Chronology Texas is the second-largest U.S state after Alaska with an area of 268,820 square miles (696,200 km2) Though 10% larger than France and almost twice as large as Germany or Japan it ranks only 27th worldwide amongst country subdivisions by size If it were an independent country Texas would be the 40th largest behind Chile and Zambia, Houston Texas Business Directory, vte 1910 115,693 81.4% The German Reichstag after its capture by the Allied forces 3 June 1945. .
. Houston Texas Business Directory Houston Texas Business Directory 4.3 Texas Legislature Though Houston is the largest city in the United States without formal zoning regulations it has developed similarly to other Sun Belt cities because the city's land use regulations and legal covenants have played a similar role. Regulations include mandatory lot size for single-family houses and requirements that parking be available to tenants and customers Such restrictions have had mixed results Though some have blamed the city's low density urban sprawl and lack of pedestrian-friendliness on these policies the city's land use has also been credited with having significant affordable housing sparing Houston the worst effects of the 2008 real estate crisis the city issued 42,697 building permits in 2008 and was ranked first in the list of healthiest housing markets for 2009. . 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). These soils were deposited by tributaries of local waterways particularly the Brazos and Trinity rivers. There is a considerable contrast in soil composition to the north around Cypress Creek; most of the surface there consists of tan-colored sand with small amounts of gray clay the north and northwestern regions of Houston and Harris County feature a slightly steeper slope than other parts of the city with occasional escarpments caused by faulting or erosion.
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