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  2. Hemipelagic sediment - Wikipedia

    en.wikipedia.org/wiki/Hemipelagic_sediment

    [1] [2] Hemipelagic sediments are deposited on continental shelves and continental rises, and differ from pelagic sediment compositionally. Pelagic sediment is composed of primarily biogenic material from organisms living in the water column or on the seafloor and contains little to no terrigenous material. [ 1 ]

  3. Marine sediment - Wikipedia

    en.wikipedia.org/wiki/Marine_sediment

    Marine sediment, or ocean sediment, or seafloor sediment, are deposits of insoluble particles that have accumulated on the seafloor.These particles either have their origins in soil and rocks and have been transported from the land to the sea, mainly by rivers but also by dust carried by wind and by the flow of glaciers into the sea, or they are biogenic deposits from marine organisms or from ...

  4. Lava-flow hazard zones - Wikipedia

    en.wikipedia.org/wiki/Lava-flow_hazard_zones

    Lava Flow Hazard map of Haleakala. The Maui Hazard Zone numbers are a different scale from the island of Hawaiʻi's map. The lava flow hazard zones on Maui use a different scale. They can be compared to Hawai'i Island's lava zones. [4] [5] Maui Zone 1 - Includes the crater of Haleakalā and some rift zones, mainly areas that have experienced ...

  5. Academician Ridge - Wikipedia

    en.wikipedia.org/wiki/Academician_Ridge

    Academician Ridge is an underwater, structural high separating two of Lake Baikal's three basins, the Central and North basins Situated in the central part of the Baikal Rift, it serves as an "accommodation zone", transferring "motion between faults of similar displacement but different orientation" (Hutchinson et al., 1992).

  6. Continental rise - Wikipedia

    en.wikipedia.org/wiki/Continental_rise

    Because the continental rise lies below the continental slope and is formed from sediment deposition, it has a very gentle slope, usually ranging from 1:50 to 1:500. [1] As the continental rise extends seaward, the layers of sediment thin, and the rise merges with the abyssal plain, typically forming a slope of around 1:1000.

  7. Pelagic zone - Wikipedia

    en.wikipedia.org/wiki/Pelagic_zone

    Altogether, the pelagic zone occupies 1,330 million km 3 (320 million mi 3) with a mean depth of 3.68 km (2.29 mi) and maximum depth of 11 km (6.8 mi). [2] [3] [4] Pelagic life decreases as depth increases. The pelagic zone contrasts with the benthic and demersal zones at the bottom of the sea. The benthic zone is the ecological region at the ...

  8. Do you live in a fire-risk area? These maps show high-risk zones.

    www.aol.com/live-fire-risk-area-maps-203215388.html

    Los Angeles and other areas in California are among the highest-risk areas for wildfires — but they're not the only ones. Many fires take place in areas where humans have overstepped into nature ...

  9. Pelagic sediment - Wikipedia

    en.wikipedia.org/wiki/Pelagic_sediment

    Pelagic sediment or pelagite is a fine-grained sediment that accumulates as the result of the settling of particles to the floor of the open ocean, far from land. These particles consist primarily of either the microscopic, calcareous or siliceous shells of phytoplankton or zooplankton; clay-size siliciclastic sediment; or some mixture of these.