Hoodoo refers to tall, thin columns of rock formed through natural erosion processes, particularly differential weathering, where softer rock erodes faster than harder rock. Examples, like those in Bryce Canyon, showcase these unique geologic formations worldwide.
Hoodoo typically refers to a geologic formation characterized by tall, thin columns of rock, often composed of sedimentary or volcanic material. These columns are the result of natural erosion processes over extended periods of time. The most common type of hoodoo is the result of differential weathering, where softer rock erodes more quickly than harder rock, leaving behind unique pillar-like structures.
One well-known example of hoodoos is found in Bryce Canyon National Park in the United States, where a collection of intricate and striking hoodoos has been shaped by the forces of erosion. Hoodoos can also be found in various other geological landscapes globally, each exhibiting its distinct characteristics based on the local geological composition and weathering processes.