No, rainshadow deserts are on the leeward side of mountains.
Yes, they are called rainshadow deserts because the mountains prevent atmospheric moisture from coming into the desert.
Mountains block moisture from crossing into the leeward side, forcing most rain to fall on the windward side of the mountain. The leeward side is considered as a desert.
Deserts often form on the leeward side of a mountain.
There are no deserts in West Virginia.
The Andes block moisture from the Atlantic Ocean and Amazon basin from reaching the west coast areas of South America, resulting in the formation of rainshadow deserts such as the Atacama and Sechura.
Mountains can block the flow of atmospheric moisture causing rain to fall on the windward side of the mountains. The leeward side is left dray forming a rain shadow desert. See the image above.
Many deserts are rain shadow deserts. Mountain ranges block the flow of moisture from the ocean and cause it to fall on the windward side. The dry air then passes over the mountains to the leeward side and there is no moisture left so a rain shadow desert forms. See the diagram above,
Mountains in deserts are called . . . . . . . . mountains!
The mountains act as a barrier to atmospheric moisture from crossin the mountain to the leeward side. The rain falls instead on the windward side forming a rain shadow desert on the leeward side of the mountains.
No, not all deserts are surrounded by deserts.
Yes, Brazil has mountainous regions, such as the Serra do Mar and Serra da Mantiqueira. However, Brazil does not have deserts; its landscape is mostly covered by rainforests, savannas, and wetlands.
There are really three mountain/hill groups in the Middle East that have a strong effect.1) The Judean Hills, the Mount Lebanon Range, and the Anti-Lebanon Mountains form a long line of mountains that are somewhat inland from the Mediterranean coast. The windward sides of these mountains are along the Mediterranean, creating more fertile regions in northern Israel and Lebanon between the mountains and the Mediterranean. These ranges also create a rainshadow for southern Israel, much of Jordan and a large portion of Syria. This is why those areas are mostly deserts, save for river irrigation.2) The Elburz and Zagros Mountains create a large internal rainshadow in Iran, which is called the Dasht-i-Lut and is one of the most lifeless areas on Earth. However, along these mountain ranges are relatively fertile regions, including where Tehran, the capital of Iran, sits.3) Sarawat Mountains run along the southwestern edge of the Arabian Peninsula, extending along the Saudi and Yemeni coast of the Red Sea. These mountains create a very minimal windward side, which in Yemen hosts the majority of that country's agriculture and population. Far more extensive is the rainshadowed Arabian desert, which dominates most of the rest of the peninsula.