The Denver Formation is a geological formation that is present within the central part of the Denver Basin that underlies the Denver, Colorado, area. It ranges in age from latest Cretaceous (Maastrichtian) to early Paleocene (Danian), and includes sediments that were deposited before, during and after the Cretaceous-Paleogene boundary event.
The formation is known for its paleontological resources, including dinosaur remains that are found in the Late Cretaceous part of the formation, and it includes aquifers that are important sources of water for the area. Some of North America's most iconic end-Cretaceous dinosaurs, such as Triceratops and Tyrannosaurus, were first identified from the Denver Formation before being properly described from better-preserved remains in end-Cretaceous formations further north.' The formation also preserves one of the most world's most diverse earliest Paleocene mammalian faunas, providing an important record of the diversification of mammals in the immediate aftermath of the K-Pg extinction.
The Denver Formation rests on the Arapahoe Formation, and its base is marked by the first appearance of tuffaceous sediments. It is overlain by the Dawson Arkose.
In 2002 the Denver Formation was included as part of a larger unconformity-bounded unit named the D1 sequence, in order to facilitate basin-wide studies and avoid confusion arising from the lateral and vertical facies changes that occur within the Denver Basin. The base of the D1 is marked by the abrupt facies change at the top of the Laramie Formation, and its top is placed at the base of a regional paleosol series. The Arapahoe Formation and the Dawson Arkose are also included in the D1 Sequence.
The Denver Formation consists of alluvial fan, fluvial, and paludal deposits that accumulated at the foot of the growing Rocky Mountain Front Ranges. It ranges in thickness from to in the central part of the Denver Basin. It is characterized by significant amounts of andesitic volcanic debris, and is composed of primarily of light-grey to brown, lenticular bedded, loosely cemented silty claystone, mudstone, siltstone, tuffaceous sandstone and, in some areas, andesitic conglomerate. Beds of low-rank coal and carbonaceous shale occur in the upper in some areas.
Several early Paleocene lava flows are present in the upper part of the Denver Formation at North and South Table Mountain near Golden, Colorado. The Ralston Dike, a body of intrusive monzonite located several miles to the northwest, probably represents the volcanic vent from which the flows erupted. Generally referred to as basaltic, they are classified either as monzonite (the lowest flow) and latite (the upper two flows), or as shoshonite. They contain the minerals augite, plagioclase, and olivine altered to serpentine, with accessory sanidine and/or orthoclase, apatite, magnetite, and biotite. One of the flows hosts a wide variety of zeolite minerals, including analcime, thomsonite, mesolite, chabazite, and others.
The Denver Formation spans the Cretaceous-Paleogene boundary. The lava flows in the upper part of the formation are about 62 to 64 million years old according to radiometric dating, which places them in the early Paleocene Epoch. The Cretaceous-Paleogene boundary occurs in the lower part of the formation, and an exposure of the boundary layer has been identified and documented on South Table Mountain near the city of Golden.
Plant fossils and remains of vertebrates, including turtles and mammals, are found throughout the Denver Formation. Dinosaur remains are restricted to the lower, Late Cretaceous, part.
Based on the Paleobiology Database except where noted:
The Denver Formation's dinosaur fauna appears to share close similarities with those of other Maastrichtian-aged formations in western North America. However, the dinosaur remains in the Denver Formation are significantly more disarticulated and fragmentary, suggesting that the formation's depositional environment was not conducive to the rapid burial that would have preserved articulated dinosaur skeletons.'
This formation represents the first known discoveries to science of Triceratops (a partial cranium with horns) and Tyrannosaurus (a tooth), as well as the type locality for another well-known dinosaur, Ornithomimus.'
Former "condylarths".