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Logo bar of the Alaska Public Lands Information Center which are located in Anchorage, Fairbanks, Tok and Ketchikan
calm waters reflect a sea side glacier in Glacier Bay National Park and Preserve
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Glacial Fun Facts
 

Digital animation of Bear Glacier in Kenai Fjords National Park


Note: This Embedded video resides on the official Alaska National Park YouTube channel

Watch the Audio Described version of this video on YouTube.

This animation uses satellite imagery and digital elevation information to create a 3-D model of the Bear Glacier in Kenai Fjords National Park. Created with Geographic Information Systems (GIS) animation, this video simulates what a person would see if they flew over Bear Glacier.

Now that you've seen it, want to learn more about beautiful Bear Glacier?



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NPS/Kent Miller

Impress your friends with your knowledge about glaciers!

  • Glaciers form by snow falling and not melting but building up over hundreds of years. As more snow falls it squishes the snow under it and eventually packs it down so forcefully that it forms ice!

  • Glacial ice is that beautiful glowing blue color because the ice is so dense and hard that only the blue wavelength of light, the one with the most energy, can bounce off. All other wavelengths of light are absorbed by the glacier.
  • How to spot a fake glacier: If someone gives you an ice cube and says it's glacier ice, look for bubbles. A normal ice cube will have one big bubble in the center because it froze from the outside in, squeezing any air bubbles to the middle. But a genuine glacier ice cube will have lots of tiny bubbles in layers because of the years of airy snowflakes that were packed down to form it!

  • Glacier ice is very dense and melts slowly which provides water downstream all summer long. If glaciers melt so much that they disappear, no water can be frozen and stored for the summertime.

  • In Washington state, 75% of water used in the state comes from glaciers!




 
A Black and White photo of Skagway before 1900. A short row of false-front buildings line the right side of a rough dirt road. Spruce trees and mountains are in the background. Did You Know?
Skagway and Dyea were the two major points of entry for miners during the Alaskan Gold Rush. The Lynn Canal is the northernmost point of the Inside Passage.
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