Round Mountain (California)
{{Short description|Round Mountain Volcano - California}}
{{Infobox mountain
| name = Round Mountain
| elevation_ft = 2,294
| last_eruption = 8,500–10,000 years ago
| volcanic_field = Clear Lake Volcanic Field
| photo = Round Mountain Volcano.jpg
| coordinates = {{coords|39.048955|N|122.636205|W}}
| location = Lake County, Clearlake Oaks, California, USA
| type = Cinder cone
}}
Round Mountain is a dormant volcanic cinder cone located in the Clear Lake Volcanic Field in the eastern end of the High Valley. It last erupted approximately 8,500–10,000 years ago and filled the valley with volcanic debris, raising the valley level to 400 feet above Clear Lake.{{Cite web |last=Sutton |first=Nancy |date=July 1, 2005 |title=Establishment of the High Valley Viticultural Area (2003R-361P) |url=https://www.federalregister.gov/d/05-13042/p-27 |website=Federal Register}}
The Clear Lake Volcanic Field is the site of Late Pliocene to early Holocene activity and consists of lava domes, cinder cones, and maars{{Cite journal |last=Ball |first=Jessica |date=September 1, 2022 |title=Stratigraphy and eruption history of maars in the Clear Lake Volcanic Field, California |journal=Frontiers in Earth Science |volume=10 |doi=10.3389/feart.2022.911129 |doi-access=free }} with eruptive products varying from basalt to rhyolite. The site's threat level is ranked "High" at #33 in the top volcanic threats in the United States in 2018 Update to the United States Geological Survey National Volcanic Threat Assessment. Cobb Mountain and Mount Konocti are the two highest peaks in the volcanic field, at {{cvt|4,724|ft|m}} and {{cvt|4,285|ft|m}} respectively.
Geography
The Geologic History of the surrounding area including the volcano (which is covered with heavy concentrations of chaparral, oak, Pacific madrone, manzanita, western white pine and other plant species of the California coastal mountains) has been studied and documented by the USGS and prominent geologists as far back as 1938. At an approximate elevation of {{cvt|2,294|ft|m}} the volcano exhibits a distinctive sunken concave of a cinder cone volcano.
History
The volcano is credited with the creation of the High Valley through repeated eruptions the last of which is thought to have occurred 8,500–10,000 years ago. The result was an elevated valley at approximately {{cvt|1,600|ft|m}} in elevation with distinct ridgelines reaching up to {{cvt|3,000|ft|m}}.{{Cite web |title=Lake County's Volcanic Soils |url=https://www.lakecountywinegrape.org/volcanics/lake-county-soil/ |access-date=2024-07-31 |website=Lake County Winegrape Commission}}