EPOD - a service of USRA
The Earth Science Picture of the Day (EPOD) highlights the diverse processes and phenomena which shape our planet and our lives. EPOD will collect and archive photos, imagery, graphics, and artwork with short explanatory
captions and links exemplifying features within the Earth system. The
community is invited to contribute digital imagery, short captions and
relevant links.
Bearpaw Formation in Montana
January 14, 2022
EPODbearpawash
Photographer: Rod Benson
Summary Author: Rod Benson
This photo was taken along an intermittent tributary of the
Missouri River in the Missouri Breaks region of central
Montana. The sediments exposed in the cut bank are part of the
Bearpaw formation (aka Bearpaw shale). The silts and clays were
deposited in the Western Interior Seaway, an inland sea that
extended from the Arctic to the Gulf of Mexico during the mid to late
Cretaceous period. The part of the sea that covered this part of
Montana is sometimes called the Bearpaw Sea, named for the Bears Paw
Mountains located 60 miles (100 km) northwest of here.
Over millions of years the sea advanced and retreated across the
region, changing the location of the shoreline and the depth of the
water. In the meantime, occasional volcanic eruptions to the west
spewed ash that winds carried over the sea. The thicker
light-colored layer in the photo is ash from one of those eruptions. A
few thinner deposits of ash are also exposed in the cut bank. Volcanic
ash deposited in seawater changes over time; weathering converts it
into a clay material called bentonite. Although it looks like ash
from a distance, it feels like a sticky clay that has little
resemblance to the ancient ash that settled here.
In addition to bentonite (altered ash) the Bearpaw formation contains a
variety of marine fossils and some dinosaurs. Geologists estimate
that sediments of the Bearpaw formation were deposited between 75 and
72 million years ago. In places the formation is 1150 feet (350 meters)
thick. Outcrops can be found in Montana as well as the Canadian
provinces of Alberta and Saskatchewan. As the Western Interior
Seaway retreated to the southwest, the Bearpaw shales were covered by
deltaic and coastal plains sediments.
Related EPODs
Bearpaw Formation in Montana Archive - Armorican Quartzite
Calcite Crystals and Earth’s Microbial History Gingham Skirt
Butte Art Imitates Nature The Cataclysmic Birth of Montana’s
Earthquake Lake
More...
Geology Links
* Earthquakes
* Geologic Time
* Geomagnetism
* General Dictionary of Geology
* Mineral and Locality Database
* Mohs Scale of Mineral Hardness
* This Dynamic Earth
* USGS
* MyShake - University of California, Berkeley
* USGS Ask a Geologist
* USGS/NPS Geologic Glossary
* USGS Volcano Hazards Program
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