Answer:True
Volcanic mountains
Explanation: volcanic mountains are mountains that arise as a result of non violent movement of molten lava which flows out of fissure to the earth's surface forming volcanic mountains over time after cooling. The point from where the dusts,volcanic materials (lava) are released from is known as the VENT. Volcanic mountains are different from other kinds of mountains due to their non violent movement that led to their formation.
Answer:
Hanging valleys or U-shaped valleys are some of the landforms formed by the depositional work of the glaciers .
Answer:
The correct response is Option C: "High Grasslands."
Explanation:
Kenya has produced some of the world's top distance runners because of the unique features of its terrain. The country is characterized by vast stretches of high grasslands like those in the Great Rift Valley where the land is flat and the weather is mild year-round. This encourages outdoor running on a regular basis. Researcher Bruce Hamilton has also noted that social variables are important for Kenyan runners. He states that years of running to and from school has helped them develop this talent and propensity for running. Most children and adolescents of modest means have to run long distances to and from school and it can partly explain why Kenyan children develop a great capacity and endurance for running.
In 2011, a major earthquake and tsunami destroyed much of the capital infrastructure in japan. those natural disasters were examples of negative shocks to the long-run aggregate supply curve.
Lifeline infrastructure such as electricity, water, sewage, and gas was also damaged. Such services were quickly restored in most of the affected areas, but at the time of writing, the most affected coastal areas of Tohoku Japan still lack such services.
The Tohoku tsunami produced waves up to 40 meters high. The tsunami left him homeless over 450,000 people. Over 15,500 people died. The tsunami also severely paralyzed the country's capital infrastructure.
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Aeolian processes are effective wherever fine-grained unconsolidated sedimentary material is exposed to the atmosphere without protection