PHYSIOGRAPHIC REGIONS OF THE LOWER 48 UNITED STATES

LAURENTIAN UPLAND

  1. Superior Upland

ATLANTIC PLAIN

  1. Continental Shelf (not on map)
  2. Coastal Plain
  3. Embayed section
  4. SeaIsland section
  5. Floridian section
  6. EastGulf Coastal Plain
  7. Mississippi Alluvial Plain
  8. WestGulf Coastal Plain

APPALACHIAN HIGHLANDS

  1. Piedmont province
  2. Piedmont Upland
  3. Piedmont Lowlands
  4. Blue Ridge province
  5. Northern section
  6. Southern section
  7. Valley and Ridge province
  8. Tennessee section
  9. Middle section
  10. HudsonValley
  11. St. Lawrence Valley
  12. Champlain section
  13. Northern section (not on map)
  14. Appalachian Plateaus province
  15. Mohawk section
  16. Catskill section
  17. Southern New York section
  18. AlleghenyMountain section
  19. Kanawha section
  20. Cumberland Plateau section
  21. CumberlandMountain section
  22. New EnglandProvince
  23. Seaboard Lowland section
  24. New England Upland section
  25. White Mountain section
  26. GreenMountain section
  27. Taconic section
  28. Adirondack province

INTERIOR PLAINS
  1. Interior Low Plateaus
  2. Highland Rim section
  3. Lexington Plain
  4. NashvilleBasin
  5. Central Lowland
  6. EasternLake section
  7. WesternLake section
  8. Wisconsin Driftless section
  9. Till Plains
  10. Dissected Till Plains
  11. Osage Plains
  12. Great Plains province
  13. Missouri Plateau, glaciated
  14. Missouri Plateau, unglaciated
  15. Black Hills
  16. High Plains
  17. Plains Border
  18. ColoradoPiedmont
  19. Raton section
  20. PecosValley
  21. EdwardsPlateau
  22. Central Texas section

INTERIOR HIGHLANDS

  1. Ozark Plateaus
  2. Springfield-Salem plateaus
  3. Boston"Mountains"
  4. Ouachita province
  5. ArkansasValley
  6. Ouachita Mountains

ROCKY MOUNTAIN SYSTEM

  1. Southern Rocky Mountains
  2. WyomingBasin
  3. Middle Rocky Mountains
  4. Northern Rocky Mountains

INTERMONTANE PLATEAUS

  1. Columbia Plateau
  2. Walla Walla Plateau
  3. BlueMountain section
  4. Payette section
  5. Snake River Plain
  6. Harney section
  7. Colorado Plateaus
  8. High Plateaus of Utah
  9. UintaBasin
  10. Canyon Lands
  11. Navajo section
  12. Grand Canyon section
  13. Datil section
  14. Basin and Range province
  15. Great Basin
  16. SonoranDesert
  17. Salton Trough
  18. Mexican Highland
  19. Sacramento section

PACIFIC MOUNTAIN SYSTEM

  1. Cascade-SierraMountains
  2. Northern Cascade Mountains
  3. Middle Cascade Mountains
  4. Southern Cascade Mountains
  5. Sierra Nevada
  6. Pacific Border province
  7. Puget Trough
  8. Olympic Mountains
  9. OregonCoastRange
  10. KlamathMountains
  11. California Trough
  12. CaliforniaCoast Ranges
  13. Los AngelesRanges
  14. Lower California province

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A Tapestry of Time and Terrain:
The Union of Two Maps - Geology and Topography

Rocks of Ages:
An explanation of the legend

Geologists subdivide time variously by eras (Precambrian to Cenozoic), periods (Cambrian to Quaternary), and epochs - only Pleistocene (early Quaternary) and Holocene (late Quaternary) are used here (see column at left). These units are quite uneven in elapsed time, the older intervals generally being of much longer duration. Rocks in the U.S. range in age from early Precambrian (2.6 billion years ago) to Holocene, which includes the present. The orderly sequence of Earth materials, from oldest to youngest, is represented by an equally well-ordered sequence of "prismatic" colors (based on the rainbow). To improve the color balance of the tapestry, the Holocene is represented by two hues, light gray in the East and beige in the West.

The King and Beikman geologic map of the U.S. was compiled from many detailed maps that describe the rocks of smaller areas. The constituent maps were made by many individuals from field and laboratory observations. These geologic maps distinguish among types of rocks that form in different ways: igneous granite and basalt; sedimentary sandstone, shale, and limestone; and metamorphic slate, marble, gneiss, and schist. From several converging lines of evidence - fossils, the layered sequence of strata, and the systematic radioactive decay of certain minerals - geologists have been able to place the rock formations in their correct time order, and from that arrangement construct a sequence of likely geologic events.