Glacier size is dependent on snowfall and temperature.
Valley glaciers are narrower and longer, flowing through valleys and carving deep U-shaped valleys. Continental glaciers are wider and thicker, covering large land areas and shaping landscapes through erosion and deposition. Valley glaciers are more localized in their impact, while continental glaciers have a broader influence on the land.
The two main types of glaciers are alpine glaciers, which form in mountainous regions and flow down valleys, and ice sheets, which are massive continental glaciers that cover large areas of land. Alpine glaciers are smaller and more common, while ice sheets are much larger and thicker.
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.
Two types of glaciers are valley glaciers, which flow down valleys, and ice sheets, which cover large land areas. Valley glaciers are narrower and are found in mountainous regions, while ice sheets are massive and cover extensive areas.
The two remaining continental glaciers are Antarctica and Greenland. While Greenland is part of North America and located between the Arctic and Atlantic Oceans, Antarctica is situated at the South Pole.
Two kinds of glaciers are valley glaciers and ice sheets. Valley glaciers are long, narrow glaciers that form in mountain valleys, while ice sheets are vast, continent-sized glaciers that cover large land areas. The main difference is in their size and location, with valley glaciers typically being smaller and found in mountainous regions, while ice sheets are much larger and exist in polar regions.
Porosity refers to the measure of how much of a rock is open space. The two factors concerning particles in a rock that have the greatest effect on the rock's porosity are shape and distribution.
There are two syllables in the word 'glaciers'.
Increase: Survival and Immigration Decrease: Death and Emigration
Mass as well as distance.
Continental and Valley Glaciers.
Two factors that affect a planets revolution are distance from the sun and size.
Valley glaciers are narrower and longer, flowing through valleys and carving deep U-shaped valleys. Continental glaciers are wider and thicker, covering large land areas and shaping landscapes through erosion and deposition. Valley glaciers are more localized in their impact, while continental glaciers have a broader influence on the land.
The two factors that determine the strength of the Coriolis effect are the rotation speed of the Earth and the latitude of the location. The effect is strongest at the poles and weakest at the equator due to the Earth's rotational speed and curvature.
It is valley and continental glaciers they are different because continental glaciers are the largest, and valley glaciers are on the top of mountain peaks.
franz josef and fox glaciers
Synergistic effect refers to the interaction of two or more factors or substances that results in a combined effect greater than the sum of their individual effects. In other words, when two substances or factors work together, their combined effect is stronger than expected based on their individual effects.