
Newberry Crater dominates this volcanic landscape in central Oregon, holding Paulina Lake and East Lake within its distinctive caldera. In the early 1930s, this area was a convergence of natural geologic wonders and industrial expansion. The timber industry is highly visible through the presence of Brooks-Scanlon Camp 2 and Brooks-Scanlon Camp 3, connected by an extensive network of Logging RR lines. Along the Deschutes River, several falls including Lava Island Falls and Benham Falls mark the water's path near the northern border. Cultural landmarks of the era are well-documented, from the Vandevert Sch and Stookey Ranch to the Oregon Trunk Railway corridor. The map also highlights unique subterranean features such as the Lava River Cave and Arnold Ice Cave, which drew early interest to the volcanic terrain of the Paulina Mountains.
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This is the sole edition of this map. No revisions or reprints were ever made.
1926 · Bend
USGS Topo · 1:125,000
1929 · Bend
USGS Topo · 1:125,000
1929 · Three Sisters
USGS Topo · 1:125,000
1930 · Maiden Peak
USGS Topo · 1:125,000
1932 · Three Sisters
USGS Topo · 1:125,000
1934 · Maiden Peak
USGS Topo · 1:125,000
1935 · Chemult
USGS Topo · 1:96,000
1935 · Newberry Crater
USGS Topo · 1:125,000
1941 · Chemult
USGS Topo · 1:125,000
1955 · Crescent
USGS Topo · 1:250,000