Cinder Cone

While the intro suggests warmer months for optimal enjoyment, winter access to Cinder Cone can be challenging due to snow. The park roads, including the one leading to Butte Lake, may close seasonally. Always check the official Lassen Volcanic National Park website for current road conditions and trail status before planning a winter visit.

In Lassen Volcanic National Park, pets are generally permitted only on paved roads, in campgrounds, and in developed areas. They are typically not allowed on hiking trails, including the Cinder Cone trail, to protect wildlife and natural resources. Always verify current pet regulations on the official park website before your visit.

Cinder Cone is located within Lassen Volcanic National Park, so a park entrance fee is required. This fee grants access to the park for a set number of days. No additional permits are typically needed for day hiking the Cinder Cone trail itself, but always check the National Park Service website for any updated regulations or specific backcountry permits if planning extended trips.

The Painted Dunes are older formations, created during an earlier eruptive phase of Cinder Cone (between 1630 and 1666 CE). Their vibrant colors come from the oxidation of volcanic ash. The Fantastic Lava Beds were formed during a later eruptive phase, when basalt lava flows erupted from Cinder Cone's base, spreading northeast and southwest. These flows dammed creeks, creating Snag Lake and Butte Lake.

The Cinder Cone trail is approximately 4 miles (6.4 km) round trip from the Butte Lake trailhead. While the ascent to the summit is steep and challenging, the entire hike typically takes 2-4 hours, depending on your pace and how much time you spend exploring the summit and crater.

Yes, while the Cinder Cone summit hike is challenging, the area around Butte Lake offers more accessible options. The historic Nobles Emigrant Trail follows the edge of the Fantastic Lava Beds and skirts Snag Lake, providing a flatter, scenic walk suitable for families. You can also enjoy the Butte Lake Day Use Area and its surroundings.

Cinder Cone was formed during two eruptive phases between 1630 and 1666 CE, making it the youngest scoria cone in the continental United States. The earlier phase created the Painted Dunes, and the later phase, ending in 1666 CE, produced the Fantastic Lava Beds. Scientists used dendrochemistry and carbon-14 dating from killed trees to pinpoint these eruption dates.

The trailhead for Cinder Cone is located near the boat ramp in the Butte Lake Day Use Area, where parking is available. However, like many popular national park destinations, parking can fill up quickly, especially during peak season (warmer months) and on weekends. Arriving early in the morning is highly recommended to secure a spot and avoid crowds on the trail.

The Butte Lake Day Use Area, where the Cinder Cone trailhead is located, typically offers basic amenities such as restrooms and potable water during the operating season. However, it's always wise to carry your own water, especially for the exposed and strenuous hike up Cinder Cone, and to check the park's website for current facility availability.

Yes, for those seeking an even closer look, there is an additional trail that allows hikers to descend into the bowl-shaped crater of Cinder Cone. This offers a unique perspective of the volcano's interior and is a memorable part of the experience for many visitors.

Beyond the impressive cone, visitors can observe the colorful Painted Dunes, formed from oxidized volcanic ash, and the vast Fantastic Lava Beds, which are basaltic lava flows. A unique characteristic of Cinder Cone is the presence of quartz xenoliths, which are pieces of quartz picked up from the underlying Sierra Nevada batholith by the magma as it rose to the surface.