Metcalf Gap serves as a critical passage through the Palo Pinto Mountains in this central Texas landscape. The terrain is defined by dramatic elevation changes, where prominent summits like Sugarloaf Mtn and Antelope Mtn overlook a complex network of seasonal drainages. Waterways such as Little Joni Cr and Eagle Cr carve through the limestone-rich topography, eventually feeding into Hodgkins Lake or winding through corridors like Brushy Hollow.
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1890 · Breckenridge
USGS Topo · 1:125,000
1891 · Palo Pinto
USGS Topo · 1:125,000
1918 · Palo Pinto
USGS Topo · 1:125,000
1924 · Palo Pinto 2-c
USGS Topo · 1:48,000
1924 · Breckenridge 1-d
USGS Topo · 1:48,000
1927 · Pickwick
USGS Topo · 1:62,500
1931 · Ivan
USGS Topo · 1:62,500
1954 · Abilene
USGS Topo · 1:250,000
1958 · Abilene
USGS Topo · 1:250,000
1958 · Palo Pinto
USGS Topo · 1:62,500