A desert is a landscape or region that receives very little precipitation, typically less than 250 millimeters (10 inches) per year. Deserts can be found on every continent and cover about one-fifth of the Earth'slandsurface. They are characterized by arid conditions, extreme temperatures, and sparse vegetation.
Types of Deserts
There are four main types of deserts:
Hot and Dry Deserts: These deserts have high temperatures and very low humidity. Examples include the Sahara Desert in Africa and the Arabian Desert in the Middle East.
Semiarid Deserts: These deserts have slightly more moisture than hot and dry deserts, but still experience long dry seasons. The Chihuahuan Desert in North America is an example of a semiarid desert.
Coastal Deserts: Found along the coasts of continents, these deserts have moderate temperatures and low precipitation. The Atacama Desert in South America is a coastal desert.
Cold Deserts: These deserts have low temperatures and can experience snowfall. The Gobi Desert in Asia is a cold desert.
Earth/Space Science: Students will use scientific skills and processes to explain the chemical and physical interactions (i.e., natural forces and cycles, transfer of energy) of the environment, Earth, and the universe that occur over time.
Earth History: Explain how sedimentary rock is formed periodically, embedding plant and animal remains and leaving a record of the sequence in which the plants and animals appeared and disappeared.
Explain how sedimentary rock buried deep enough may be reformed by pressure and heat and these reformed rock layers may be forced up again to become land surface and even mountains.
Explain why some fossils found in the top layers of sedimentary rock are older then those found beneath in lower layers: Folding; Breaking; Uplift; Faulting; Tilting.