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Cuchara Formation
The Cuchara Formation is a geologic formation in Colorado. It preserves fossils dating back to the Ypresian stage of the Eocene period, or Wasatchian in the NALMA classification.Cuchara Formation
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Fossil content

The following fossils have been reported from the formation:


Mammals

;Ferae * '' Didymictis sp.''Robinson, 1963 ;Perissodactyla * '' Hyracotherium sp.< ...
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Colorado State Highway 12
State Highway 12 (SH 12), also known as the Highway of Legends National Scenic Byway, in the U.S. state of Colorado is a mountainous state highway through the Rocky Mountains in southern Colorado. The route travels from La Veta through the mountains to Trinidad. It is included in the Colorado Scenic and Historic Byways system and runs through the San Isabel National Forest. In 2021, the highway was designated a National Scenic Byway. Route description SH 12 begins at the junction with U.S. Route 160 (US 160) north of La Veta. It heads southward through that town before entering the San Isabel National Forest and passing through Cuchara, near the Spanish Peaks Wilderness. It then crosses Cucharas Pass into Las Animas County. SH 12 heads through Monument Park and turns eastward near Stonewall Gap. It then passes eastward along the Purgatoire River through Weston, Segundo, Valdez, Cokedale, and Jansen. It then ends in Trinidad at an intersection with Interstate 25, US& ...
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DeBeque Formation
The DeBeque Formation is a geologic formation in Colorado's Piceance Basin,Bown & Kihm, 1981 preserving fossils which date back to the Late Paleocene to Early Eocene period ( Clarkforkian to Wasatchian in the NALMA classification.DeBeque Formation
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Hirsch et al., 1997 Examples of these fossils are held in the .


Wasatchian correlations

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Hatchetigbee Bluff Formation
The Hatchetigbee Bluff Formation is a geologic formation in Alabama, Georgia, Louisiana and Mississippi. The youngest unit of the Wilcox Group preserves fossils dating back to the Ypresian stage of the Eocene period, or Wasatchian in the NALMA classification.Hatchetigbee Bluff Formation
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The formation is named for Hatchetigbee Bluff on the Tombigbee River, Washington Coun ...
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Nanjemoy Formation
The Nanjemoy Formation is a geologic formation pertaining to both the Wilcox Group and the Pamunkey Group of the eastern United States, stretching across the states of Virginia, Maryland, and District of Columbia. The formation crops out east of the Appalachians and dates back to the Paleogene period. Specifically to the Ypresian stage of the Eocene epoch, about 55 to 50 Ma or Wasatchian in the NALMA classification, defined by the contemporaneous Wasatch Formation of the Pacific US coast. The about thin formation crops out in a narrow irregular band and only in certain of the many creeks of the Maryland peninsula and on the southern side of the Potomac River in Virginia. The two members the formation was divided into by Clark and Martin in 1901; Potapaco and Woodstock, represent different phases in the basin history. The lower Potapaco Member is much more clayey, described as marl, than the upper Woodstock Member, probably characteristic of less storm influences in the shal ...
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Margaret Formation
The Margaret Formation is a geologic formation of the Eureka Sound Group in the Sverdrup Basin in Northwest Territories and Nunavut, Canada. The unit belonging to the Eureka Sound Group which crops out at Ellesmere Island preserves fossils dating back to the Early Eocene period, or Wasatchian in the NALMA classification.Margaret Formation
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The Margaret Formation comprises s, sandy

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Kamloops Group
Kamloops ( ) is a city in south-central British Columbia, Canada, at the confluence of the South flowing North Thompson River and the West flowing Thompson River, east of Kamloops Lake. It is located in the Thompson-Nicola Regional District, whose district offices are based here. The surrounding region is sometimes referred to as the Thompson Country. The city was incorporated in 1893 with about 500 residents. The Canadian Pacific Railroad was completed through downtown in 1886, and the Canadian National arrived in 1912, making Kamloops an important transportation hub. With a 2021 population of 97,902, it is the twelfth largest municipality in the province. The Kamloops census agglomeration is ranked 36th among census metropolitan areas and agglomerations in Canada with a 2021 population of 114,142. Kamloops is promoted as the ''Tournament Capital of Canada''. It hosts more than 100 sporting tournaments each year (hockey, baseball, curling, etc) at world-class sports faci ...
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Allenby Formation
The Allenby formation is a sedimentary rock formation in British Columbia which was deposited during the Ypresian stage of the Early Eocene. It consists of conglomerates, sandstones with interbedded shales and coal. The shales contain an abundance of insect, fish and plant fossils known from 1877 and onward, while the Princeton Chert was first indented in the 1950's and is known from anatomically preserved plants. There are several notable fossil producing localities in the Princeton & Tulameen basins. Historical collection sites included Nine Mile Creek, Vermilian Bluffs, and Whipsaw Creek, while modern sites include One Mile Creek, Pleasant Valley, Thomas Ranch, and the Princeton Chert. Extent and correlation The Allenby is estimated to have an overall extent of approximately , though actual outcroppings of the formation make up less than 1% of the formation, while other exploratory contact is via boreholes and mines. The half-graben which contains the formation is separ ...
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Coldwater Beds
The Coldwater Beds are a geologic formation of the Okanagan Highlands in British Columbia, Canada. They preserve fossils dating back to the Ypresian stage of the Eocene period, or Wasatchian in the NALMA classification.Coldwater Beds
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The formation comprises mudstones, s and s deposited in a

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Golden Valley Formation
The Golden Valley Formation is a stratigraphic unit of Late Paleocene to Early Eocene age in the Williston Basin of North Dakota.Hickey, 1977 It is present in western North Dakota and was named for the city of Golden Valley by W.E. Benson and W.M. Laird in 1947.Benson, W.E. and Liard, W.M. 1947. Eocene of North Dakota. Geological Society of America Bulletin, vol. 60, pp. 1166–1167. It preserves significant assemblages of fossil plants and vertebrates,Jepsen, G.L. 1963. Eocene vertebrates, coprolites, and plants in the Golden Valley Formation of western North Dakota. Geological Society of America Bulletin, vol. 74, pp. 673–684. as well as mollusk and insect fossils. Stratigraphy The Golden Valley Formation is present as a series of outliers in western North Dakota. It is underlain by the Sentinel Butte Formation and unconformably overlain by the White River Group. It reaches thicknesses of up to and is subdivided into two members: the ''Bear Den Member'' (lower) and the ''Cam ...
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Willwood Formation
The Willwood Formation is a sedimentary sequence deposited during the late Paleocene to early Eocene, or Clarkforkian, Wasatchian and Bridgerian in the NALMA classification.Willwood Formation
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Neasham & Vondra, 1972


Description

It consists of fine grained clastic rocks ( and ) interbedded with medium grained clastic rocks (

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Tatman Formation
The Tatman Formation is a Wasatchian geologic formation in Wyoming. It preserves fossils dating back to the Ypresian stage of the Eocene period.Tatman Formation
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Fossil content

The following fossils have been recovered from the formation:Wing et al., 1995


Flora

* '' Allantoidiopsis erosa'' * '' Cercidiphyllum genetrix'' * ''
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