kantsideslipning

Kantsideslipning is a phenomenon that originated in Norway, specifically in the region of Telemark, in the 19th century. The name is derived from a contraction of the Norwegian words "Kanten" meaning "the edge" and "sideslippning" meaning "sideways slip". It is a type of sliding or gliding that occurs on snow-covered slopes when an individual uses one ski to initiate the descent while the other ski remains parallel to the ground, generating a small amount of speed and control.

This technique was popularized by Norwegian skiers in the late 19th century, particularly by enthusiasts of the sport in the Telemark region. It was initially used for both recreational and competitive purposes. Kantsideslipning was considered a crucial skill for downhill skiing, allowing skiers to maintain speed and control while navigating steep and icy slopes.

Kantsideslipning is distinct from other skiing techniques, such as the now more widely used parallel turn. The key difference between the two lies in how the skis are positioned and how they interact with the snow. Kantsideslipning involves shifting one ski sideways while maintaining the other ski parallel to the ground, which generates a lateral force that propels the skier downward.

While kantsideslipning is not as widely practiced today as it once was, it remains an important part of Norwegian skiing history and is sometimes used in vintage skiing events or as a nostalgic throwback to the early days of the sport.