program is to protect public health and safety, to restore and enhance environmental quality, and to sustain economic vitality through effective and ...

  9. Chino Creek - Wikipedia

    en.wikipedia.org/wiki/Chino_Creek

    Chino Creek rises from underground in a storm water channel flowing southwards from a subdivision in southern Pomona, eastern Los Angeles County.. The concrete channelized stream soon enters southwestern San Bernardino County and runs generally southeast across the Chino Valley between the Chino Hills to the south, and the city of Chino to the northeast.

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