About: Mitchell Plain     Goto   Sponge   NotDistinct   Permalink

An Entity of Type : geo:SpatialThing, within Data Space : dbpedia.demo.openlinksw.com associated with source document(s)
QRcode icon
http://dbpedia.demo.openlinksw.com/describe/?url=http%3A%2F%2Fdbpedia.org%2Fresource%2FMitchell_Plain&invfp=IFP_OFF&sas=SAME_AS_OFF

The Mitchell Plain is a karst area in Indiana of relatively low relief. The extensive underlying cave system developed in Mississippian age limestone bedrock. Surface drainage is rare due to most streams in the area disappearing into caves or joints within the rock. The limestone is a vestige of an early shallow cratonic sea that covered what would become Indiana, while the North-South linearity of the region is left over from the Cincinnati Uplift, sloping the rock layers from a high in the East sloping downward towards Cairo, Illinois.

AttributesValues
rdf:type
rdfs:label
  • Mitchell Plain (en)
rdfs:comment
  • The Mitchell Plain is a karst area in Indiana of relatively low relief. The extensive underlying cave system developed in Mississippian age limestone bedrock. Surface drainage is rare due to most streams in the area disappearing into caves or joints within the rock. The limestone is a vestige of an early shallow cratonic sea that covered what would become Indiana, while the North-South linearity of the region is left over from the Cincinnati Uplift, sloping the rock layers from a high in the East sloping downward towards Cairo, Illinois. (en)
geo:lat
geo:long
dcterms:subject
Wikipage page ID
Wikipage revision ID
Link from a Wikipage to another Wikipage
sameAs
dbp:wikiPageUsesTemplate
georss:point
  • 38.416666666666664 -86.16666666666667
has abstract
  • The Mitchell Plain is a karst area in Indiana of relatively low relief. The extensive underlying cave system developed in Mississippian age limestone bedrock. Surface drainage is rare due to most streams in the area disappearing into caves or joints within the rock. The limestone is a vestige of an early shallow cratonic sea that covered what would become Indiana, while the North-South linearity of the region is left over from the Cincinnati Uplift, sloping the rock layers from a high in the East sloping downward towards Cairo, Illinois. The Mitchell Plain is bound by the older rocks of Norman Upland on the East and the younger rocks of Crawford Upland on the West. (en)
gold:hypernym
prov:wasDerivedFrom
page length (characters) of wiki page
foaf:isPrimaryTopicOf
geo:geometry
  • POINT(-86.166664123535 38.416667938232)
is Link from a Wikipage to another Wikipage of
is foaf:primaryTopic of
Faceted Search & Find service v1.17_git139 as of Feb 29 2024


Alternative Linked Data Documents: ODE     Content Formats:   [cxml] [csv]     RDF   [text] [turtle] [ld+json] [rdf+json] [rdf+xml]     ODATA   [atom+xml] [odata+json]     Microdata   [microdata+json] [html]    About   
This material is Open Knowledge   W3C Semantic Web Technology [RDF Data] Valid XHTML + RDFa
OpenLink Virtuoso version 08.03.3330 as of Mar 19 2024, on Linux (x86_64-generic-linux-glibc212), Single-Server Edition (378 GB total memory, 50 GB memory in use)
Data on this page belongs to its respective rights holders.
Virtuoso Faceted Browser Copyright © 2009-2024 OpenLink Software