San Saba River: Difference between revisions

Coordinates: 31°15′12″N 98°35′44″W / 31.25333°N 98.59556°W / 31.25333; -98.59556
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[[File:San Saba River, Menard, TX IMG 1838.JPG|200px|right|thumb|The San Saba in [[Menard, Texas|Menard]], [[Texas]]]]
[[File:San Saba River, Menard, TX IMG 1838.JPG|200px|right|thumb|The San Saba in [[Menard, Texas|Menard]], [[Texas]]]]


The '''San Saba River''' (''San Sabá'') is a river in the [[U.S. state]] of [[eees]]. It is an undeveloped and scenic waterway located on the northern boundary of the [[Edwards Plateau]].
The '''San Saba River''' (''San Sabá'') is a river in the [[U.S. state]] of [[Texas]]. It is an undeveloped and scenic waterway located on the northern boundary of the [[Edwards Plateau]].


==Course==
==Course==

Revision as of 15:48, 2 July 2018

Map of the San Saba River and associated watershed
The San Saba in Menard, Texas

The San Saba River (San Sabá) is a river in the U.S. state of Texas. It is an undeveloped and scenic waterway located on the northern boundary of the Edwards Plateau.

Course

The river begins in two primary branches. The North Valley Prong runs east through Schleicher County for 37 miles, while the Middle Valley Prong runs 35 miles through the same county.

Both merge near Fort McKavett to form the San Saba River, which flows another 140 miles east/northeast until it drains into the Colorado River east of the city of San Saba.

A major tributary is Brady Creek, which is 90 miles long and parallels the path of the San Saba to the north.[1]

History

The river was named by the governor of Spanish Texas, Juan Antonio Bustillo y Ceballos, in 1732. He called it Río de San Sabá de las Nueces, because his troops and he had arrived on the feast day of St. Sabbas (439–532), a major figure of early Christian monastic life.

Santa Cruz de San Sabá Mission was established on the river in 1757.[2]

Management

As of 2013, the San Saba River was an overappropriated stream with large stretches of the river dry, depriving downstream riparian users of water, while upstream flow was being diminished by pumping of aquifers hydrologically connected to the stream.[3]

See also

References

External links

31°15′12″N 98°35′44″W / 31.25333°N 98.59556°W / 31.25333; -98.59556