
Mowich Spring emerges as a key water source in this high-altitude landscape within the Lake county region, situated in a terrain defined by volcanic features. The 2023 data highlights the administrative divisions between the Fremont National Forest and the Deschutes National Forest, where the land is carved by significant topographic depressions and cinder cones. While the area lacks dense residential settlements, the intricate network of forest roads and the presence of summits like Summit Butte, Big Hole Butte, and Katati Butte reveal a landscape managed for timber, grazing, and public recreation. The distinctive geological formation of the Big Hole itself dominates the central topography, offering a clear record of the volcanic activity that shaped this portion of the Oregon backcountry.
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1931 · Newberry Crater
USGS Topo · 1:125,000
1935 · Newberry Crater
USGS Topo · 1:125,000
1955 · Crescent
USGS Topo · 1:250,000
1957 · Crescent
USGS Topo · 1:250,000
1958 · Crescent
USGS Topo · 1:250,000
1963 · Spring Butte
USGS Topo · 1:24,000
1963 · Moffitt Butte
USGS Topo · 1:24,000
1970 · Crescent
USGS Topo · 1:250,000
1979 · Crescent
USGS Topo · 1:100,000
1981 · Wickiup Spring
USGS Topo · 1:24,000