Mars still has glaciers. Besides the ice caps scientists have discovered glaciers near the equator of mars that are up to half a mile thick.
The planet Mars has glaciers made of water ice, mostly located in its polar regions. These glaciers have been observed by orbiters and are thought to be composed of a mix of water and carbon dioxide ice.
Well, Mars has mountains, volcanoes, and canals, where it is possible water went through a very long time ago. There are also frozen ice glaciers on Mars, except they aren't melting like Earth's are.
Ice has been found on Mars multiple times through observations made by spacecraft, such as the Mars Reconnaissance Orbiter and the Mars Phoenix Lander. The first confirmed discovery of ice on Mars was in 2002 using data collected by NASA's Odyssey orbiter. Additionally, scientists have also found glaciers, ice caps, and frost on the surface of Mars.
Ice Sheets Ice Shelves Ice Caps Ice Streams/Outlet Glaciers Icefields Mountain Glaciers Valley Glaciers Piedmont Glaciers Cirque Glaciers Hanging Glaciers Tidewater Glaciers
There are 2 main types of glaciers, Continental is one, they float away from central regions. The second is alpine or valley which are the glaciers that flow down the valley from the mountain.
Glaciers formed in mountains are called mountain glaciers or alpine glaciers. They are found in high-altitude regions and flow downhill through valleys.
Evidence of ancient water channels, lakes, and glaciers on Mars, suggesting the presence of liquid water in the planet's past. Identification of methane in the Martian atmosphere, hinting at potential microbial life or geological activity. Detection of diverse minerals and geological formations, providing insights into Mars' geological history and potential habitability.
Continental glaciers are thicker and larger. Valley glaciers are formed on mountains; continental glaciers are formed on flat land.
glaciers are very big
there are no glaciers in Ireland
Continental glaciers and valley glaciers are both types of glaciers that form from accumulated snowfall. They both flow under the influence of gravity, albeit in different directions. While continental glaciers cover vast areas like an ice sheet, valley glaciers are confined to mountain valleys and flow down through them.
There are two syllables in the word 'glaciers'.