Columbia River Basalt Group
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Columbia River Basalt Group
Summary
Columbia River Basalt Group is a large igneous province[1]. It draws 202 Wikipedia views per month (large_igneous_province category, ranking #4 of 14).[2]
Key Facts
- Columbia River Basalt Group is in the country of United States[3].
- Columbia River Basalt Group's instance of is recorded as large igneous province[4].
- Columbia River Basalt Group's instance of is recorded as group[5].
- Columbia River Basalt Group's Commons category is recorded as Columbia River Basalt Group[6].
- Columbia River Basalt Group's has part is recorded as Grande Ronde Basalt[7].
- Columbia River Basalt Group's has part is recorded as Imnaha Basalt[8].
- Columbia River Basalt Group's has part is recorded as Picture Gorge Basalt[9].
- Columbia River Basalt Group's has part is recorded as Saddle Mountains Basalt[10].
- Columbia River Basalt Group's has part is recorded as Wanapum Basalt[11].
- Columbia River Basalt Group's has part is recorded as Weiser Basalt[12].
- Columbia River Basalt Group's underlies is recorded as Rattlesnake Formation[13].
- Columbia River Basalt Group's overlies is recorded as John Day Formation[14].
- Columbia River Basalt Group's Freebase ID is recorded as /m/0262dcd[15].
- Columbia River Basalt Group's topic's main category is recorded as Category:Columbia River Basalt Group[16].
- Columbia River Basalt Group's Commons gallery is recorded as Columbia River Basalt Group[17].
- Columbia River Basalt Group's described at URL is recorded as https://ngmdb.usgs.gov/Geolex/UnitRefs/ColumbiaRiverRefs_7672.html[18].
- Columbia River Basalt Group's Geolex ID is recorded as ColumbiaRiver_7672[19].
Body
Geography
Columbia River Basalt Group is in the country of United States[3].
Designation and Status
Recorded instance of include large igneous province[4] and group[5].
Why It Matters
Columbia River Basalt Group draws 202 Wikipedia views per month (large_igneous_province category, ranking #4 of 14).[2] It is known by 5 alternative names across languages and contexts.[20]