Duffy's Peak
Duffy's Peak is located in the rolling plains to the south and east of the Caprock Escarpment of the Llano Estacado. The soils of the area are moderately deep silt loams that support mesquite, yucca, cacti, and grasses. The local terrain is eroded, cut by highly intermittent streams such as the Salt Fork Brazos River, and its tributaries, such as McDonald Creek and Lake Creek. These streams typically flow only during periods of heavy rainfall, when flash floods sweep through the area. The erosionally resistant sandstones of the peak's cap have protected underlying soils that have remained intact, while surrounding sediments have eroded away. As a result of this process, Duffy's Peak now stands out as a small but relatively prominent landmark that can be seen from a significant distance.
In 1969, the Texas Historical Commission erected a historical marker for Duffy's Peak along Texas State Highway 207.
See also
References
- ^ Anonymous. "Duffy's Peak". Handbook of Texas Online. Retrieved November 2, 2012.
- ^ United States Department of Agriculture, Soil Conservation Service (1975). "Soil Survey of Garza County, Texas" (PDF).
- ^ Anonymous. "Duffy's Peak - Post, Garza County, Texas". StoppingPoints. Retrieved September 14, 2017.