sailing icebergs that have lately combined over.
This cave in the glacier ice is caused by glacial work, or Moulin where rainfall and liquefy water on the glacier area are routed into sources that get into the glacier at cracks. The fountain touches an opening into the glacier while the ponded water empties towards reduced heights by developing lengthy ice caverns with an store at the terminus of the glacier. The excellent grained sediments in the water along with breeze flow offered sediments cause the freezing meltwater flow to appear in a dirty color while the top of the cave displays the dark azure color. Due to the quick activity of the glacier of about 1 m per day over irregular geography, this ice cave damaged up at its end into an in-depth straight crevice, known as cerrac. This causes the oblique sunlight to get into the ice cave from both stops leading to homogeneous illumination of the ice tube.
he cave is available through a 22-foot entry on the coastline. At the end it tapers to a limited press no more than four legs great. Ice caverns are in common volatile factors and can failure whenever. They are secure to get into only during the freezing months months season when the freezing conditions firm up the ice. Even so one could listen to continuous breaking appears to be within the cave. It was not because it was going to failure but because the cave was going along with the glacier itself. Everytime the glacier shifted a millimeter noisy appears to be could be observed.