Logo
Unionpedia
Communication
Get it on Google Play
New! Download Unionpedia on your Android™ device!
Free
Faster access than browser!
 

Cordilleran Ice Sheet and Dam

Shortcuts: Differences, Similarities, Jaccard Similarity Coefficient, References.

Difference between Cordilleran Ice Sheet and Dam

Cordilleran Ice Sheet vs. Dam

The Cordilleran ice sheet was a major ice sheet that periodically covered large parts of North America during glacial periods over the last ~2.6 million years. A dam is a barrier that stops or restricts the flow of water or underground streams.

Similarities between Cordilleran Ice Sheet and Dam

Cordilleran Ice Sheet and Dam have 4 things in common (in Unionpedia): Flood, Glacier, Lake Missoula, North America.

Flood

A flood is an overflow of water that submerges land that is usually dry.

Cordilleran Ice Sheet and Flood · Dam and Flood · See more »

Glacier

A glacier is a persistent body of dense ice that is constantly moving under its own weight; it forms where the accumulation of snow exceeds its ablation (melting and sublimation) over many years, often centuries.

Cordilleran Ice Sheet and Glacier · Dam and Glacier · See more »

Lake Missoula

Lake Missoula was a prehistoric proglacial lake in western Montana that existed periodically at the end of the last ice age between 15,000 and 13,000 years ago.

Cordilleran Ice Sheet and Lake Missoula · Dam and Lake Missoula · See more »

North America

North America is a continent entirely within the Northern Hemisphere and almost all within the Western Hemisphere; it is also considered by some to be a northern subcontinent of the Americas.

Cordilleran Ice Sheet and North America · Dam and North America · See more »

The list above answers the following questions

Cordilleran Ice Sheet and Dam Comparison

Cordilleran Ice Sheet has 43 relations, while Dam has 335. As they have in common 4, the Jaccard index is 1.06% = 4 / (43 + 335).

References

This article shows the relationship between Cordilleran Ice Sheet and Dam. To access each article from which the information was extracted, please visit:

Hey! We are on Facebook now! »