Midland

Description

Source: Wikipédia

The Midland Formation is a Mesozoic (latest Triassic to earliest Jurassic) geological formation in the Culpeper Basin of Virginia. It is a sedimentary unit which formed in a short period of time between the first two basalt flows in the basin: the Hickory Grove and Mount Zion Church basalts. The most common rocks in the formation are dark reddish interbedded sandstones and siltstones, representative of fluvial (stream) environments. Rare but fossiliferous calcareous shale and limestone also occurs, representing recurring lacustrine (lake) conditions. The Midland Formation is considered equivalent to the Shuttle Meadow Formation of the Hartford Basin, the Feltville Formation of the Newark Basin, and the Bendersville Formation of the Gettysburg Basin. Some sources prefer to classify the Midland Formation as part of the Shuttle Meadow Formation.
Based on conchostracan biostratigraphy, the Midland Formation is believed to contain the Triassic-Jurassic boundary near its base. A prominent shale layer containing Hettangian-age fossilized fish, the Midland fish bed, is present about 10 meters above the base of the formation. Though now flooded by a manmade lake, it was formerly well-exposed along Licking Run, just north of Midland, Virginia. Plant spores, coprolites, and dinosaur footprints have also been recorded at nearby outcrops.

Découvertes

Source: The Paleobiology Database

Site(s) correspondant(s) à cette formation: 1

• Oak Hill tracksite : Virginia - Loudoun ^{12444 23520 50062 54204 55917 77283 85047}
near Aldie, on the former estate of James Monroe, later the F. C. Littleton farm. Original discovery was from flagstones used to renovate the home of President James Monroe. These came from a quarry on the N side of the Little River, 1.6 mi. N of the mansion.
• Theropoda