Alabama: Sand to Cedars

This area of the museum shows the Geologic regions of Alabama.



 
 
Highland Rim
These rocks make up the second oldest in the state.  The rock types are mostly limestone and chert.  This area is referred to as a cedar glade.  A glade is made of flat limestone outcroppings and shallow soils that are interspersed with islands of cedar trees and other hardwoods. 
Cumberland Plateau
This is an upland region  that is best known as Alabama's coal mining region.  The rocks are Paleozoic in age.  It is the westernmost extension of the Appalachian Highlands and the elevation in this area ranges from 500 to 1900 feet.   The steep canyons found in this region provide a cooler habitat that allows for trees that usually are found more northward to grow here.  Some examples are eastern hemlock and sweet birch. 
Valley and Ridge
This is an area of folded and fractured rocks.  The folding exposes many rock layers that would typically lie far beneath the earth surface. Oak, hickory and pine are the most common type of trees in this area.   Major rocks in the area include , dolomite, shale, siltstone, sandstone, chert, mudstone and marble. Karst limestone and fractured rock aquifers are found in this area.  The cougar was the largest predator  prior to 1940.  It needed 35 deer each year to survive.  The cougar is no larger found in Alabama.  The deer population is controlled by humans.
Piedmont
The oldest rocks at the surface are found in this region.  Many of the exposed rocks are igneous and metamorphic therefore fossils in this area are not common. Cheaha Mountain with an elevation of 2,407 feet is the highest point in Alabama.  The fall line separates the Piedmont from the coastal plain.  Alabama has more mussel species than any other state.  Because mussels are filter feeders and sensitive to pollution they are good water quality indicators.  Currently 71% of the 300 species of mussels are now extinct.  Why is this so?
Coastal Plain
The is the area south of the fall line.  The region is made up mostly of sand and clays.   The upper coastal plain also includes an arc shaped area called the black belt.  This area is underlain with chalk.   The coastal plain is the youngest area of the state.   The most south east portion of the coastal plain it made up of an exotic rock types called the Suwannee Terrane.  It is thought to be part of Africa that was sutured on during the collision that made Pangaea.

Back to Anniston