Glacier National Park (U.S.)
Dublin Core
Title
Glacier National Park (U.S.)
Subject
Tourism
Description
Located on the US-Canada border in northwest Montana, the park covers over 4,000 square kilometres, includes parts of two Rocky Mountain subranges and has over 130 named lakes, and is home to over a thousand species of plants and hundreds of animals.
The mountains of Glacier National Park began forming 170 million years ago when ancient rocks were forced eastwards and overlain by younger rock formations. These sedimentary rocks, known as Lewisian retrogradational rocks, are considered to be the finest fossils of early life on Earth.
Maps and photographs from the mid-20th century show that the 150 glaciers that existed in the park 100 years ago have in many cases retreated significantly, if not disappeared altogether. Based on warming trends in the early 21st century, scientists had estimated that the park's remaining glaciers would melt by 2020. However, a later estimate suggested that the glaciers could disappear by 2030.
Source
is51102023
Contributor
yx63@st-andrews.ac.uk
Language
English
Type
Site
Identifier
656
Date Submitted
27/04/2023
References
https://en.wikipedia.org/wiki/Glacier_National_Park_(U.S.)
Extent
cm x cm x cm
Spatial Coverage
current,48.61475368407372,-113.74420166015626;
Provenance
US National Park Service(NPS)
Europeana
Europeana Data Provider
Glacier National Park (U.S.)
Object
https://www.nps.gov/glac/index.htm
Europeana Type
TEXT
Site Item Type Metadata
Institutional nature
Place Name
Place
Glacier National Park Headquarters West Glacier, MT 59936
Prim Media
1269
Status
public
Condition
1
Contact
yx63@st-andrews.ac.uk
Citation
“Glacier National Park (U.S.),” STAGE, accessed December 13, 2025, https://stage.openvirtualworlds.org/omeka/items/show/1276.
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