Gallo Spring serves as a vital hydrological marker in this high-desert landscape of Lincoln County, where seasonal water flow and drainage patterns are defined by the Cola del Gallo Arroyo. The terrain is characterized by a series of deeply incised canyons including Taylor Canyon, Miner Canyon, and Hodge Canyon, which provide natural corridors through the varied elevations. High points such as Rattlesnake Hill and Round Top overlook the complex system of draws that eventually converge toward Gallo Spring Canyon and Gallo Canyon. This survey illustrates how the physical geography—marked by names like Mesa Canyon and Round Top Canyon—dictates the movement of water and the likely historical placement of seasonal camps or early livestock ranges in the New Mexico interior.
15 named features on this map. Tap any name to fly to it.
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This is the sole edition of this map. No revisions or reprints were ever made.
1954 · Fort Sumner
USGS Topo · 1:250,000
1958 · Fort Sumner
USGS Topo · 1:250,000
1980 · Corona
USGS Topo · 1:100,000
1981 · Gallo Spring Canyon
USGS Topo · 1:24,000
1981 · Camaleon Draw West
USGS Topo · 1:24,000
1981 · Camaleon Draw East
USGS Topo · 1:24,000
1981 · Pelon Hill
USGS Topo · 1:24,000
1981 · Red Bluff Draw East
USGS Topo · 1:24,000
1981 · Corona South
USGS Topo · 1:24,000
1981 · Gallo Spring Canyon NE
USGS Topo · 1:24,000