Many of Mount Rainier’s lava flows are andesite. This type of lava tends to be moderately viscous and slow moving. The amount of silica in the lava differentiates it from other types of lava like basalt, which has 45 to 53 percent silica. The less silica a lava contains, the more fluid it is and less viscous, or “sticky”. As it cools, the andesite lava turns into grey rock that can fracture into columns, called columnar jointing. These formations are visible in several locations in the park, particularly along the Sunrise Road. (The Sunrise area typically opens for the season in July).