Pilvandmeid

Pilvandmeid is a geological formation in the state of Alaska, United States. Specifically, it is located in the Wrangell-St. Elias National Park and Preserve, which is the largest national park in the US.

The name "Pilvandmeid" is derived from the Athabascan language and translates to "grass fence" or "fence of grass". This refers to a unique natural formation within the park that resembles a series of narrow ridges and hills.

Pilvandmeid is characterized by a series of distinctive glacial moraines, which are remnant deposits of rocks and soil left behind by the retreating ice of the gigantic Malaspina Glacier. The formation results from the interaction of tectonic forces and glacial erosion, demonstrating the park's complex and varied geological history.

From a visitor's perspective, Pilvandmeid offers opportunities for geo-tourism and appreciation of the natural landscapes shaped by these geological forces. Visitors may access the area via a designated trail, allowing for a closer exploration of this unique glacial landscape. The surrounding Wrangell-St. Elias National Park and Preserve is renowned for its extensive, untouched wilderness areas that showcase an unparalleled range of geological features.

It is worth noting that considerable scientific research has taken place in and around Pilvandmeid. Studies of glacial geomorphology have led to the development of new understanding of the Balto-Silique glaciation and give greater insight into the workings of these complex glacial dynamics.