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这些火山锥是苏加塔谷和图尔卡纳湖之间火山杂岩的一部分。
These cinder cones are part of a broad volcanic complex between the Suguta Valley and Lake Turkana to the north.
这些火山锥在大小和形状上与在冰岛发现的火山锥颇为相似。
These cones are similar in size and shape to cones found in Iceland.
被融化的岩石由于粘性较低,因此能轻易流到岩石层上方形成火山锥。
The melted rock has a low viscosity, and it flows easily up through the overlying rock.
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