Inside Hawaiian Volcanoes

1112

Narrated by Roger Mudd, this video is full of detailed, informative graphics and live action that chronicles the volcanic history of the Hawaiian Islands (e. g. Kilauea and Mauna Loa). The development of the Hawaii islands is due to the five shield volcanoes that erupted during the Pleistocene Period. They are part of a volcanic chain located along the crest of the Hawaiian-Emperor seamount chain. Similarly, glaciation and changes in sea level have effected the geologic formation of the Volcanoes in the National Park. A small icecap that once existed on the volcano of Mauna Kea during the Pleistocene Epoch that resulted in glaciers, and has led to snow falls on both Mauna Kea and Mauna Loa volcanoes. Additionally, changes in the sea level have resulted in land submergence and shorelines decreasing.

No ratings yet.

Please rate this:

LEAVE A REPLY

Please enter your comment!
Please enter your name here

This site uses Akismet to reduce spam. Learn how your comment data is processed.