Fossiliferous flint (Upper Mercer Flint, Middle Pennsylvanian; Tunnel Hill North Portal Outcrop, Coshocton County, Ohio, USA) 4 : 無料・フリー素材/写真
Fossiliferous flint (Upper Mercer Flint, Middle Pennsylvanian; Tunnel Hill North Portal Outcrop, Coshocton County, Ohio, USA) 4 / James St. John
| ライセンス | クリエイティブ・コモンズ 表示 2.1 |
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| 説明 | Fossiliferous flint from the Pennsylvanian of Ohio, USA. (~7.9 cm across at its widest)This rock sample is from the Pottsville Group of eastern Ohio. The Pottsville Group is a Pennsylvanian-aged cyclothemic succession containing nonmarine shales, marine shales, siltstones, sandstones, coals, marine limestones, and chert ("flint"). The lower Pottsville dates to the late Early Pennsylvanian. The upper part dates to the early Middle Pennsylvanian. The Lower-Middle Pennsylvanian boundary is apparently somewhere near the Boggs Member (?).The Upper Mercer Flint is a moderately laterally persistent chert horizon in the Pottsville Group. It is often black-colored but can be dark bluish to bluish-black colored as well (the latter colors are referred to as "Nellie Blue Flint"). Upper Mercer Flint has whitish-colored fossils and fossil fragments that include fusulinid foraminifera, crinoid ossicles, and other Late Paleozoic normal marine fossils. Apparent phylloidal algae can also be present as squiggly lines.This chert horizon is actually a chertified fossiliferous limestone. Non-chertified limestone is frequently present, although minor in volume. Limestone usually occurs along the outside portions of chert masses, but also in relatively small patches within the chert.In places, the Upper Mercer Flint/Limestone horizon is missing, usually removed by paleoerosion.American Indians sometimes used Upper Mercer Flint to make arrowheads and spear points and knife blades. "Flint Ridge Flint" (= Vanport Flint) was the most desirable source rock for these objects, but other chert horizons also attracted attention.In this sample, the dark-colored material is the flint. The light-colored specks in the flint are fossils and fossil fragments. The brownish-colored material is a thin rind of non-chertified limestone.Stratigraphy: Upper Mercer Flint (= chertified Upper Mercer Limestone), upper Pottsville Group, Atokan Stage, lower Middle PennsylvanianLocality: Tunnel Hill North Portal Outcrop (= Noland Tunnel's northern portal), ~1.75 air miles north-northeast of the town of Tunnel Hill, western Coshocton County, eastern Ohio, USA (~40° 16’ 33.27” North latitude, ~82° 01’ 53.04” West longitude) |
| 撮影日 | 2016-11-06 23:22:59 |
| 撮影者 | James St. John |
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