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Geodiversity refers to the full variety of natural geologic (rocks, minerals, sediments, fossils, landforms, and physical processes) and soil resources and processes that occur in the park. A product of the Geologic Resources Inventory, the NPS Geodiversity Atlas delivers information in support of education, Geoconservation, and integrated management of living (biotic) and non-living (abiotic) components of the ecosystem.

In-depth geologic information is contained in the baseline inventory products of the Geologic Resources Inventory, see table below.
Geologic Features and Processes
The Lewis Overthrust
This surface, best seen exposed north of Marias Pass, represents older (950 million years old) limestones, shales, and sandstones thrusted eastward for over 60 kilometers on top of younger (90 million year old) shales. Within the geologic science community, it is considered one of the finest examples of such an overthrust in the world. The relatively hard rocks in the overlying sheet provided the resistance to the alpine glaciers of the last ice age that created the sculpted landforms we see today. Without this hard carapace, the ice would likely have left little relief beneath it, similar to what we see on the Blackfoot Reservation today.
Chief Mountain
Standing alone in front of the ranges to its west, Chief Mountain is a klippe, a geologic term for the erosional remnant of older rocks in a thrust sheet completely detached from comparably aged rocks trailing behind. Like the Lewis Overthrust itself, Chief Mountain is considered one of the world’s outstanding examples of a klippe; its images grace the pages of many geologic textbooks.
Sedimentary Rock Structures
While well known among geologists, the general public is largely unaware of the significance of these small features which are remarkably well preserved and represent conditions that the rocks were deposited under. Notable are mud cracks, raindrop impressions, and ripple marks.
Purcell Lava Flow and Associated Features
This igneous dike, whose mineralogy gives it a dark gray to black appearance, was intruded as a molten fluid into the surrounding carbonate rocks. The high temperature of the fluid essentially baked the light gray carbonates into a white chill zone, providing the distinctive white-gray-white striping seen wherever the flow is exposed.
Glacial Landforms
Almost too many to mention, but notable are bergschrunds, crevasses, cirques, horns, arêtes, hanging valleys, glacial stairways, paternoster lakes, waterfalls, moraines, moraine lakes, and glacial deposits.
Stromatolites
Described in the paleontology section.
Pillow Basalts
Lava extruded onto a lake or ocean floor will solidify in pillow shaped blocks. The inaccurately named Granite Park (actually a basalt), is an excellent location to see these.
Goat Lick
The rocks at this location are rich in sodium, something lacking elsewhere in local mountain goats’ diet. This exposure is a significant attraction to goats determined to make up this deficiency.
More information on these features can be found in the Geologic Resources Inventory Report.
Paleontological Resources
The rocks of Glacier record the ancient beginnings of life on earth. The Precambrian Belt Supergroup strata range in age from about 1,325 million years ago (m.y.) to about 900 m.y. The Belt Supergroup was thrust over Cretaceous age shales in the Glacier Park area. Fossils at the park record the first forms of life and include several types of Precambrian age algae (stromatolites) and later Cretaceous oysters, brachiopods and dinosaurs.
All NPS fossil resources are protected under the Paleontological Resources Preservation Act of 2009 (Public Law 111-11, Title VI, Subtitle D; 16 U.S.C. §§ 470aaa - 470aaa-11).
Cave and Karst
There are at least 16 known caves in Glacier National Park with the longest being slightly over 1 mile in length and the deepest being 365 feet deep. The Helena Formation, part of the older Mesoproterozoic units consists of thick beds of dolomite and limestone and contains caves. Eighteen percent of the park is considered to be karst.
All NPS cave resources are protected under the the Federal Cave Resources Protection Act of 1988 (FCRPA)(16 U.S.C. § 4301 et seq.).
Abandoned Mineral Lands
There was considerable mineral exploration activity that predated the establishment of the park in 1910. This includes copper mining and oil and gas exploratory wells. Approximately 28 AML sites having 48 distinct features have been identified in the park.
NPS AML sites can be important cultural resources and habitat, but many pose risks to park visitors and wildlife, and degrade water quality, park landscapes, and physical and biological resources. Be safe near AML sites—Stay Out and Stay Alive!
Regional Geology
Glacier National Park is a part of the Northern Rocky Mountains Province and shares its geologic history and some characteristic geologic formations with a region that extends well beyond park boundaries.
Maps and Reports

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Geologic Resources Inventory
The Geologic Resources Inventory produces digital geologic maps and reports for more than 270 natural resource parks. The products listed below are currently available for this park, check back often for updates as many maps, reports, and posters are still in progress.
Scoping summaries are records of scoping meetings where NPS staff and local geologists determined the park’s geologic mapping plan and what content should be included in the report.
- Digital geologic maps include files for viewing in GIS software, a guide to using the data, and a document with ancillary map information. Newer products also include data viewable in Google Earth and online map services.
- Reports use the maps to discuss the park’s setting and significance, notable geologic features and processes, geologic resource management issues, and geologic history.
- Posters are a static view of the GIS data in PDF format. Newer posters include aerial imagery or shaded relief and other park information. They are also included with the reports.
- Projects list basic information about the program and all products available for a park.
Source: NPS DataStore Saved Search 2879
. To search for additional information, visit the
NPS DataStore.
Soil Resources inventory
A NPS Soil Resources Inventory project has been completed for Glacier National Park and can be found on the NPS Data Store.
Source: NPS DataStore Saved Search 2950
. To search for additional information, visit the
NPS DataStore.

Red Eagle Mountain.
Related Links
- Glacier NP—Glaciers / Glacial Features
- Glacier NP—Mountains
- Glacier NP—Fossils
- Glacier NP—Soils
- Glacier NP—Geologic Activity
- Glacier NP—Hydrologic Activity
- NPS—Glaciers and Glacial Landforms
- NPS—Fossils and Paleontology
- NPS—Geologic Time
- NPS—Explore Regional Geology
- NPS—Geology
Montana Bureau of Mines & Geology
Related Articles
Glacier National Park
- Glacier's bat inventory and monitoring program: Using partners, collaborators, and volunteers to make it a success — Park biologists race the clock to learn as much as they can about bats before risks from white-nose syndrome and wind energy development alter bat populations and movements in and around Glacier National Park.
- Climate Change & Geologic History at Glacier National Park — Geologic history can help shape our understanding of the climate crisis of today. As you will see, the climate of today is the result of changes, choices, and climates of the past.
- Series: Park Paleontology News - Vol. 16, No. 2, Fall 2024 — All across the park system, scientists, rangers, and interpreters are engaged in the important work of studying, protecting, and sharing our rich fossil heritage. Park Paleontology news provides a close up look at the important work of caring for these irreplaceable resources. Contribute to Park Paleontology News by contacting the newsletter editorLearn more about Fossils & Paleontology Celebrate National Fossil Day with events across the nation
- New Mammal Fossils from Glacier National Park Shed Light on the Rocky Mountains 28 Million Years Ago — Glacier National Park in northwest Montana is known for its rich fossil record of plants, insects, mollusks, and fish, but also mammals from the Eocene. In a recent publication, a team of scientists describes the first Oligocene-aged fossil mammals, the youngest fossil mammals ever discovered in the park.
- Making an Impact: Long-Term Monitoring of Natural Resources at Intermountain Region National Parks, 2021 — Across the Intermountain Region, Inventory & Monitoring Division ecologists are helping to track the effects of climate change, provide baseline information for resource management, evaluate new technologies, and inspire the next generation of park stewards. This article highlights accomplishments achieved during fiscal year 2021.
- The Stromatolites of Glacier National Park — The rugged high peaks of Glacier National Park are a beautiful sight to behold, with people traveling from all around the globe to experience this iconic place. The rocks that compose those amazing peaks and valley walls hold the secrets to a time when this land was once covered by a vast shallow sea, a billion and a half years ago.
- Studying the Past and Predicting the Future Using Rat Nests — In the western United States, packrat middens are one of the best tools for reconstructing recent environments and climates. These accumulations of plant fragments, small vertebrate remains, rodent droppings, and other fossils can be preserved for more than 50,000 years. Packrat middens have been found in at least 41 National Park Service units.
- Series: Park Paleontology News - Vol. 14, No. 2, Fall 2022 — All across the park system, scientists, rangers, and interpreters are engaged in the important work of studying, protecting, and sharing our rich fossil heritage. Park Paleontology news provides a close up look at the important work of caring for these irreplaceable resources. Contribute to Park Paleontology News by contacting the newsletter editorLearn more about Fossils & Paleontology Celebrate National Fossil Day with events across the nation
- Series: Geologic Time—Major Divisions and NPS Fossils — The National Park System contains a magnificent record of geologic time because rocks from each period of the geologic time scale are preserved in park landscapes. The geologic time scale is divided into four large periods of time—the Cenozoic Era, Mesozoic Era, Paleozoic Era, and The Precambrian.
- The Precambrian — The Precambrian was the "Age of Early Life." During the Precambrian, continents formed and our modern atmosphere developed, while early life evolved and flourished. Soft-bodied creatures like worms and jellyfish lived in the world's oceans, but the land remained barren. Common Precambrian fossils include stromatolites and similar structures, which are traces of mats of algae-like microorganisms, and microfossils of other microorganisms.
National Park Service Geodiversity Atlas
The servicewide Geodiversity Atlas provides information on geoheritage and geodiversity resources and values within the National Park System. This information supports science-based geoconservation and interpretation in the NPS, as well as STEM education in schools, museums, and field camps. The NPS Geologic Resources Division and many parks work with National and International geoconservation communities to ensure that NPS abiotic resources are managed using the highest standards and best practices available.
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