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  1. 25 paź 2018 · Glaciation: A Very Short Introduction offers an overview of glaciers and ice sheets as systems, considering the role of geomorphology and sedimentology in studying them, and their impacts on our planet in terms of erosional and depositional processes.

  2. Abstract. The ‘glacial theory’ championed by Louis Agassiz in the 19th century saw the beginning of the geological community’s partial acceptance of the concept of multiple and more extensive glaciations. Formal recognition of multiple glaciations came in 1909 with Penck and Brückner’s Alpine model. Since then, research on the Earth ...

  3. An example of a glacial landsystem model, in this case for a typical mid-latitude active temperate glacier: (1) moraines; (2) glacifluvial landforms; (3) glacially overridden landforms and flutings. The typical sediment sequence shows: (i) outwash; (ii) and (iii) deformed sediments or glacitectonite; and (iv) till.

  4. link.springer.com › referenceworkentry › 10Glaciation - SpringerLink

    1 gru 2021 · Definition. A glaciation or glacial period is a geologically short period of time within an ice age characterized by very low surface temperatures and the advance of glaciers.

  5. 1 sty 2014 · Dynamics of glaciers are the resulting ice flow processes caused by the interplay of the physical mechanism causing a glacier to move (gravity) and forces resisting this movement (e.g., friction). Alternatively it can be defined as a glacier’s response to climate change or to other external or internal forcings.

  6. 21 sie 2024 · A glaciation (or ice age) occurs when the Earth’s climate becomes cold enough that continental ice sheets expand, covering large areas of land. Four major, well-documented glaciations have occurred in Earth’s history: one during the Archean-early Proterozoic Eon, ~2.5 billion years ago; another in late Proterozoic Eon, ~700 million years ...

  7. In order to assess the economic damage of a hypothetical return to an ice age, we compute the evolution of average GDP per capita by country with or without the corresponding global cooling, following the methodology described in BHM using the replication data provided with their publication.

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