gptkbp:instance_of
|
gptkb:geological_formation
|
gptkbp:bfsLayer
|
6
|
gptkbp:bfsParent
|
gptkb:Witwatersrand_Basin
|
gptkbp:age
|
approximately 3.1 billion years
|
gptkbp:associated_with
|
Banded Iron Formation
|
gptkbp:composed_of
|
gptkb:organization
shale
quartzite
|
gptkbp:contains
|
gptkb:dinosaur
gold deposits
|
gptkbp:cultural_significance
|
local heritage
|
gptkbp:depicted_in
|
gptkb:Johannesburg
|
gptkbp:diameter
|
up to 10,000 meters
|
gptkbp:discovered_by
|
1886
gold prospectors
|
gptkbp:features
|
sedimentary rocks
|
gptkbp:formed
|
Neoarchaean era
|
gptkbp:founded
|
tectonic processes
|
gptkbp:has_impact_on
|
gptkb:local_economy
|
gptkbp:has_influence_on
|
regional geology
|
gptkbp:historical_significance
|
gold rush era
|
https://www.w3.org/2000/01/rdf-schema#label
|
Witwatersrand Supergroup
|
gptkbp:includes
|
Central Rand Group
East Rand Group
West Rand Group
|
gptkbp:influences
|
local geology
|
gptkbp:is_associated_with
|
mineralization events
|
gptkbp:is_atype_of
|
gptkb:Transvaal_Supergroup
Chuniespoort Group
|
gptkbp:is_characterized_by
|
metamorphic processes
|
gptkbp:is_essential_for
|
paleontology
|
gptkbp:is_explored_in
|
geological surveys
|
gptkbp:is_home_to
|
various ecosystems
|
gptkbp:is_known_for
|
rich mineral resources
|
gptkbp:is_located_near
|
Johannesburg Goldfields
|
gptkbp:is_part_of
|
gptkb:Witwatersrand_Basin
South African geology
|
gptkbp:is_recognized_by
|
gptkb:archaeological_site
|
gptkbp:is_studied_in
|
geologists
stratigraphy
geological expeditions
|
gptkbp:is_subject_to
|
environmental studies
|
gptkbp:is_used_in
|
educational research
|
gptkbp:is_valued_for
|
geological diversity
|
gptkbp:is_vulnerable_to
|
mining activities
mining companies
|
gptkbp:judges
|
geological time scale
|
gptkbp:located_in
|
gptkb:South_Africa
|
gptkbp:named_after
|
geologists
Witwatersrand region
|
gptkbp:part_of
|
gptkb:Kaapvaal_Craton
|
gptkbp:research_interest
|
geological history
|
gptkbp:significance
|
gold mining
economic geology
|
gptkbp:strategic_importance
|
high-value minerals
|