valley glacier - определение. Что такое valley glacier
Diclib.com
Словарь ChatGPT
Введите слово или словосочетание на любом языке 👆
Язык:     

Перевод и анализ слов искусственным интеллектом ChatGPT

На этой странице Вы можете получить подробный анализ слова или словосочетания, произведенный с помощью лучшей на сегодняшний день технологии искусственного интеллекта:

  • как употребляется слово
  • частота употребления
  • используется оно чаще в устной или письменной речи
  • варианты перевода слова
  • примеры употребления (несколько фраз с переводом)
  • этимология

Что (кто) такое valley glacier - определение

GEOMORPHOLOGY OF GLACIERS
Piedmont glacier; Outlet glacier; Valley glacier; Glacial geomorphology; Ice dome; Tidal outlet glacier; Glacier cap
  • Elephant Foot Glacier, a well-known Piedmont glacier in [[Romer Lake]], northeastern [[Greenland]].<ref>[http://earthobservatory.nasa.gov/IOTD/view.php?id=85303&src=eoa-iotd Elephant Foot Glacier] at NASA Earth Observatory</ref>
  • Grosser Aletschgletscher]], [[Bernese Alps]], Switzerland
  • Image of a Cirque Glacier
  • Image of a Piedmont Glacier
  • Southern Patagonia Ice Field from [[ISS]], astronaut photo. North is to the right.

Suárez Glacier         
  • Suárez Glacier (also known as Petzval Glacier) in Skontorp Cove
GLACIER IN GRAHAM LAND, ANTARCTICA
Suarez Glacier; Petzval Glacier
Suárez Glacier also known as Petzval Glacier () is a glacier flowing into the small cove between Skontorp Cove and Sturm Cove on the west coast of Graham Land. It was first mapped by Scottish geologist David Ferguson in 1913–14.
Ferpècle Glacier         
GLACIER IN SWITZERLAND
Glacier de Ferpècle; Ferpecle Glacier
The Ferpècle Glacier () is a long glacier (2005) situated in the Pennine Alps in the canton of Valais in Switzerland. In 1973 it had an area of .
Pūanu Glacier         
ANTARCTIC GLACIER
Puanu Glacier
Pūanu Glacier () is a glacier that occupies the upper portion of Papitashvili Valley in the Apocalypse Peaks of Victoria Land. Pūanu is a Māori word, meaning "intense cold", and was applied descriptively to this glacier in 2005 by the New Zealand Geographic Board.

Википедия

Glacier morphology

Glacier morphology, or the form a glacier takes, is influenced by temperature, precipitation, topography, and other factors. The goal of glacial morphology is to gain a better understanding of glaciated landscapes and the way they are shaped. Types of glaciers can range from massive ice sheets, such as the Greenland ice sheet, to small cirque glaciers found perched on mountain tops. Glaciers can be grouped into two main categories:

  • Ice flow is constrained by the underlying bedrock topography
  • Ice flow is unrestricted by surrounding topography