This HTML5 document contains 89 embedded RDF statements represented using HTML+Microdata notation.

The embedded RDF content will be recognized by any processor of HTML5 Microdata.

Namespace Prefixes

PrefixIRI
dctermshttp://purl.org/dc/terms/
dbohttp://dbpedia.org/ontology/
foafhttp://xmlns.com/foaf/0.1/
geohttp://www.w3.org/2003/01/geo/wgs84_pos#
n12https://global.dbpedia.org/id/
dbthttp://dbpedia.org/resource/Template:
rdfshttp://www.w3.org/2000/01/rdf-schema#
n9http://commons.wikimedia.org/wiki/Special:FilePath/
rdfhttp://www.w3.org/1999/02/22-rdf-syntax-ns#
owlhttp://www.w3.org/2002/07/owl#
wikipedia-enhttp://en.wikipedia.org/wiki/
dbchttp://dbpedia.org/resource/Category:
dbphttp://dbpedia.org/property/
provhttp://www.w3.org/ns/prov#
xsdhhttp://www.w3.org/2001/XMLSchema#
wikidatahttp://www.wikidata.org/entity/
dbrhttp://dbpedia.org/resource/
georsshttp://www.georss.org/georss/

Statements

Subject Item
dbr:Eldon_Formation
rdf:type
geo:SpatialThing
rdfs:label
Eldon Formation
rdfs:comment
The Eldon Formation is a stratigraphic unit that is present on the western edge of the Western Canada Sedimentary Basin in the southern Canadian Rockies of southwestern Alberta and southeastern British Columbia. It is a thick sequence of massive, cliff-forming limestones and dolomites that was named for Eldon Switch on the Canadian Pacific Railway near Castle Mountain in Banff National Park by Charles Doolittle Walcott, who discovered the Burgess Shale fossils. The Eldon Formation was deposited during Middle Cambrian time, and it includes fossil stromatolites. The Eldon forms the scenic cliffs at the top of Castle Mountain, and can also be seen at Mount Yamnuska and other mountains in Banff and Yoho National Parks.
dbp:name
Eldon Formation
geo:lat
51.30236053466797
geo:long
-115.9291687011719
foaf:depiction
n9:Mount-Yamnuska2-Szmurlo.jpg
dcterms:subject
dbc:Geologic_formations_of_Canada dbc:Cambrian_British_Columbia dbc:Cambrian_System_of_North_America dbc:Cambrian_Alberta dbc:Geologic_formations_of_Alberta dbc:Western_Canadian_Sedimentary_Basin dbc:Stratigraphy_of_British_Columbia
dbo:wikiPageID
60611467
dbo:wikiPageRevisionID
904430249
dbo:wikiPageWikiLink
dbr:Limestone dbr:Dolomite_(mineral) dbc:Cambrian_Alberta dbc:Cambrian_British_Columbia dbc:Geologic_formations_of_Alberta dbc:Cambrian_System_of_North_America dbr:Mount_Yamnuska dbr:Laurentia dbr:British_Columbia dbc:Western_Canadian_Sedimentary_Basin dbr:Supratidal_zone dbr:Castle_Mountain dbr:Stephen_Formation dbr:Stratigraphic_unit dbr:Fossils_of_the_Burgess_Shale dbr:Mudstone dbr:Charles_Doolittle_Walcott dbr:Fossil dbr:Pika_Formation dbr:Calcite dbr:Dolomitization dbr:Earlie_Formation dbr:Yoho_National_Park dbr:Western_Canadian_Sedimentary_Basin dbr:Limestones dbr:Snake_Indian_Formation dbr:Titkana_Formation dbr:Stromatolites dbc:Stratigraphy_of_British_Columbia dbr:Banff_National_Park dbr:Dolomite_(rock) dbr:Mount_Bosworth dbr:Fossils_of_the_Burgess_shale dbr:Stratigraphy dbr:Carbonate_rock dbr:Chancellor_Formation dbr:Intertidal_zone dbr:Windsor_Mountain_Formation dbr:Middle_Cambrian dbr:Canadian_Pacific_Railway dbr:Canadian_Rockies dbc:Geologic_formations_of_Canada dbr:Alberta
owl:sameAs
wikidata:Q65040376 n12:9jd4L
dbp:underlies
dbr:Pika_Formation
dbp:wikiPageUsesTemplate
dbt:Fossil_range dbt:Western_Canadian_Sedimentary_Basin dbt:Short_description dbt:Reflist dbt:Infobox_rockunit dbt:Flag dbt:Coord
dbo:thumbnail
n9:Mount-Yamnuska2-Szmurlo.jpg?width=300
dbp:age
dbr:Middle_Cambrian ~
dbp:caption
The Eldon Formation forms the cliffs of Mount Yamnuska in Alberta
dbp:region
dbr:Canadian_Rockies
dbp:thickness
Up to 500 metres
dbp:type
dbr:Stratigraphic_unit
georss:point
51.30236111111111 -115.92916666666666
dbo:abstract
The Eldon Formation is a stratigraphic unit that is present on the western edge of the Western Canada Sedimentary Basin in the southern Canadian Rockies of southwestern Alberta and southeastern British Columbia. It is a thick sequence of massive, cliff-forming limestones and dolomites that was named for Eldon Switch on the Canadian Pacific Railway near Castle Mountain in Banff National Park by Charles Doolittle Walcott, who discovered the Burgess Shale fossils. The Eldon Formation was deposited during Middle Cambrian time, and it includes fossil stromatolites. The Eldon forms the scenic cliffs at the top of Castle Mountain, and can also be seen at Mount Yamnuska and other mountains in Banff and Yoho National Parks.
dbp:namedby
Charles Doolittle Walcott in 1908
dbp:namedfor
Eldon Switch on the Canadian Pacific Railway in Banff National Park, Alberta
dbp:otherlithology
dbr:Mudstone
dbp:overlies
dbr:Snake_Indian_Formation dbr:Stephen_Formation
dbp:prilithology
dbr:Limestone dbr:Dolomite_(rock)
prov:wasDerivedFrom
wikipedia-en:Eldon_Formation?oldid=904430249&ns=0
dbo:wikiPageLength
5368
foaf:isPrimaryTopicOf
wikipedia-en:Eldon_Formation
geo:geometry
POINT(-115.92916870117 51.302360534668)