Warm Up 4/11 How did early Texans adapt to their physical environment and how have modern Texans changed the environment to meet their needs?

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Presentation transcript:

Warm Up 4/11 How did early Texans adapt to their physical environment and how have modern Texans changed the environment to meet their needs?

Learning Target: We will examine  effects of the interaction between humans and the environment in Texas during the 19th, 20th, and 21st centuries. Language Target: We will explain ways in which geographic factors such as the Galveston Hurricane of 1900, the Dust Bowl, limited water resources, and alternative energy sources have affected. Success Criteria: I will analyze multiple OPTICS of the natural disasters that hit TX

Galveston Hurricane of 1900 On September 8, 1900, a Category 4 hurricane ripped through Galveston, Texas, killing an estimated 6,000 to 8,000 people. At the time of the 1900 hurricane, Galveston, nicknamed the Oleander City, was filled with vacationers. Sophisticated weather forecasting technology didn’t exist at the time, but the U.S. Weather Bureau issued warnings telling people to move to higher ground. 

Galveston Hurricane of 1900 However, these advisories were ignored by many vacationers and residents alike. A 15-foot storm surge flooded the city, which was then situated at less than 9 feet above sea level, and numerous homes and buildings were destroyed. The hurricane remains the worst weather- related disaster in U.S. history in terms of loss of life.

Galveston Hurricane of 1900 After the hurricane, a large seawall was eventually built to protect Galveston from flooding. The city was pummeled again by major hurricanes in 1961 and 1983, but they caused less damage than the one that struck in 1900.

Galveston Hurricane of 1900

The Dust Bowl The Dust Bowl was the name given to the Great Plains region devastated by drought in 1930s depression-ridden America. The 150,000-square- mile area, encompassing the Oklahoma and Texas panhandles and neighboring sections of Kansas, Colorado, and New Mexico, has little rainfall, light soil, and high winds, a potentially destructive combination.

The Dust Bowl When drought struck from 1934 to 1937, the soil lacked the stronger root system of grass as an anchor, so the winds easily picked up the loose topsoil and swirled it into dense dust clouds, called “black blizzards.” Recurrent dust storms wreaked havoc, choking cattle and pasture lands and driving 60 percent of the population from the region. Most of these “exodusters” went to agricultural areas first and then to cities, especially in the Far West.

The Dust Bowl