Answer:
Rainshadow effect -
Explanation:
Rainshadow effect -
it is phenomenon when air parcel passes over ranges of mountain, it pass down the other side of mountain and get warms and dries out. The resultant dry air produces a rain shadow. The area on the rain shadow are typically warm and obtain very less rainfall and very less cloud cover. while on the other side i.e windward side of range of mountain receive heavy rainfall and cloud cover
The majority of neandertal fossils been found in <u>Europe </u>where they have been most studied.
More about the neandertals:
The Neanderthals have undergone extensive evolutionary change. Around 430,000 years have passed since the earliest fossils that resemble Neanderthals were discovered. The earliest Neanderthals are thought to have existed between 130,000 and 40,000 years ago, beyond which no physical proof of them can be found.
In contrast to modern humans, who have a more globular skull, Neanderthals had a long, low head with a distinctively noticeable brow ridge above their eyes.
Their face also stood out. A very large, wide nose dominated the forward-protruding middle portion of the face. They would have breathed in warm, moist air thanks to the high internal volume of their noses. The size of their front teeth and the scratch scars on them indicate that they were frequently employed as a third hand when preparing food and other materials.
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Limestone. limestone is the youngest.
Glaciers deposit their sediment when they melt. They drop and leave behind whatever was once frozen in their ice. It’s usually a mixture of particles and rocks of all sizes, called glacial till. Water from the melting ice may form lakes or other water features. Moraine is sediment deposited by a glacier. A ground moraine is a thick layer of sediments left behind by a retreating glacier. An end moraine is a low ridge of sediments deposited at the end of the glacier. It marks the greatest distance the glacier advanced.
A drumlin is a long, low hill of sediments deposited by a glacier. Drumlins often occur in groups called drumlin fields. The narrow end of each drumlin points in the direction the glacier was moving when it dropped the sediments.
An esker is a winding ridge of sand deposited by a stream of meltwater. Such streams flow underneath a retreating glacier.
A kettle lake occurs where a chunk of ice was left behind in the sediments of a retreating glacier. When the ice melted, it leaves a depression. Hope this helps ;)
