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The Guadalupe Hotel is a historic hotel in downtown New Braunfels, Texas. It is located on the Main Plaza, adjacent from the Comal County Courthouse . See also
The Comal River (/ ˈ k oʊ m æ l / KOH-mal) is the shortest navigable river in the state of Texas in the United States. Proclaimed the "longest shortest river in the world" by locals, it runs entirely within the city limits of New Braunfels in southeast Comal County. It is a tributary of the Guadalupe River.
March 24, 2008 (290 W. San Antonio: New Braunfels: 4: Andreas Breustedt House: Andreas Breustedt House: July 22, 1982 (1370 Church Hill Dr. New Braunfels: Recorded Texas Historic Landmark
Its county seat is New Braunfels. [5] Comal County is part of the San Antonio-New Braunfels, TX metropolitan statistical area. Along with Hays and Kendall Counties, Comal was listed in 2017 of the nation's 10 fastest-growing large counties with a population of at least 10,000. In 2017, Comal County was second on the list; it grew by 5,675 ...
Spring Branch is located in western Comal County along U.S. Highway 281, north of Bulverde, west of Canyon Lake and the surrounding unincorporated community of the same name. New Braunfels is approximately 21 miles (34 km) southeast of Spring Branch. The city covers 1.9 square miles, all land.
The Comal Power Plant was originally a lignite (brown coal) power generating facility, built starting in 1925, in New Braunfels, Comal County, Texas. [2] It was decommissioned in the 1970s, and was listed on the National Register of Historic Places in 2004. [1] It has since been converted to The Landmark Lofts apartments. [3]
Lake Dunlap is a reservoir on the Guadalupe River near the town of New Braunfels in Guadalupe County, Texas, United States. The reservoir was formed in 1931 by the construction of a dam to provide hydroelectric power to the area. Management of the dam and lake was assumed by the Guadalupe-Blanco River Authority on May 1, 1963. Lake Dunlap ...
The Comal Springs are fed by the Edwards Aquifer, a large karst aquifer that runs through most of central Texas. The aquifer consists of porous, water-bearing limestone features which channel rainfall and surface runoff from the aquifer's recharge zone down to various discharge zones, including the springs.
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