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Steven C. Minkin Paleozoic Footprint Site, formerly the Union Chapel Mine, is a former coal mine that became an important fossil site in Alabama after an Oneonta High School science teacher discovered tracks in the rocks at the site while preparing for a school field trip. The mine belonged to a family member of one of the children in his class.
The black limestone of Isle La Motte takes a polish, revealing the white "bird's-eye" [4] markings of embedded fossil shells, notably the spirals formed by sliced gastropod shells. Rock of the Chazy Formation was quarried from the nineteenth century at the Fisk Quarry, Isle La Motte, the oldest quarry in Vermont . [ 5 ]
This list of fossil sites is a worldwide list of localities known well for the presence of fossils. Some entries in this list are notable for a single, unique find, while others are notable for the large number of fossils found there.
The Geiseltal fossil deposit is located in the former lignite district of the Geiseltal south of the city of Halle in Saxony-Anhalt, Germany. It is an important site of now extinct plants and animals from the Middle Eocene period 48 to 41 million years ago. There is evidence that coal was first mined in the Geiseltal in 1698, but the first ...
Fossil mollusca are abundant, and fossil fish are to be found, as well as Palaeophis, a sea-snake, and Puppigerus, a sea turtle. Nummulites and other foraminifera also occur. The Bracklesham Group lies between the Barton Clay above and the Bournemouth Beds, [citation needed] Lower Bagshot, below. In the London Basin, these beds are represented ...
The Stonerose Interpretive center & Eocene Fossil Site is a 501c(3) non-profit public museum and fossil dig located in Republic, Washington. The center was established in 1989 and houses fossils that have been featured in National Geographic Magazine , Sunset magazine , and numerous scientific works.
The geology of the Isle of Mull in Scotland is dominated by the development during the early Palaeogene period of a ‘volcanic central complex’ associated with the opening of the Atlantic Ocean. The bedrock of the larger part of the island is formed by basalt lava flows ascribed to the Mull Lava Group erupted onto a succession of Mesozoic ...
A suite of dykes of Ordovician to Silurian age have been intruded into the rocks of the Manx and Dalby groups. Other than some exposed hillsides and stream sections they are not readily encountered inland but are well exposed along the rocky shores of the island south of Ramsey in the east and Kirk Michael in the west.