Earth and Environment Atlas

How The Planet Works
Sign In
Text size
100%
Theme
Geological Formation

Harvard Glacier

Glaciers and Ice Formations

The Harvard Glacier is a large tidewater glacier in Alaska's Prince William Sound. It has a 1.5 mile wide face where it calves into College Fjord, is about 300 feet thick, and covers roughly 120,000 acres of the Chugach National Forest. It is the second largest glacier in Prince William Sound after the Columbia Glacier and is a popular destination for cruise ships touring the sound. This description is adapted from Wikipedia contributors under CC BY-SA 4.0; changes were made. https://creativecommons.org/licenses/by-sa/4.0/

Facts
Classification
Protected Status
National Park or Reserve 1
Connections

Caused By

Glaciation, Processes

Wikidata P31 formation-type mapped to formative process Glaciation via reviewed judgment map (earth atlas); source citation is this entity's own cited Wikidata item.

Source Wikidata: Harvard Glacier

In Discipline

Wikidata P31 formation-type mapped to discipline Glaciology via reviewed judgment map (earth atlas); source citation is this entity's own cited Wikidata item.

Source Wikidata: Harvard Glacier
In the Other Atlases

Found In

Also in Geography Atlas: where this subject is found.

Source Wikidata: Harvard Glacier
Sources
1. UNEP-WCMC and IUCN: Protected areas at the coordinates of Harvard Glacier, World Database on Protected Areas
UNEP-WCMC and IUCNname_eng and desig_eng
Quote, name_eng and desig_eng
"name_eng": "Nellie Juan-College Fiord", "desig_eng": "Wilderness Study Area"
View the Source
Harvard Glacier (Wikipedia)
  • Lead section
    The Harvard Glacier is a large tidewater glacier in the Alaska's Prince William Sound.
  • Lead sentence
    It is 300 ft thick and covers 120,000 acres of Chugach National Forest.
View the Source
Wikidata: Harvard Glacier
Wikidata Q5676407, class allow-list match (w-wdresolver-0926)View the Source
Comments (0)
No comments yet. Be the first to share a thought.
Reader Challenges (0)
No disputes yet. Spotted an error or a better source? Open the first one.