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  2. Hemipelagic sediment - Wikipedia

    en.wikipedia.org/wiki/Hemipelagic_sediment

    Typically, hemipelagic sediment is transported to the continental slope in suspension from river mouths but can be transported by the wind. [3] The rate of deposition of hemipelagic sediment is higher than pelagic sediment but still quite slow. [9] Ordinarily hemipelagic sediments accumulate too rapidly to react chemically with seawater.

  3. Hemiboreal - Wikipedia

    en.wikipedia.org/wiki/Hemiboreal

    The term sometimes denotes the form of climate characteristic of the zone of hemiboreal forests—specifically, the climates designated Dfb, Dwb and Dsb in the Köppen climate classification scheme. On occasion, it is applied to all areas that have long, cold winters and warm (but not hot) summers—which also including areas that are semiarid ...

  4. Deposition (geology) - Wikipedia

    en.wikipedia.org/wiki/Deposition_(geology)

    Kirby R. (2002) [9] takes this concept further explaining that the fines are suspended and reworked aerially offshore leaving behind lag deposits of the main bivalve and gastropod shells separated out from the finer substrate beneath, waves and currents then heap these deposits to form chenier ridges throughout the tidal zone, which tend to be ...

  5. Hadal zone - Wikipedia

    en.wikipedia.org/wiki/Hadal_zone

    The hadal zone, also known as the hadopelagic zone, is the deepest region of the ocean, lying within oceanic trenches. The hadal zone ranges from around 6 to 11 km (3.7 to 6.8 mi; 20,000 to 36,000 ft) below sea level , and exists in long, narrow, topographic V-shaped depressions.

  6. Climate system - Wikipedia

    en.wikipedia.org/wiki/Climate_system

    The five components of the climate system all interact. They are the atmosphere, the hydrosphere, the cryosphere, the lithosphere and the biosphere. [1]: 1451 Earth's climate system is a complex system with five interacting components: the atmosphere (air), the hydrosphere (water), the cryosphere (ice and permafrost), the lithosphere (earth's upper rocky layer) and the biosphere (living things).

  7. Boreal ecosystem - Wikipedia

    en.wikipedia.org/wiki/Boreal_ecosystem

    A boreal ecosystem is an ecosystem with a subarctic climate located in the Northern Hemisphere, approximately between 50° and 70°N latitude. These ecosystems are commonly known as taiga and are located in parts of North America, Europe, and Asia. [1] The ecosystems that lie immediately to the south of boreal zones are often called hemiboreal ...

  8. Mesopelagic zone - Wikipedia

    en.wikipedia.org/wiki/Mesopelagic_zone

    The science ROV 'Hercules' (IFE/URI/NOAA) during a launch in 2005. Note the array of sampling devices and robotic arms that are used to conduct deep-sea research. There is a dearth of knowledge about the mesopelagic zone so researchers have begun to develop new technology to explore and sample this area.

  9. Climatic geomorphology - Wikipedia

    en.wikipedia.org/wiki/Climatic_geomorphology

    Atolls like Atafu in Tokelau in the Pacific Ocean are landforms associated to tropical climate. No atoll exists outside the tropics. Climatic geomorphology is the study of the role of climate in shaping landforms and the earth-surface processes. [1] An approach used in climatic geomorphology is to study relict landforms to infer ancient ...