Bus-Obo is a high cinder cone in Mongolia. The high cone is formed by basaltic rocks. It may be of Pleistocene or Holocene age.
Bus-Obo is a high cinder cone in Mongolia. The high cone is formed by basaltic rocks. It may be of Pleistocene or Holocene age.
It is located within a Caledonian orogenic belt in Mongolia, in the Middle Gobi area. A low velocity zone in the mantle is associated with Bus-Obo. Other Pliocene to Pleistocene age lava flows and craters are found within the adjacent Orchon valley, their relationship to this cone is unknown.
Discovered by embedding cosine similarity (sentence-transformers MiniLM, 384-dim).