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Snowslip Formation, numerous beds of dolomitic siltite, dolomite, and stromatolites and gray to greenish-gray, very fine grained quartzite beds. Much of the sedimentation probably occurred between about 1450 and 1400 Ma (million years) ago. [11] Sedimentary structures are well preserved in most of the Belt rocks despite their great age.
Fossilized stromatolites in the Hoyt Limestone exposed at Lester Park, near Saratoga Springs, New York Precambrian fossilized stromatolites in the Siyeh Formation, Glacier National Park Fossilized stromatolites (Pika Formation, middle Cambrian) near Helen Lake, Banff National Park, Canada. Stromatolites are a major constituent of the fossil ...
Place Names of Glacier National Park. Helena, Montana: Riverbend Publishing. ISBN 1-931832-68-4. Schutz, James Willard (1926). Signposts of Adventure: Glacier National Park as the Indians Know It. Boston, New York: Houghton Mifflin Company. OCLC 1544470. Trails Illustrated-North Fork, Glacier National Park, Montana (314) (Map) (Revised ed.). 1: ...
Glacier National Park is a national park of the United States located in northwestern Montana, on the Canada–United States border.The park encompasses more than 1 million acres (4,100 km 2) and includes parts of two mountain ranges (sub-ranges of the Rocky Mountains), more than 130 named lakes, more than 1,000 different species of plants, and hundreds of species of animals.
Glacier Park Boat Company offers tours of numerous lakes in Glacier National Park. The tour boat Little Chief has carried visitors since 1926 and now docks at St. Mary Lake.
Like other mountains in Glacier National Park, Reynolds Mountain is composed of sedimentary rock laid down during the Precambrian to Jurassic periods. Formed in shallow seas, this sedimentary rock was initially uplifted beginning 170 million years ago when the Lewis Overthrust fault pushed an enormous slab of precambrian rocks 3 mi (4.8 km) thick, 50 miles (80 km) wide and 160 miles (260 km ...
Ancient giant stromatolites used to be widespread in Earth’s Precambrian era, which encompasses the early time span of around 4.6 billion to 541 million years ago, but now they are sparsely ...
This sea was home to stromatolites and to bottom-dwelling marine life whose tracks on the benthic sediment would later fossilize. [2] Montanan life of the time included arthropods, blue-green algae, conularians, fungi, and worms. Their fossils were preserved in what are now known as Glacier National Park.
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