Palo Pinto serves as the primary hub of this landscape, situated south of the serpentining path of the Brazos River. This stretch of the river is defined by its deep, dramatic curves, including Dalton Bend, Chick Bend, and Crawford Bend, which carve through the elevated terrain of the Brazos River Valley. Higher elevations are marked by prominent peaks such as Schoolhouse Mountain and Kyle Mountain, indicating a geography of significant relief and varied drainage patterns.
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1891 · Palo Pinto
USGS Topo · 1:125,000
1918 · Palo Pinto
USGS Topo · 1:125,000
1924 · Palo Pinto 2-b
USGS Topo · 1:48,000
1924 · Palo Pinto 2-a
USGS Topo · 1:48,000
1924 · Palo Pinto 1-b
USGS Topo · 1:48,000
1924 · Palo Pinto 2-c
USGS Topo · 1:48,000
1925 · Palo Pinto 4-b
USGS Topo · 1:48,000
1927 · Pickwick
USGS Topo · 1:62,500
1927 · Mineral Wells
USGS Topo · 1:62,500
1931 · Santo
USGS Topo · 1:62,500