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The land surface in and around the city of Houston is composed of alternating layers of red, gray, sandy brown, and black organic clay; these strata generally dip to the southeast at a slope of 0.06% (3 feet (0.91 m) of vertical change for every 1 mile (1.6 km) of distance traveled). [6]
The Houston Ship Channel, in Houston, Texas, is part of the Port of Houston, one of the busiest seaports in the world. [1] The channel is the conduit for ocean-going vessels between Houston-area terminals and the Gulf of Mexico , and it serves an increasing volume of inland barge traffic.
Hurricane Ike in September 2008, forever changed the topography of the beach. What was once a driveway and public beach access is now part of the Gulf of Mexico. The land where the bait house of the pier once stood is now permanently submerged. San Luis Pass on the Galveston side is a place for bird watching. [11]
The Greater Houston region is generally earthquake-free. While the city of Houston contains over 150 to 300 active surface faults with an aggregate length of up to 310 miles (500 km), [24] [25] [26] the clay below the surface precludes the buildup of friction that produces ground-shaking in earthquakes. These faults generally move at a smooth ...
With a maximum depth of about 10 feet (3 m) and an average depth of only 6 feet (2 m), it is unusually shallow for its size. The bay has played a significant role in the history of Texas . Galveston Island is home to the city of Galveston , the earliest major settlement in southeast Texas and the state's largest city toward the end of the ...
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Barker Reservoir is a flood control structure in Houston, Texas which prevents downstream flooding of Buffalo Bayou, the city's principal river.The reservoir operates in conjunction with Addicks Reservoir to the northeast, which impounds Mayde and Bear Creeks, two tributaries of the Buffalo.
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