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  2. Hemipelagic sediment - Wikipedia

    en.wikipedia.org/wiki/Hemipelagic_sediment

    The composition of Hemipelagic sediment directly depends on the composition of the adjacent land mass and geologic events such as volcanism that influence sediment input into the ocean. [7] [8] Hemipelagic sediments are mainly terrigenous but can also have biological oozes from marine organisms like Radiolarians or Diatoms.

  3. Template:Climate chart - Wikipedia

    en.wikipedia.org/wiki/Template:Climate_chart

    Climate charts provide an overview of the climate in a particular place. The letters in the top row stand for months: January, February, etc. The bars and numbers convey the following information: The blue bars represent the average amount of precipitation (rain, snow etc.) that falls in each month.

  4. File:Köppen-Geiger Climate Zones of Florida.pdf - Wikipedia

    en.wikipedia.org/wiki/File:Köppen-Geiger_Climate...

    It is recommended to name the SVG file “Köppen-Geiger Climate Zones of Florida.svg”—then the template Vector version available (or Vva) does not need the new image name parameter. Summary Description Köppen-Geiger Climate Zones of Florida.pdf

  5. File:European Climate Zones.pdf - Wikipedia

    en.wikipedia.org/.../File:European_Climate_Zones.pdf

    European_Climate_Zones.pdf (600 × 450 pixels, file size: 1.19 MB, MIME type: application/pdf) This is a file from the Wikimedia Commons . Information from its description page there is shown below.

  6. Holdridge life zones - Wikipedia

    en.wikipedia.org/wiki/Holdridge_life_zones

    The Holdridge life zones system is a global bioclimatic scheme for the classification of land areas. It was first published by Leslie Holdridge in 1947, and updated in 1967. It is a relatively simple system based on few empirical data, giving objective criteria. [ 1 ]

  7. List of life zones by region - Wikipedia

    en.wikipedia.org/wiki/List_of_life_zones_by_region

    The climate and ecology of different locations on the globe naturally separate into life zones, depending on elevation, latitude, and location.The generally strong dependency on elevation is known as altitudinal zonation: the average temperature of a location decreases as the elevation increases.

  8. Morphoclimatic zones - Wikipedia

    en.wikipedia.org/wiki/Morphoclimatic_zones

    These zones amounts to about half of Earth's land surface, the remaining half cannot be explained in simple terms by climate-landform interactions. [5] The limitations of morphoclimatic zoning were already discussed by Siegfried Passarge in 1926 who considered vegetation and the extent of weathered material as having more direct impact than ...

  9. Template:KoppenClimate/doc - Wikipedia

    en.wikipedia.org/wiki/Template:KoppenClimate/doc

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