Blue ice occurs when snow falls on a glacier, is compressed, and becomes part of the glacier. Air bubbles are squeezed out and ice crystals enlarge, making the ice appear blue.

Small amounts of regular ice appear to be white because of air bubbles inside them and also because small quantities of water appear to be colourless. In glaciers, the pressure causes the air bubbles to be squeezed out, increasing the density of the created ice. Large quantities of water appear to be blue, as it absorbs other colours more efficiently than blue. A large piece of compressed ice, or a glacier, similarly appears blue.
A science team has been dispatched to the Arctic for a study project. The teams objective is to study various forms of ice formations. They will look at a glacier in the area, and also a frozen over lake. The team is excited to gather different data while on the trip.
Will there be more or less white ice at the glacier than the frozen lake?