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This volcanic cone’s type is a horseshoe-shaped crater (northeast). The crater is formed from a gradual ridge and was actually large and circular, but secondary lava eruption resulted in the crater bursting to the northeast.
Inside the crater is a low Al Oreum Volcanic Cone created as a result of sliding to the north, and while it is written as Min Oreum Volcanic Cone Al Oreum Volcanic Cone, it has no relation to Min Oreum Volcanic Cone and is rather an eroded portion and outer rim of Keundolimi Volcanic Cone.
At the summit of the volcanic cone are fresh lava boulders that serve as the remains of lava flow, and other regions of the volcanic cone are covered in grass, creating an artificial grassland within the crater. In maps (1:25,000), ‘Jakeundolimi Volcanic Cone’ is actually ‘Keundolimi Volcanic Cone’, and ‘Jakeundolimi Volcanic Cone’ is actually the long hill with rocks 500m to the northeast of the volcanic cone, past the eroded valley.