2014 GSA Annual Meeting in Vancouver, British Columbia (19–22 October 2014)

Paper No. 320-5
Presentation Time: 10:00 AM

SAND INJECTITE COMPLEX WITHIN THE UPPER CASSELMAN FORMATION AT MT. NEBO POINTE, PITTSBURGH, PA


ANDERSON, Calvin J., WHITMORE, John H. and AUSTIN, Steven A., Department of Science and Mathematics, Cedarville University, 251 N. Main St, Cedarville, OH 45314, calvinanderson1@cedarville.edu

A new and exceptional sand injectite complex has been identified within the Casselman Formation (Upper Pennsylvanian) near Pittsburgh, Pennsylvania. The injectites are displayed prominently on the northern highwall of the parking lot for Mt. Nebo Pointe Shopping Center, near the Camp Horne Road interchange on I-279. This previously undocumented locality is extremely well-exposed, easily accessible and contains dozens of meters-scale injectites.

The wall is 320 m long and up to 20 m high. Exposure includes flat-lying strata of Casselman Formation (Conemaugh Group). We studied the undisrupted stratigraphic interval of sandstone, siltstone, claystone and coal at a nearby roadcut on I-279. We then applied our expectation of the stratigraphic interval to the Mt. Nebo Pointe highwall. At the base of the wall is the uppermost Birmingham Sandstone overlain by laterally displaced and sheared Wellersburg Coal and claystone.

Sand dikes ranging from a few cm to 1.0 m wide intrude these lower strata. Smaller dikes tend to cut horizontally while the largest dikes intrude vertically. About 20 clear vertical dikes can be identified, with approximately 80% being concentrated in the western half of the wall. Dikes are strongly bedded parallel to orientation, melding into bedding of cross-cutting dikes at intersections. Dike shapes resemble pillars rather than V’s. Clasts are common and oriented either concurrent with the host rock or parallel to injectite direction and displaced upwards. These indicate vertical sediment flow coupled with rapid brecciation.

The upper highwall is typical Morgantown Sandstone (cross-bedded, feldspathic and comparatively well-sorted) interstratified with slurry-flow sandstone (massive, lithic and poorly sorted). This slurried lithic sand was intruded upward from the Birmingham Sandstone interval beneath the parking lot level. The overall depth of the injectites is unknown, however, a Birmingham source would imply a minimum of 6 m.

This exposure presents a unique opportunity to study sand injectites directly. It is our hope that this exceptional injectite complex will provide valuable insights into injectite formation and associated processes.

Handouts
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