About: Caimito Formation

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The Caimito Formation (Tcm) is a geologic formation in Panama. The marls, sandstones and conglomerates preserve bivalve and gastropod fossils dating back to the Late Oligocene to Early Miocene period. The name Caimito was proposed by MacDonald in 1913, named after the Caimito junction in the Panama Railroad during the construction of the Panama Canal.

Property	Value
dbo:abstract	The Caimito Formation (Tcm) is a geologic formation in Panama. The marls, sandstones and conglomerates preserve bivalve and gastropod fossils dating back to the Late Oligocene to Early Miocene period. The name Caimito was proposed by MacDonald in 1913, named after the Caimito junction in the Panama Railroad during the construction of the Panama Canal. (en)
dbo:wikiPageExternalLink	https://pubs.usgs.gov/pp/0306a/report.pdf https://pubs.usgs.gov/pp/0306f/plate-1.pdf
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dbo:wikiPageWikiLink	dbr:Caraba_Formation dbr:List_of_fossiliferous_stratigraphic_units_in_Panama dbr:Bohío_Formation dbr:United_States_Geological_Survey dbr:Early_Miocene dbr:Gatuncillo_Formation dbr:Gatún_Formation dbr:Bivalve dbr:Conglomerate_(geology) dbr:Gastropod dbr:Period_(geology) dbc:Conglomerate_formations dbc:Marl_formations dbr:Alajuela_Formation dbc:Geography_of_Panamá_Province dbc:Geologic_formations_of_Panama dbc:Neogene_Panama dbc:Panama_Canal_Zone dbr:Fossils dbr:Panama dbr:Panama_Canal dbr:Panamá_Province dbr:Formation_(geology) dbr:Siltstone dbc:Sandstone_formations dbc:Shallow_marine_deposits dbc:Siltstone_formations dbr:Late_Oligocene dbr:Marl dbr:Sandstone dbr:Formation_(stratigraphy) dbr:Panama_Basin dbr:Panama_Railroad
dbp:age	dbr:Early_Miocene dbr:Late_Oligocene
dbp:extent	dbr:Panama_Basin
dbp:name	Caimito Formation (en)
dbp:namedby	MacDonald (en)
dbp:namedfor	Caimito Junction of Panama Railroad (en)
dbp:otherlithology	dbr:Conglomerate_(geology) dbr:Siltstone dbr:Sandstone
dbp:overlies	Bohío, Caraba & Gatuncillo Formations, Cretaceous basement (en)
dbp:period	Aquitanian (en)
dbp:prilithology	dbr:Marl
dbp:region	dbr:Panamá_Province
dbp:type	dbr:Formation_(stratigraphy)
dbp:underlies	Alajuela & Gatún Formations (en)
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dbp:yearTs	1913 (xsd:integer)
dcterms:subject	dbc:Conglomerate_formations dbc:Marl_formations dbc:Geography_of_Panamá_Province dbc:Geologic_formations_of_Panama dbc:Neogene_Panama dbc:Panama_Canal_Zone dbc:Sandstone_formations dbc:Shallow_marine_deposits dbc:Siltstone_formations
gold:hypernym	dbr:Formation
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rdfs:comment	The Caimito Formation (Tcm) is a geologic formation in Panama. The marls, sandstones and conglomerates preserve bivalve and gastropod fossils dating back to the Late Oligocene to Early Miocene period. The name Caimito was proposed by MacDonald in 1913, named after the Caimito junction in the Panama Railroad during the construction of the Panama Canal. (en)
rdfs:label	Caimito Formation (en)
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geo:lat	9.200000 (xsd:float)
geo:long	-79.800003 (xsd:float)
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is dbp:overlies of	dbr:Alajuela_Formation
is foaf:primaryTopic of	wikipedia-en:Caimito_Formation