- During the last ice age the Patagonian Ice Sheet created the elongated and forested drumlins seen south of Puerto Williams, Chile.
- Here, you can watch a seminar I gave about the Patagonian Ice Sheet: Further reading
- Northern Patagonian Ice Sheet Perito Moreno Glacier Argen Flickr. 1023 x 685 · JPG. Patagonia Glaciers Ushuaia Southern Patagonian Ice Field.
- As such, ice advances before the gLGM in the southernmost part of the Patagonian Ice Sheet are likely to indicate a wider climatic forcing at this time.
- In order to better understand the region's potential contribution to sea level rise, scientists wanted to more accurately characterize the size of Patagonia's ice sheets.
- We use these data to generate new empirical reconstructions of the Patagonian Ice Sheet (PIS) and subsequent ice masses and ice-dammed palaeolakes at 35 ka...
- @article{076a70930d0b4414acaa7d11043aa6ea, title = "The evolution of the Patagonian Ice Sheet from 35 ka to the Present Day (PATICE)"
- The Patagonian Ice Sheet was a massive ice sheet in what is now Chile and western Argentina around 20,000 years ago.
- 1756 1757 5.4.3 Ice sheet reconstruction 1758 Figure 25 shows our ice sheet reconstruction for the Southern Patagonian Icefield section.
- Patagonia is home to the largest ice fields in the Southern Hemisphere outside Antarctica, and its glaciers are among the fastest-moving in the world.
- The Patagonian Ice Sheet was an ice sheet characterised by a wide variety of environments, including glaciolacustrine, land-terminating lowland lobes...
- The Patagonian Ice Sheet was a large elongated and narrow ice sheet centered in the southern Andes that existed during the Llanquihue glaciation.
- John L and Thorndycraft, Varyl R (2020) The evolution of the Patagonian Ice Sheet from 35 ka to the present day (PATICE).
