Hornerstown Formation (original) (raw)

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The Hornerstown Formation is a Paleogene or latest Mesozoic geologic formation in New Jersey. The age of these deposits have been controversial. While most fossils are of animals types known from the earliest Cenozoic era, several fossils of otherwise exclusively Cretaceous age have been found. These include remains of the shark Squalicorax, the teleost fish Enchodus, several species of ammonite, and marine lizards referred to the genus Mosasaurus. Some of these remains show signs of severe abrasion and erosion, however, implying that they are probably re-worked from older deposits. Most of these fossils are restricted to the lowest point in the formation, one rich in fossils and known as the Main Fossiliferous Layer, or MFL. Other explanations for the out-of-place fossils in the MFL is th

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dbo:abstract The Hornerstown Formation is a Paleogene or latest Mesozoic geologic formation in New Jersey. The age of these deposits have been controversial. While most fossils are of animals types known from the earliest Cenozoic era, several fossils of otherwise exclusively Cretaceous age have been found. These include remains of the shark Squalicorax, the teleost fish Enchodus, several species of ammonite, and marine lizards referred to the genus Mosasaurus. Some of these remains show signs of severe abrasion and erosion, however, implying that they are probably re-worked from older deposits. Most of these fossils are restricted to the lowest point in the formation, one rich in fossils and known as the Main Fossiliferous Layer, or MFL. Other explanations for the out-of-place fossils in the MFL is that they represent a time-averaged assemblage that built up and remained unburied during a time of low sediment deposition, or that they were stirred up from deeper in the sediment and deposited together during a tsunami. (en)
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dbo:wikiPageWikiLink dbr:Ammonite dbr:Bird dbr:Bottosaurus dbc:Paleogene_geology_of_New_Jersey dbr:Hyposaurus dbr:Vincentown_Formation dbr:Telmatornis dbr:Cretaceous dbr:Geological_formation dbr:Enchodus dbr:Graculavus dbr:Mosasaurus dbr:Cenozoic dbr:Tinton_Formation dbr:Tsunami dbr:Tytthostonyx dbr:Anatalavis dbr:Danian dbr:Palaeotringa dbr:Paleogene dbr:Formation_(geology) dbr:Laornis dbc:Danian_Stage dbr:Squalicorax dbr:Mesozoic dbr:New_Egypt_Formation dbr:New_Jersey dbr:List_of_dinosaur-bearing_rock_formations dbr:Crocodylomorph
dbp:age dbr:Danian ~ (en)
dbp:name Hornerstown Formation (en)
dbp:overlies New Egypt Formation and Tinton Formation (en)
dbp:period Danian (en)
dbp:region dbr:New_Jersey
dbp:type dbr:Geological_formation
dbp:underlies dbr:Vincentown_Formation
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dcterms:subject dbc:Paleogene_geology_of_New_Jersey dbc:Danian_Stage
gold:hypernym dbr:Paleogene
rdf:type yago:WikicatMesozoicGeologicFormations yago:Abstraction100002137 yago:Arrangement107938773 yago:Formation108426461 yago:Group100031264
rdfs:comment The Hornerstown Formation is a Paleogene or latest Mesozoic geologic formation in New Jersey. The age of these deposits have been controversial. While most fossils are of animals types known from the earliest Cenozoic era, several fossils of otherwise exclusively Cretaceous age have been found. These include remains of the shark Squalicorax, the teleost fish Enchodus, several species of ammonite, and marine lizards referred to the genus Mosasaurus. Some of these remains show signs of severe abrasion and erosion, however, implying that they are probably re-worked from older deposits. Most of these fossils are restricted to the lowest point in the formation, one rich in fossils and known as the Main Fossiliferous Layer, or MFL. Other explanations for the out-of-place fossils in the MFL is th (en)
rdfs:label Hornerstown Formation (en)
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is dbp:underlies of dbr:Tinton_Formation
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