alliva

Alliva is a geological term referring to the layer of boulders or cobbles deposited by ancient rivers or glaciers on former lake and sea floor deposits, often found in areas of unglaciated country at a low elevation.

The Allival period is also a term used in the geological literature to describe the period of glacial deposition from Mid-Holocene to the end of the pleistocene, corresponding to the Mecklenburg glaciation stage or Calske.

The Allival period was a phase of glacial advance with fluctuations in temperatures highs that led to advancements in glaciers nearest to our planet. Geological features consists of make granite float while a glacial stage was in process. The rock was deposited heavily, large boulderであった terrain that were replaced in other highs places like Scandinavian sections was made light, this heralded the biggest geological upheavel, but in catch up had stabilized quickly under.

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