The terrain of Palo Pinto County, Texas, is defined by an intricate network of waterways draining the northern reaches of the region. Board Timber Cr and Board Tree Cr flow through the eastern portion of the quadrangle, while the western side is marked by the winding path of Filibuster Cr. These small branches and creeks suggest a landscape historically shaped by seasonal water flow and cattle ranching, with the topography guiding the placement of local roads and land boundaries. Smaller tributaries such as Coon Br and McCumber Br feed into larger systems like Rock Cr, illustrating the natural drainage patterns that have influenced settlement and transportation in this part of north-central Texas. Further south, Pinnington Cr continues this pattern, providing a detailed look at the local hydrography at the end of the second decade of the 21st century.
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This is the sole edition of this map. No revisions or reprints were ever made.
1890 · Breckenridge
USGS Topo · 1:125,000
1891 · Palo Pinto
USGS Topo · 1:125,000
1918 · Palo Pinto
USGS Topo · 1:125,000
1924 · Breckenridge 1-a
USGS Topo · 1:48,000
1924 · Palo Pinto 2-b
USGS Topo · 1:48,000
1924 · Palo Pinto 2-a
USGS Topo · 1:48,000
1924 · Graham 4-d
USGS Topo · 1:48,000
1927 · Graham
USGS Topo · 1:62,500
1927 · Pickwick
USGS Topo · 1:62,500
1931 · Ivan
USGS Topo · 1:62,500