This HTML5 document contains 47 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/
yago-reshttp://yago-knowledge.org/resource/
dbohttp://dbpedia.org/ontology/
foafhttp://xmlns.com/foaf/0.1/
n14http://ceb.dbpedia.org/resource/
geohttp://www.w3.org/2003/01/geo/wgs84_pos#
n4https://global.dbpedia.org/id/
yagohttp://dbpedia.org/class/yago/
n20http://www.pc.gc.ca/pn-np/bc/glacier/natcul/natcul1/
dbthttp://dbpedia.org/resource/Template:
n19http://arz.dbpedia.org/resource/
rdfshttp://www.w3.org/2000/01/rdf-schema#
dbpedia-svhttp://sv.dbpedia.org/resource/
freebasehttp://rdf.freebase.com/ns/
rdfhttp://www.w3.org/1999/02/22-rdf-syntax-ns#
owlhttp://www.w3.org/2002/07/owl#
n21https://www.gutenberg.org/files/51042/51042-h/
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#
goldhttp://purl.org/linguistics/gold/
wikidatahttp://www.wikidata.org/entity/
dbrhttp://dbpedia.org/resource/
georsshttp://www.georss.org/georss/
n15http://sws.geonames.org/6085645/

Statements

Subject Item
dbr:Nakimu_Caves
rdf:type
yago:PhysicalEntity100001930 geo:SpatialThing yago:GeologicalFormation109287968 yago:WikicatCavesOfBritishColumbia yago:Cave109238926 yago:YagoPermanentlyLocatedEntity yago:YagoGeoEntity yago:Object100002684
rdfs:label
Nakimu Caves Nakimu Caves
rdfs:comment
The Nakimu Caves are a cave system located in Glacier National Park in British Columbia, Canada. The caves run for six kilometres in the central region of the park. The name means "grumbling spirits" in the Shuswap language. They were formed by the action of Cougar Brook on a soluble limestone strata. The access is through Balu Pass. The caves consist of marbloid rocks from the Cambrian period, many of which exhibit scalloping patterns. The cave contains cauliflower-shaped agglomerations of a substance called moonmilk; this is a precipitate of calcium carbonate and bacteria. Nakimu Caves är en grotta i Kanada. Den ligger i provinsen British Columbia, i den centrala delen av landet, 3 100 km väster om huvudstaden Ottawa. Nakimu Caves ligger 1 976 meter över havet. Terrängen runt Nakimu Caves är bergig. Den högsta punkten i närheten är 2 627 meter över havet, 1,6 km norr om Nakimu Caves. Trakten runt Nakimu Caves är nära nog obefolkad, med mindre än två invånare per kvadratkilometer..
geo:lat
51.27916717529297
geo:long
-117.591667175293
dcterms:subject
dbc:Glacier_National_Park_(Canada) dbc:Caves_of_British_Columbia
dbo:wikiPageID
39230574
dbo:wikiPageRevisionID
1060643047
dbo:wikiPageWikiLink
dbr:Revelstoke,_British_Columbia dbr:Shuswap_language dbc:Caves_of_British_Columbia dbr:Illecillewaet_River dbr:Glacier_House dbr:Parks_Canada dbr:Moonmilk dbc:Glacier_National_Park_(Canada) dbr:Glacier_National_Park_(Canada)
dbo:wikiPageExternalLink
n20:j.aspx n21:51042-h.htm
owl:sameAs
n4:fKGA dbpedia-sv:Nakimu_Caves yago-res:Nakimu_Caves freebase:m.0tkk61c n14:Nakimu_Caves n15: n19:كهوف_ناكيمو wikidata:Q17081300
dbp:wikiPageUsesTemplate
dbt:Reflist dbt:Coord
georss:point
51.27916666666667 -117.59166666666667
dbo:abstract
Nakimu Caves är en grotta i Kanada. Den ligger i provinsen British Columbia, i den centrala delen av landet, 3 100 km väster om huvudstaden Ottawa. Nakimu Caves ligger 1 976 meter över havet. Terrängen runt Nakimu Caves är bergig. Den högsta punkten i närheten är 2 627 meter över havet, 1,6 km norr om Nakimu Caves. Trakten runt Nakimu Caves är nära nog obefolkad, med mindre än två invånare per kvadratkilometer.. Trakten runt Nakimu Caves består i huvudsak av gräsmarker. Trakten ingår i den hemiboreala klimatzonen. Årsmedeltemperaturen i trakten är −5 °C. Den varmaste månaden är augusti, då medeltemperaturen är 10 °C, och den kallaste är december, med −16 °C. The Nakimu Caves are a cave system located in Glacier National Park in British Columbia, Canada. The caves run for six kilometres in the central region of the park. The name means "grumbling spirits" in the Shuswap language. They were formed by the action of Cougar Brook on a soluble limestone strata. The access is through Balu Pass. The caves were discovered in 1902 by D. Woolsey and W. Scott. They were more thoroughly explored in 1904 by Revelstoke resident Charles Deutchmann, and were called both Cheop's Caves and Deutchmann Caves before being called Nakimu. Deutchmann signed a contract with Parks Canada to operate tours in the caves. A teahouse was constructed near the cave mouth and a road was built from the Illecillewaet River valley. During the heyday of in the early 1900s, Deutchmann constructed a series of wooden stairs and boardwalks and the caves were visited heavily by tourists. The natural features were significantly damaged by human contact during the period. The Nakimu Caves had for a period what was considered the only true "show" cave among the Canadian national parks, although this section was closed in 1935 because of decreased tourist attendance. Parks removed the remnants of Deutchmann's construction, and closed the caves completely to all but experienced cavers with permits. The caves consist of marbloid rocks from the Cambrian period, many of which exhibit scalloping patterns. The cave contains cauliflower-shaped agglomerations of a substance called moonmilk; this is a precipitate of calcium carbonate and bacteria.
gold:hypernym
dbr:System
prov:wasDerivedFrom
wikipedia-en:Nakimu_Caves?oldid=1060643047&ns=0
dbo:wikiPageLength
3088
foaf:isPrimaryTopicOf
wikipedia-en:Nakimu_Caves
geo:geometry
POINT(-117.59166717529 51.279167175293)