Keluo (Chinese: 科洛, p Kēluò) is a dormant volcanic field 310 kilometers (190 mi) north-by-northwest of Daquijin in northeastern China.

It is located at an intersection of regional lineaments trending northeast and northwest; the volcanoes were erupted through basement igneous and sedimentary rocks from the Jurassic to Cretaceous, through granite, and through pre-Permian metasediments.

Like the Wudalianchi volcanic to its south, it contains high-potassium basaltic cinder cones.

[1] The field possesses 23 cones over an area of 350 km2 (140 sq mi).

The morphology of a number of the cones—including Nanshan (南山), Gushan (孤山), Jianshan (尖山), Dayishan (大椅山), and Xiaoyishan (小椅山)—suggests their formation during the last 10,000 years (the Holocene).