Hot and Dry Deserts: These deserts have high temperatures during the day and low temperatures at night. Examples include the Sahara Desert in Africa and the Arabian Desert in the Middle East.
Cold Deserts: These deserts experience cold winters and may receive some snowfall. Examples include the Gobi Desert in Asia and the Patagonian Desert in South America.
Coastal Deserts: These deserts are located near coastal areas and are influenced by cold ocean currents. Examples include the Atacama Desert in Chile and the Namib Desert in Namibia.
Semiarid Deserts: These deserts have slightly more precipitation than other types of deserts, but still experience long dry periods. Examples include the Great Basin Desert in the United States and the Karoo Desert in South Africa.
Deserts are unique and diverse ecosystems that are home to a wide variety of plants and animals. Understanding the adaptations of desert organisms and the impact of human activities on desert environments is crucial for the conservation and preservation of these fragile ecosystems.
The student demonstrates an understanding of geochemical cycles by describing that most smaller rocks come from the breaking and weathering of larger rocks as part of the rock cycle.
The student demonstrates an understanding of geochemical cycles by recognizing the physical properties of water as they relate to the rock cycle.