Located approximately 6 miles (10 km) north of Burney, California, McArthur–Burney Falls Memorial State Park is the second oldest state park in the California State Parks System. The park offers camping, fishing, watersports, hiking and horseback riding facilities. The park is mainly known for the waterfall, Burney Falls, at the entrance of the park. Wildlife in the park, as far as most campers see, consists mainly of many types of bass and trout in the streams, and land animals such as Steller's Jays, squirrels, woodpeckers, deer, and even the occasional black bear will meander into campgrounds.
The park is within the Cascade Range and Modoc Plateau natural region, with 910 acres (4 km²) of forest and five miles (8 km) of streamside and lake shoreline, including a portion of Lake Britton.
The park's centerpiece is the 129 foot (39 m) Burney Falls, which is not the highest or largest waterfall in the state, but arguably the most beautiful. Additional water comes from springs, joining to create a mist-filled basin. Burney Creek originates from the park's underground springs and flows to Lake Britton, getting larger along the way to the falls.
The park's landscape was created by volcanic activity as well as erosion from weather and streams. This volcanic region is surrounded by mountain peaks and is covered by black volcanic rock, or basalt. Created over a million years ago, the layered, porous basalt retains rainwater and snow melt, which forms a large underground reservoir.
Within the park, the water emerges as springs at and above Burney Falls, where it flows at 100 million gallons every day (4.4 m³/s).
The park is within the Cascade Range and Modoc Plateau natural region, with 910 acres (4 km²) of forest and five miles (8 km) of streamside and lake shoreline, including a portion of Lake Britton.
The park's centerpiece is the 129 foot (39 m) Burney Falls, which is not the highest or largest waterfall in the state, but arguably the most beautiful. Additional water comes from springs, joining to create a mist-filled basin. Burney Creek originates from the park's underground springs and flows to Lake Britton, getting larger along the way to the falls.
The park's landscape was created by volcanic activity as well as erosion from weather and streams. This volcanic region is surrounded by mountain peaks and is covered by black volcanic rock, or basalt. Created over a million years ago, the layered, porous basalt retains rainwater and snow melt, which forms a large underground reservoir.
Within the park, the water emerges as springs at and above Burney Falls, where it flows at 100 million gallons every day (4.4 m³/s).
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