The Appalachians are older than the Alps. The Appalachians were created many eras ago when North America crashed into Europe. Then the Appalachians were split apart when the Atlantic Ocean opened up. The Mid Atlantic ridge and other phenomena split them into The Mountains of Norway and Sweden, The Highlands of Scotland, The Appalachians of North America, and the Ouchita Mountains of Arkansas, Oklahoma, and Texas. The Alps were pushed up when Italy moved up and Crashed into Europe. That happened only a few Million years ago.
The Appalachian Mountains are older than the Alps. The Appalachian Mountains are estimated to be around 480 million years old, while the Alps began forming around 80 million years ago.
The Appalachians are older than the Alps. The Appalachians formed around 480 million years ago during the Paleozoic Era, while the Alps began forming around 50 million years ago during the Cenozoic Era.
The Alps, Urals, and Appalachians are examples of fold mountains, which form due to tectonic plate movement and the folding of rock layers over time.
The hilly continent is Europe. Europe is known for its diverse landscapes, including mountain ranges such as the Alps, the Pyrenees, and the Carpathians, which contribute to its hilly terrain.
The Alps are younger than Pangaea. The formation of the Alps began around 30 million years ago during the Tertiary period, while Pangaea existed around 335 to 175 million years ago during the Paleozoic and Mesozoic eras.
A mountainous or hilly section of a country is known as a mountain range or a hill range. It is a series of mountains or hills that are connected geographically and typically run in a specific direction. Examples include the Rocky Mountains in North America and the Alps in Europe.
The Appalachians are older than the Alps. The Appalachians formed around 480 million years ago during the Paleozoic Era, while the Alps began forming around 50 million years ago during the Cenozoic Era.
The Alps, Rockies, Appalachians.
Alps Himalayas Appalachians
The Alps, Urals, and Appalachians are examples of fold mountains, which form due to tectonic plate movement and the folding of rock layers over time.
the alps and Tauern mountainsKatu
flat in the north (near the sea) to mountained in the south (part of the Alps)
The Alps are younger than Pangaea. The formation of the Alps began around 30 million years ago during the Tertiary period, while Pangaea existed around 335 to 175 million years ago during the Paleozoic and Mesozoic eras.
The Appalachians are older than the rocky mountains because of the fact that the Appalachians are smaller in size proving that the Appalachians have had longer to have been worn away by weathering also please do not just copy and paste you will learn nothing...
The Alps have higher peaks and are a larger mountain range. However, the Pyrénées are the same type of rugged, young mountains and also have some high summits.
Continental collision is the geological event that generated many mountain belts.
Continental collision is the geological event that generated many mountain belts.
Some of the major mountain ranges in Italy include the Alps, which run along the northern border with France and Switzerland, and the Apennines, which stretch the length of the Italian peninsula. The Dolomites, located in the northeastern part of the country, are also a famous mountain range known for their distinctive jagged peaks.