University of Kansas Campus | Lawrence

Information

Landmark: University of Kansas Campus
City: Lawrence
Country: USA Kansas
Continent: North America

University of Kansas Campus, Lawrence, USA Kansas, North America

Lost Creek State Park is a protected natural area located in Anaconda, Montana, USA.

Visual Characteristics

The park features a prominent limestone cliff face with a natural arch. The creek itself is characterized by clear, shallow water flowing over a gravel bed. Vegetation consists primarily of Ponderosa pine and various grasses adapted to arid conditions.

Location & Access Logistics

Lost Creek State Park is situated approximately 16 miles west of Anaconda, Montana. Access is via Montana Highway 1, turning onto County Road 102 (Lost Creek Road). The road is paved for the initial section and transitions to gravel. Parking is available at designated lots near the trailhead and picnic areas. No public transport services operate directly to the park.

Historical & Ecological Origin

The limestone formations are the result of geological processes occurring over millions of years, primarily erosion and deposition. The natural arch is a product of differential weathering. The area's ecology is representative of the Northern Rocky Mountains foothills, supporting a range of flora and fauna.

Key Highlights & Activities

Hiking the 1.5-mile loop trail to the natural arch is the primary activity. Rock climbing and bouldering are permitted on designated routes on the limestone cliffs. Picnicking is available at established sites. Wildlife viewing opportunities exist for deer and various bird species.

Infrastructure & Amenities

Restrooms are available at the main parking area. Picnic tables and fire rings are provided. Shade is limited, primarily found near the picnic sites. Cell phone signal is unreliable within the park boundaries.

Best Time to Visit

The best time for hiking and photography is during late morning or early afternoon when sunlight illuminates the arch. The months of May through October offer the most favorable weather conditions, with minimal snow cover. The creek's water level is typically highest in late spring.

Facts & Legends

Local folklore suggests the natural arch was formed by a giant's hammer. Geologically, the arch is a remnant of a larger cave system that has eroded over time.