Glaciers are massive sheets of ice, sliding slowly down a mountain and carving enormous grooves in the land. They flow down to the lowest point where gravity can take them, often into the ocean. The normal school of thought for these "tidewater glaciers" said that due to their weight and compaction to the earth's surface, they were grounded on the sea floor, only to arise once disintegrated. However, there is one glacier that extends into the water, floating intact on the ocean waves.