Rocks and mountains change very slowly, but they do change. As soon as a rocky mass is pushed upward, forces of erosion slowly begin to level it again. Wind and rain wear it away, grain by grain. Freezing water expands, enlarging small cracks until the rocks begin to crumble.
Lichens are often the first organisms to colonize the rocks. The dead lichens combined with dust from the air to become soil for mosses and small plants. As plant roots fill the cracks, the rocks break apart and the formation of soil continues. Decomposing plants add a fertile top layer to the soil. Burrowing mammals and insects mix and loosen the soil, which increases the amount of water available to plants.
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Itineraries across USA
Acadia
Arches National Park
Badlands
Big Bend
Biscayne
Black Canyon Of The Gunnison
Bryce Canyon
Canyonlands
Capitol Reef
Carlsbad Caverns
Channel Islands
Congaree
Crater Lake
Cuyahoga Valley
Death Valley
Dry Tortugas
Everglades
Gateway Arch
Glacier
Grand Canyon
Grand Teton
Great Basin
Great Smoky Mountains
Guadalupe Mountains
Haleakalā
Hawaiʻi Volcanoes
Hot Springs
Indiana Dunes
Isle Royale
Joshua Tree
Kenai Fjords
Kobuk Valley
Lassen Volcanic
Mammoth Cave
Mesa Verde
Mount Rainier
North Cascades
Olympic
Petrified Forest
Pinnacles
Rocky Mountain
Saguaro
Shenandoah
Theodore Roosevelt
Virgin Islands
Voyageurs
White Sands
Wind Cave
Yellowstone
Yosemite
Zion