Depositional Surfaces in the Eagle Sandstone at Billings, Montana
No route; this field guide describes two stops in Billings, MT. One of the two stops provides a panoramic view of the sandstone units; the other stop provides an opportunity to study the outcrop.
Roads (and Trails)
Various roads in Billings, Black Otter Trail at Swords Park
Marine shelf sandstones and barrier bars are commonly formed by lateral accretion of sand bodies with time lines inclined to the formation boundaries. Shelton (1965) described low-angle inclined bedding in the lowermost sandstone unit of the Eagle Sandstone at Billings, Montana. He recognized these beds as shoreface accretion surfaces of a barrier bar and likened them to those found on present-day Galveston Island, Texas. The Billings location provides an excellent opportunity to examine an important hydrocarbon reservoir rock of the Northern Rocky Mountain region.
Key Lithologic Features
- Lower and middle members of the Eagle Sandstone
- sedimentary structures and burrows
- sandstone cliffs (rimrocks)
- observation of an important hydrocarbon reservoir
Hansen, W.B., and Kendrick, K.R., 1987, Depositional surfaces in the Eagle Sandstone at Billings, Montana, in
Beus, S.S., ed., Centennial Field Guide Volume 2: Rocky Mountain Section of the Geological Society of America
, p. 79-82.
Out of print. Check Amazon.com
. Digital access to this publication is available via the links in the references section above.