300px|thumb|Uran-Togoo Khanuy-Gol (also known as Bulgan Volcanic Field, Chanuj Gol Hanui Gol or Hanuy Gol) is a volcanic field in Mongolia. Khanuy-Gol is located in the northern Hangai range, north of the settlement of Bulgan. 300px|thumb|Topographic map It covers a surface area of southwest of Ulaanbaatar. Among the 10 cones with heights of that make up the field are Baga Togo Uul/Bogo-Togo-Ula (meaning "Little Togo Mountain", high, to ), Ikh Togo Uul/Ikha-Togo-Ula (meaning "Great Togo mountain", high, ), Togo, Urun Dush, and Uran Uul. This cone is the highest of the field, with a height of
300px|thumb|Uran-Togoo Khanuy-Gol (also known as Bulgan Volcanic Field, Chanuj Gol Hanui Gol or Hanuy Gol) is a volcanic field in Mongolia. Khanuy-Gol is located in the northern Hangai range, north of the settlement of Bulgan. 300px|thumb|Topographic map It covers a surface area of southwest of Ulaanbaatar. Among the 10 cones with heights of that make up the field are Baga Togo Uul/Bogo-Togo-Ula (meaning "Little Togo Mountain", high, to ), Ikh Togo Uul/Ikha-Togo-Ula (meaning "Great Togo mountain", high, ), Togo, Urun Dush, and Uran Uul. This cone is the highest of the field, with a height of . Baga Togo Uul has one maar-like vent among its three vents, these vents are named Javalach, Togo and Tulga. Both Togo cones have a vegetation cover.
Volcanic activity began 12.5 ± 1.0 mya, with trachybasalts erupting along the Hanui river. Later two unnamed cones less than west of the river formed Pleistocene lava flows, one of which is thick. The last eruption is not dated, may be in the Holocene though, judging by Uran Uul's steep sided appearance. The Baga Togo Uul cones are certainly older than 3-4 ka and probably Pleistocene. The field is part of the Hangai volcanic region, which is in turn part of the Baikal rift zone. The Hangai region has been subject to tectonic uplift and high heat flow anomalies and hot springs are found.
Discovered by embedding cosine similarity (sentence-transformers MiniLM, 384-dim).