Mount Kembar

Mount Kembar is a shield volcano in Aceh featuring two prominent peaks rising roughly 2,245 meters above sea level. Its broad slopes contain a geothermal field called Gayolesten marked by steaming vents and active gas emissions.

The volcano formed during the Pleistocene when two major fault lines intersected in the northern Sumatra region. This geological past shaped the mountain's dual structure and the thermal system that remains active today.

The mountain is known locally as Twin Mountain, a name reflecting its distinctive double peak that stands out in the landscape. Local residents have woven stories and meanings around this formation that remain part of their regional identity today.

Visitors must obtain permits from local authorities before attempting the climb and should bring proper hiking gear and safety equipment. The steep terrain and altitude require good physical fitness and careful preparation before heading out.

The mountain's two peaks resulted from the intersection of two fault lines that continuously feed energy to the Gayolesten geothermal field. This rare geological arrangement makes the site an example of how plate tectonics shapes the visible landscape.