Cinder Cone is a prominent feature located in the Pacific Ranges mountain range. Standing at an elevation of approximately 6,879 feet (2,097 meters), it is a volcanic cone formed by an eruption in the late 17th century. This cone-shaped mountain covers an area of about 2 square miles (5 square kilometers) and is characterized by its unique composition of volcanic cinders and ash.

During the winter season, Cinder Cone experiences a significant snowpack range, thanks to its location in a region with a relatively high annual snowfall. The snowpack can reach depths of several feet, making it a popular destination for winter sports enthusiasts. This mountain's snow-covered slopes provide excellent opportunities for activities such as skiing, snowboarding, and snowshoeing.

Cinder Cone is also known for its contribution to the local hydrology. Several creeks and rivers in the surrounding area receive runoff from the mountain's melting snowpack during the warmer months. This runoff sustains the flow of water in these waterways, ensuring a healthy ecosystem for various plant and animal species.

The name "Cinder Cone" accurately describes the mountain's appearance and geological composition. It has a rich history, with Native American tribes having their own legends and lore associated with the mountain. It is important to consult multiple independent sources to ensure accuracy and gather a comprehensive understanding of Cinder Cone's significance in the Pacific Ranges mountain range.

• Camp

• Streamgauges