| dbo:abstract
|
- The Tin Mountain pegmatite is an igneous intrusion located in the southern Black Hills, South Dakota. It is a part of the Harney Peak Granite dome that formed in the Late Paleoproterozoic around 1.7 billion years ago. The Harney Peak Granite system includes thousands of pegmatites, one of which is the Tin Mountain. The Tin Mountain pegmatite is rich in lithium, but was first mined in search of tin, which gave the mountain its name. (en)
|
| dbo:thumbnail
| |
| dbo:wikiPageID
| |
| dbo:wikiPageLength
|
- 6421 (xsd:nonNegativeInteger)
|
| dbo:wikiPageRevisionID
| |
| dbo:wikiPageWikiLink
| |
| dbp:age
|
- Late Paleoproterozoic, ~1.7 Ga (en)
|
| dbp:caption
|
- Geological map showing the Tin Mountain pegmatite and the associated Harney Peak Granite system . (en)
|
| dbp:extent
| |
| dbp:name
|
- Tin Mountain pegmatite (en)
|
| dbp:prilithology
| |
| dbp:region
|
- Black Hills of South Dakota (en)
|
| dbp:type
| |
| dbp:wikiPageUsesTemplate
| |
| dcterms:subject
| |
| rdfs:comment
|
- The Tin Mountain pegmatite is an igneous intrusion located in the southern Black Hills, South Dakota. It is a part of the Harney Peak Granite dome that formed in the Late Paleoproterozoic around 1.7 billion years ago. The Harney Peak Granite system includes thousands of pegmatites, one of which is the Tin Mountain. The Tin Mountain pegmatite is rich in lithium, but was first mined in search of tin, which gave the mountain its name. (en)
|
| rdfs:label
|
- Tin Mountain pegmatite (en)
|
| owl:sameAs
| |
| prov:wasDerivedFrom
| |
| foaf:depiction
| |
| foaf:isPrimaryTopicOf
| |
| is foaf:primaryTopic
of | |
