It is characterized by alternating beds of arkosic sandstone and mudstone.
[1][3] The Dawson Arkose contains plant remains[4] and other nonmarine fossils, and hosts aquifers that are important sources of water for the area.
[5] The Dawson Arkose consists of alluvial fan and fluvial deposits that accumulated at the foot of the growing Rocky Mountain Front ranges.
It overlies and interfingers with the Denver Formation which spans the Cretaceous-Paleogene boundary, and is of early Paleocene (Puercan) age.
[6] In 2002 the Dawson Arkose 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.