Planet Earth

Planet Earth — page 9
s th a Building E a r L Giant What makes mountains Several different processes n s c apes EA R C H LIG S contribute to mountain building And most mountains are formed by a combination of these usually over millions of years d H T Deep inside the Earth is so incredibly hot that everything is melted or molten This molten material or lava escapes to the Earth’s surface when volcanoes erupt The lava cools and becomes hard and solid This happens again and again collecting until there is a volcanic mountain Mount Fuji in Japan and Mount St Helens in Mountains are made when a volcanoes erupt b earthquakes happen c the Earth pushes together d all of the above Washington state U S are volcanic mountains There are also many undersea volcanic mountains much taller than anything on land In some cases strong earthquakes caused the surface rock for miles and miles to break Part of the surface would then be lower and part of it higher More earthquakes moved the lower parts down and the upper parts up Eventually the high parts became tall enough to make mountains Still other mountains were pushed up from the bottom of an ocean when two enormous portions of the Earth crashed together very slowly over millions and millions of years Some of the largest mountain chains formed this way The Andes of South America are an example Another mountain-building process is called folding If you push a carpet up against a wall it folds and rumples That’s basically the way the Appalachian Mountains in eastern North America were formed At first most mountains were steep and sharp But even hard rocks can be worn away Slowly with the wind and the rain rubbing at them steep sharp mountains grow smoother shorter and rounder LEARN MORE READ THESE ARTICLES CAVES ISLANDS OCEANS DID YOU KNOW To be considered a mountain the land must rise at least 2,000 feet above its surroundings Mount Everest the world’s highest mountain rises 29,035 feet above sea level 12 D a v i d M u e n c h C o r b s i