Diamond Craters Explained

Diamond Craters
Map:Oregon
Location:Harney County, Oregon, U.S.
Coordinates:43.1°N -118.75°W
Elevation Ft:4707
Elevation Ref:[1]
Range:Basin and Range
Topo:USGS Diamond Swamp
Type:Volcanic field / shield volcano
Age:7320 to 7790 calendar years. B.P.[2]
Easiest Route:roads and trails
Map Width:240

The Diamond Craters is a monogenetic volcanic field about 40miles southeast of Burns, Oregon. The field consists of a 270NaN0 area of basaltic lava flows, cinder cones, and maars. The reexamination of radiocarbon dates from older studies and interpretation of paleomagnetic data and new radiocarbon dates limits the eruption of volcanic vents in this volcanic field to the time period between 7320 and 7790 calendar years B.P.[2] [3]

Diamond Craters and the nearby Diamond post office were named after the Diamond Ranch, established in the area by the pioneer Mace McCoy. The ranch used a diamond-shaped brand, hence the name.[3] [4]

In the 1970s, Diamond Craters was a source of controversy between the Bureau of Land Management and commercial stonecutters who were illegally removing slabs of lava to sell as veneer for fireplaces, home exteriors, and chimneys.[5] Geologists familiar with the area cited the craters' unusual research value, a "museum of basaltic volcanic features" apt to be destroyed by slab harvesting and associated heavy equipment.[5] In 1982, the area gained additional protection when it was designated an Outstanding Natural Area.[4]

Notable vents

Name Elevation Last eruption
Big Bomb Crater[6] 1308m (4,291feet) 43° 04' 34.64" N, 118° 44' 59.13" W -
Central Crater Complex 1378m (4,521feet) 43° 05' 38.48" N, 118° 47' 08.53" W -
Cloverleaf Crater- 43° 05' 21.54" N, 118° 43' 58.84" W -
Dry Maar 1268m (4,160feet) 43° 06' 11.92" N, 118° 49' 04.55" W -
East Twin Crater 1326m (4,350feet) 43° 05' 52.83" N, 118° 48' 19.46" W -
Keyhole Explosion Crater - 43° 05' 07.30" N, 118° 45' 30.12" W -
Lava Pit Crater 1305m (4,281feet) 43° 04' 32.66" N, 118° 45' 24.06" W -
Little Red Cone - 43° 06' 11.57" N, 118° 44' 44.17" W -
Malheur Maar 1286m (4,219feet) 43° 06' 14.68" N, 118° 48' 59.54" W -
Nolf Crater[7] - 43° 06' 26.54" N, 118° 48' 15.60" W -
Oval Crater - 43° 04' 56.85" N, 118° 45' 56.88" W -
Red Bomb Crater 1323m (4,341feet) 43° 04' 39.94" N, 118° 46' 08.23" W -
West Twin Crater 1326m (4,350feet) 43° 05' 56.52" N, 118° 48' 31.70" W -

External links

Notes and References

  1. 322170. Diamond Craters.
  2. Sherrod, D.R., D.E. Champion, and J.P. McGeehin (2012) Age and duration of volcanic activity at Diamond Craters, southeastern Oregon. Journal of Volcanology and Geothermal Research. 247–248:108–114
  3. Peterson, N.V. and Groh, E.A., 1964. Diamond Craters, Oregon. Ore Bin, 26(2), pp.17-34.
  4. Book: McArthur, Lewis A. . Lewis A. McArthur . McArthur. Lewis L.. Lewis L. McArthur . . 1928 . 7th. 2003 . Oregon Historical Society Press . Portland, Oregon. 0-87595-277-1 . 286.
  5. News: Hofferber. Connie. BLM, Stonecutters Square Off Over Mining Diamond Craters. NewsBank. The Oregonian. August 3, 1979. 69. January 4, 2016. subscription .
  6. Bureau of Land Management, 2021. Diamond Craters Outstanding Natural Area. Bureau of Land Management, Washington, D.C. 1 map.
  7. Mehringer, P.J., and P.E. Wigand. 1990. Comparison of late Holocene environments from woodrat middens and pollen. Pages 294–325 in J.L. Betancourt, T.R. Van Devender, and P.S. Martin (eds.). Packrat middens: the last 40,000 years of biotic change. University of Arizona Press, Tucson.