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Idea 1:
Me as a rat: I'm about to eat so much fucking cheese
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California girls we're unaccountable
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Panama Bread enters peoples lives when they need it the most. Accept them with open arms
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there is a special place in hell for dippy fresh
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o()xxx[{:::::::::::::::::::::::::::::> - - - oxx(:::::::::> - - - oxx(:::::::::>
A quick spin on our melee battle. Dont worry, the damage technically scales to melee so happy battles!! 馃槇馃槇
<Reblog to get a sword.>
o()xxx[{::::::::::::::::::::::::::::>
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Long awaited, here is the soil map of Skyrim using the Canadian System of Soil classification. Brief description of my conclusions under the cut:
Chernozem: Whiterun Hold is likely home to the majority of Skyrim鈥檚 Chernozems. The majority of biological carbon sequestering in grassland environments are below ground, within the root systems. Organic material- humus, builds up, causing the upper layers of the soil to take on a dark colour. Additionally, Solonetzic soils could be present, peppered throughout the hold if the parent material to the soil is salty enough.
Cryosols are formed in Skyrim鈥檚 far North and high alpine regions. The mean annual soil temperature being 0 degrees C, with permafrost conditions. Freeze-thaw cycles lead to permafrost at the soils surface, but also cryoturbation: soil movement arising from frost action.
Additionally in mountainous regions, you would find Regosols. Soils which develop on unstable landforms and have had little time to develop, such as mountain slopes, or river floodplains.
Gleysols occur across the landscape of Skyrim, but primarily in Hjaalmarch. Gleysols are commonly found in depressions or low-lying areas where water saturates the soil continuously, leading to a molted characteristic to the soil.
Organic soils would primarily be found in the water saturated soils of Hjaalmarch. These are wetland soils found in forested areas and are commonly known as peat, muck, bogs or fens.
Borrowing from the USDA soil taxonomy, Inceptisols are light colored soils with moderate alteration, occurring under cool and cold climates. These soils would be found in the Eastmarch caldera.
Luvisols are associated with forested landscapes overlying loamy glacial till, or on clayey lacustrine deposits. Lake Honrich dominates a large portion of the Rift, according to UESP, seemingly draining from the lake. I believe this to be the site of a melted glacier, the lake being meltwater. Clay sediments are associated with lakes because of their deposition, coarser sediments bordering the lake near the shore, and finer particles at the deepest reaches. Additionally, at the end of the Karth river, where sandy deposits would be deposited at Solitude, before the stream looses power further down the river, leaving only clay to be deposited.
Podzols are associated with igneous parent materials, coniferous vegetation and high acidity. Primarily they are found in Falkreath Hold and Southern Eastmarch.
Brunisols are an intermediate stage between Regosols (undeveloped soils), and Podzol or Luvisols. I believe with the unstable, mountainous landscape of the Reach, soils would remain still rather undeveloped. Brunisols would also be interspersed among the Luvisols.
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They should make food for men
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