
Hood Spring serves as a vital water source in this arid stretch of Brewster County, where the topography is defined by significant elevation changes and seasonal drainage systems. The landscape is carved by prominent corridors such as Bacon Draw, which cut through the high ground towards the intermittent flows of Indian Cr and San Francisco Cr to the north and east. The concentration of water features in the central portion of the sheet, including Kincaid Spring and its associated Kincaid Creek, indicates a historical reliance on these specific points for ranching and survival in the Chihuahuan Desert. This 2022 survey illustrates the enduring importance of isolated springs in a terrain where natural landmarks like Kincaid Creek dictate the movement of both wildlife and humans.
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1917 · Hood Spring
USGS Topo · 1:62,500
1918 · Bone Spring
USGS Topo · 1:125,000
1918 · Hood Spring
USGS Topo · 1:62,500
1918 · Dove Mountain
USGS Topo · 1:62,500
1920 · Longfellow
USGS Topo · 1:125,000
1920 · Marathon
USGS Topo · 1:62,500
1921 · Marathon
USGS Topo · 1:62,500
1931 · Hood Spring
USGS Topo · 1:62,500
1954 · Fort Stockton
USGS Topo · 1:250,000
1958 · Fort Stockton
USGS Topo · 1:250,000