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The term "piedmont" means foothills: the Piedmont ecoregion lies at the foot of the Appalachian Mountains, with a topography that ranges from rugged to gently rolling. It is made up of a mosaic...

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Overview of the Georgia Blue Ridge Ecoregion ​ ​Forest and Woodland Communities Northern Hardwoods and Boulderfield Forests Montane Oak Forests ​ Fertile Cove (Mesic) Forests Acidic Cove...

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Rare natural element occurrences (EOs) are plant and animal populations, natural plant communities, bird nesting colonies, caves and other elements in nature that are important for biodiversity conservation.

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Georgia Rare Elements Data Portal. Rare natural element occurrences (EOs) are plant and animal populations, natural plant communities, bird nesting colonies, caves and other elements in nature that are important for biodiversity conservation.

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Georgia Habitats Passages and Activities

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Georgia Habitats Passages and Activities

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Guide to the Natural Communities of Georgia

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Guide to the Natural Communities of Georgia

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Ecoregions of Georgia The Georgia Piedmont Ecoregion is described here. ​ The Georgia Blue Ridge Ecoregion is described here . The Georgia...

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EXPLORING GEORGIA'S WILDLIFE COLORING BOOK

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EXPLORING GEORGIA'S WILDLIFE COLORING BOOK

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Georgia Ecological Services Field Offices

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Home page of the Region 4 U.S. Fish and Wildlife Service, representing Alabama, Arkansas, Florida, Georgia, Kentucky, Louisiana, Mississippi, North Carolina, Tennessee, the US Virgin Island, and Puerto Rico, a bureau in the Department of Interior. Our mission is, working with others, to conserve…

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Located in the center of the South Atlantic Bight, coastal Georgia is a region rich in history, beauty, mystery and natural wonders. Cultures have mixed here for ages, just as the rivers mix with the sea. With its large tidal range, vast salt marshes and picturesque barrier islands, coastal Georgia has drawn people throughout its history.

This region's rich mosaic of nutrient-rich estuaries, cultural heritage, productive salt marshes and historic sites provides the backdrop for coastal residents and visitors alike. Some come for the breathtaking vistas and uncrowded beaches; others come to experience the legacy and traditions of an original U.S. colony.

In this richly diversified land-and seascape, activities such as saltwater fishing, sailing, kayaking and bird watching continue to grow in popularity, contributing to the vibrant coastal economy.

As the coastal population and tourism continue to increase, we are charged with striking a balance between human use and the protection of our natural resources. Healthy coastal ecosystems provide many sustainable benefits, from coastal tourism to the harvesting of fresh seafood. It is only through the wise stewardship of our richly endowed environment that the special beauty and life of coastal Georgia will be preserved for generations to come.

The mission of the Department of Natural Resources is to sustain, enhance, protect and conserve Georgia's natural, historic and cultural resources for present and future generations while recognizing the importance of promoting the development of commerce and industry that utilize sound environmental practices.

To enjoy living to the fullest it is momentous to be healthy. How can medications help up? There are sundry conditions when you should buy medicaments online. For example Diprolene cream is a topical corticosteroid. This medicine reduce swelling associated with divers skin problems. One of the most best-known is Levitra. What about buying cialis online and sexual disorders? What do you already know about ? Other question is . While erectile malfunction is more common among older men, that doesn't make it 'normal'. A common class of antidepressants, which include Prozac, can kill the mood in bedroom. What is the most vital information you should consider regard about this? Several people using this curing as a rule do not have possibly serious side effects to Levitra. Follow the directions for use on your prescription label.

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Located in the center of the South Atlantic Bight, coastal Georgia is a region rich in history, beauty, mystery and natural wonders. Cultures have mixed here for ages, just as the rivers mix with the sea. With its large tidal range, vast salt marshes and picturesque barrier islands, coastal Georgia has drawn people throughout its history.

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NOAA's Office of National Marine Sanctuaries is pleased to announce that Stan Rogers, a policy and planning supervisor with NOAA Fisheries, has been named superintendent at Gray's Reef National Marine Sanctuary. He succeeds Sarah Fangman, who left the sanctuary in 2017 to become superintendent at Florida Keys National Marine Sanctuary. Mr. Rogers will begin August 5, 2019.
Press Release
This year NOAA's Office of National Marine Sanctuaries is hosting its fifth national "Get into Your Sanctuary" celebration to raise awareness about the value of our national marine sanctuaries as iconic destinations for responsible recreation through a series of special activities. These events will begin over the long weekend of August 2-4, 2019 across the National Marine Sanctuary System - from sea to shining sea.
Friday, August 2, 2019
Learn About Diving in Gray's Reef

Join us at the Southern Dive Center in Statesboro, GA to learn about diving in Gray's Reef, including experiencing virtual reality dives of this national marine sanctuary.
Saturday, August 3, 2019
There will be a variety of activities surrounding Gray's Reef for "Get Into Your Sanctuary" weekend! They include diving in Gray's Reef National Marine Sanctuary, driving by the Nancy Foster, a NOAA Research Vessel operating at Gray's Reef, and meeting in the ocean with a member of the Gray's Reef science team to learn about research being conducted in this national marine sanctuary.
Sunday, August 4, 2019
Activities from Saturday will continue into Sunday for "Get Into Your Sanctuary" Weekend. They include diving in Gray's Reef National Marine Sanctuary and driving by the Nancy Foster, a NOAA Research Vessel operating at Gray's Reef.
For more information on Diving at Gray's Reef, click HERE

Be aware, and be prepared to slow down or steer clear.

Boat strikes are a leading cause of sea turtle injuries and mortalities.

To learn more click here.

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Welcome: Gray's Reef National Marine Sanctuary

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NOAA's Office of National Marine Sanctuaries is pleased to announce that Stan Rogers, a policy and planning supervisor with NOAA Fisheries, has been named superintendent at Gray's Reef National Marine Sanctuary. He succeeds Sarah Fangman, who left the sanctuary in 2017 to become superintendent at Florida Keys National Marine Sanctuary.

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Wildlife & Habitat

Black bears are just one of the many different species of wildlife that call Okefenokee National Wildlife Refuge "home".

American Alligator

Sandhill Crane

Gopher Tortoise

Longleaf Pine

Okefenokee Swamp

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Wildlife & Habitat - Okefenokee - U.S. Fish and Wildlife Service

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Black bears are just one of the many different species of wildlife that call Okefenokee National Wildlife Refuge "home". American Alligator Sandhill Crane Gopher Tortoise Longleaf Pine Okefenokee Swamp

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USA Today

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Cypress trees sway in the breeze. A heron hunts along the shoreline. The dark shape of an alligator slips silently beneath the surface. There's something about a swamp that is simultaneously repelling and mesmerizing - all nature's beauty and all its danger reflected in the dark water. Swamps and marshes are some of the most crucial ecosystems in Georgia, providing a refuge for countless plant and animal species, and for those who venture into them, endless opportunities for outdoor recreation.

Okefenokee Swamp

Spanning more than 400,000 acres across the Florida/Georgia border, the Okefenokee Swamp is one of the world's largest intact freshwater ecosystems. The bulk of this remarkable place lies on the Georgia side of the state line within Okefenokee National Wildlife Refuge, which includes 353,981 acres of National Wilderness Area. It's the largest swamp in Georgia, home to more than 600 plant species and endangered animals like the wood stork and red-cockaded woodpecker. A strong case could be made for the Okefenokee Swamp as the best bird-watching area in the Eastern United States. It also offers excellent fishing and 120 miles of water trails for canoes and kayaks.

Stephen C. Foster State Park is within Okefenokee National Wildlife Refuge, and it's managed jointly by the Georgia DNR and the U.S. Fish and Wildlife Service. The state park includes boat rentals, water trails, fishing access, guided boat tours, interpretive programs, rental cabins and campsites for tents and RVs.

Chickasawhatchee Swamp

Georgia's second-largest swamp is the Chickasawhatchee, a sprawling wetland complex covering more than 30,000 acres along the Flint River Basin, just outside of Albany. A rich network of forest, creeks and wetlands, the Chickasawhatchee Swamp is an intricate ecosystem that supports an incredible diversity of wildlife, including a thriving alligator population. It's also a crucial nesting ground for migratory birds like the wood thrush and prothonotary warbler. At the center of this swamp, the Flint River is a broad, meandering river that offers excellent canoeing and fishing for shoal bass, a rare relative of the more common largemouth bass.

Nearly 20,000 acres of the Chickasawhatchee Swamp is protected within Chickasawhatchee Wildlife Management Area, which includes ample fishing and boating access, as well as campsites and trails for hiking, biking and horseback riding. The Wildlife Management Area is also open to hunting, so use caution if you visit during one of Georgia's hunting seasons.

Coastal Salt Marshes

The hundred-or-so miles that make up Georgia's coastline are home to ½ million acres of salt marshes, which span an area 4 to 8 miles wide between the mainland and the barrier islands off the Gulf Coast. They are unique, often harsh places. The daily shifting of the tides creates a constant state of flux - many of the areas are inundated by water daily, only to be left dry every time the tide recedes - and few animals are permanent residents. Some species, such as crabs, shrimp and other crustaceans, start their lives here as larvae before migrating toward open waters. Others, including many species of wading birds and predatory fish, come here to hunt.

Salt marshes can be seen along vast stretches of the Georgia coast, but one of the best places to see them is Cumberland Island National Seashore. Managed by the U.S. National Park Service, this national seashore protects Georgia's largest barrier island, along with 9,341 acres of salt marsh. Cumberland Island National Seashore is also home to pristine maritime forests and miles of undeveloped beaches, where visitors can fish, swim, hike, kayak and camp out along the coast.

Know Before You Go

Venturing into any swamp or marshland requires a degree of caution. Many areas in Okefenokee Swamp, Chickasawhatchee Swamp and the marshes along Cumberland Island are developed, with hiking trails, boardwalks, and well-maintained boat launches and fishing access sites that make them relatively safe, but deeper areas within these swamps are still very wild. Hazards range from becoming lost and encountering dangerous wildlife to Lyme disease and heat exhaustion.

If you're planning a canoe or kayak trip, be sure to take necessary safety precautions. Never enter swamp areas alone, always bring an emergency kit, and pack clothing for all weather. If you are unaccustomed to wilderness trips, find an experienced guide who can safely lead your party.

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From the cypress mazes of the Okefenokee Swamp to the vast grassy salt marshes along the coast, wetlands in Georgia provide essential wildlife habitat and unmatched opportunities for adventure.

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Georgia's Natural Wonder Animals

The Okefenokee Swamp is a true wildlife refuge. The wildlife seen in the great swamp are in their natural surroundings. These are the natural inhabitants, the original inhabitants - now protected by law. Few places in America can offer as varied and extensive wildlife as this southeastern swamp. Over 200 species of birds have been identified by refuge personnel and visiting ornithologists. There are over 40 species of mammals, more than 50 species of reptiles, and 60 species of amphibians. The waters house an abundance of fish, 34 different kinds.
Black Bear
The bear is by far the most powerful animal in the Okefenokee. At one time they were a menace to the small farmers living near the swamp. They made repeated raids carrying off hogs, small calves, or anything else they could find to eat. Organized bear hunts were not for sport to the settlers but a necessity to protect their livestock. The bear mates in the summer, and the cubs, usually two, a male and a female, are born in the late winter. At birth the cubs are blind, almost hairless, and weigh less than one pound. The mother often sits with the cubs between her legs, blowing her warm breath on them. They are one of the most helpless and dependent animals at birth and in no way resemble the large and powerful animal they later become. They grow 100 pounds a year for the first two years, then 50 to 75 pounds the next couple of years. A full gown bear will weigh around 300 pounds and stand over six feet tall on his hind legs. In spite of their size, they are not slow and cumbersome, but are capable of great speed. The bear is omnivorous, eating both plants and meat. He eats plants, berries, nuts, roots, insects, fish, eggs and small animals. The bear has even learned to find the camouflaged turtle nest by raking its long claws over the disturbed ground until it finds a deep soft spot. It is able to feast on the eggs hidden from so many other swamp creatures.
Otter
The otter is one of the most graceful of all animals in the water. It swims with tremendous speed, as well as grace, and with seemingly little effort. The otter grows to around four to four and a half feet and weighs around fifteen to twenty pounds. At one time they were hunted by dogs as well as trapped because of their valuable furs.
Water Moccasin
Of the 27 species of snakes in the swamp, the water moccasin is one of the largest and one of the few venomous ones. The majority of snakes lay eggs, but the moccasin is one of the few species that give birth to living young. It has large hollow fangs which are connected to sacs of poison in its cheeks. When biting its enemy, it squeezes the sacs to inject the poisonous venom, and returns to its coiled position in approximately ONE-HALF SECOND.
Alligators
The American Alligator was at one time seriously threatened and considered one of the endangered species. "Gator Hunting" became popular and extremely profitable as reptile shoes, handbags, and belts grew in popularity. The alligator was seldom hunted for sport or game but strictly as a business. Two hunters could kill as many as forty gators in an evening. The female alligator builds a large nest, measuring five or six feet across and two or three feet high, in an open area near the water. She lays 30 to 60 eggs and covers them with leaves, muck, moss, and other trash. She then splashes this down good with water and the sun heats the damp vegetation and the eggs in the mound. It takes from 60 to 90 days for the eggs to hatch, and the baby alligators immediately start making a clucking sound. The mother hearing the clucking, uncovers the newly hatched alligators. When hatched, the young alligators are about six inches long. These young alligators grow about one foot a year for the first six or seven years. Full grown they may reach twelve to fifteen feet in length and weigh 700 pounds. The alligator is extremely fast, although he looks slow and clumsy basking in the sunshine. He feeds on snakes, fish, small animals, turtles, and even baby alligators.
Sandhill Crane
This is a large bird between four and five feet in height. They are gray and have extremely long legs. The Sandhill Crane keeps the same mate for life. They nest in fairly open places where trees do not block their vision. They lay two eggs which take about four weeks to hatch. The young cranes can fly fairly long distances within two months because of their rapid growth. Many Sandhill Cranes were killed in the early hunting days of the swamp. Although they were hard to kill because of their extreme wariness and good vision. When frightened or sensing danger a crane sounds its alarm cry that can be heard for miles. Other cranes and animals recognize the distress call of the Sandhill, take up the cry and flee the area. They have been called the "watchmen of the swamp."
Osprey
At one time the osprey nest served as guide-post to the local natives penetrating the unchartered interior. Osprey are known to be territorial. A pair will build their nest usually in a high tree near a prairie and this area for a couple of miles in all directions will become their domain. No other osprey will establish a nest in their territory. The osprey repair their nests when necessary using the same nest year after year. The fact that these nests are in high places, are large and easily seen, remain for many years, and are several miles apart, make them useful landmarks to the local natives.
Anhinga
Many a new-comer in the early days killed himself a "water turkey", thinking he had a good meal. Anhingas, or water turkeys, look a great deal like a wild turkey except that it has webbed feet and is definitely not good to eat. This bird can fly, swim on top of the water, or dive beneath the water, where it can swim at great speed. It eats a great deal of fish which its speed and keen vision help it secure. After diving beneath the water it takes only a few minutes in the sunshine to sufficiently dry out its feathers enough to fly again. On dark, cloudy days when there is no sun it instinctively knows not to go beneath the water.

Other Swamp Birds include the Barred Owl, Great Blue Heron, Prothonotary Warbler, Yellow Crowned Night Heron, Red-Billed Woodpecker, Great Egret, White Ibis, and many more.

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The Okefenokee Swamp is a true wildlife refuge. The wildlife seen in the great swamp are in their natural surroundings. These are the natural inhabitants, the original inhabitants - now protected by law. Few places in America can offer as varied and extensive wildlife as this southeastern swamp.

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Georgia's Natural Wonder Plants

The Okefenokee Swamp is a true wildlife refuge. The wildlife seen in the great swamp are in their natural surroundings. These are the natural inhabitants, the original inhabitants - now protected by law. Few places in America can offer as varied and extensive wildlife as this southeastern swamp. Over 200 species of birds have been identified by refuge personnel and visiting ornithologists. There are over 40 species of mammals, more than 50 species of reptiles, and 60 species of amphibians. The waters house an abundance of fish, 34 different kinds.
Carnivorous Plants
If an animal eats a plant, it is of no particular interest; but when a plant eats an animal, that is of interest. The fact that there are few flesh-eating plants make them fascinating and interesting to everyone.
Pitcher Plant or Fly Catcher (Saracenia flava)
The inner part of these beautiful pitchers are covered with stiff hairs and are half-filled with a liquid. The insects are attracted by the beautiful flower and the sweet fluid. The hairs on the inner surface of the pitcher allow the insect to travel down but they prevent its traveling upward and out. Therefore it continues downward into the fluid where it drowns. The plant absorbs the soft parts of the body and the skeleton remains in the bottom of the pitcher. Pitcher plants are often found with many skeletons hidden inside.
Bladderwort (Utricularia inflata)
In the springtime the prairies are carpeted in the yellow flower of the bladderwort. This plant lives in shallow waters and swamps of the Southeast. The leaves have small air sacs or bladders in which minute water creatures such as larvae, nematodes, water fleas, protozoa, and small worms are trapped. Each bladder has a small opening through which the tiny animal can enter but cannot escape. Eventually the trapped organisms die and their bodies decompose forming the nitrogenous food for the bladderwort.
Sun Dew (Drosera intermedia)
Small insects, such as gnats are attracted by the beautiful dew-like substance on the leaves of this plant. Once they have come in contact with this sticky substance, however, they cannot escape. After a short time the leaf slowly folds, completely encloses the insect and digests its body.

Other Swamp Plants include Pickerelweed (Pontederia cordata) , Yellow Fringed Orchid (Habenaria ciliaris), Swamp Iris (Iris caroliniana), Grass Pink (Calopogon pulchellus), Water Lily (Castalia odorata), Red Choke Berry (Pyrus arbutifolia), and many more.

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The Okefenokee Swamp is a true wildlife refuge. The wildlife seen in the great swamp are in their natural surroundings. These are the natural inhabitants, the original inhabitants - now protected by law. Few places in America can offer as varied and extensive wildlife as this southeastern swamp.

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UGA Marine Extension and Georgia Sea Grant

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Included are field guides, identification sheets and journal articles that highlight coastal Georgia flora, fauna, educational activities and research.

Coastal Georgia Identification Guides

Coastal Georgia Information

Curriculum

Coastal Birds

Marine Articles

Roger Day's Marsh Madness Study Guides

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Education Resources and Teaching Materials - UGA Marine Extension and Georgia Sea Grant

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These teacher resources were created by UGA Marine Extension and Georgia Sea Grant faculty and Marine Education Interns. Included are field guides, identification sheets and journal articles that highlight coastal Georgia flora, fauna, educational activities and research. Coastal Georgia Identification... Full story

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UGA Marine Extension and Georgia Sea Grant

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Included are field guides, identification sheets and journal articles that highlight coastal Georgia flora, fauna, educational activities and research.

Coastal Georgia Identification Guides

Coastal Georgia Information

Curriculum

Coastal Birds

Marine Articles

Roger Day's Marsh Madness Study Guides

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Education Resources and Teaching Materials - UGA Marine Extension and Georgia Sea Grant

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These teacher resources were created by UGA Marine Extension and Georgia Sea Grant faculty and Marine Education Interns. Included are field guides, identification sheets and journal articles that highlight coastal Georgia flora, fauna, educational activities and research. Coastal Georgia Identification... Full story

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UGA Marine Extension and Georgia Sea Grant

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Twice a day, the tides along the coast rise and fall 6 to 8 feet. The tide allows unique ecosystems to exist, such as the important salt marshes. On the southeastern coast of the United States, salt marshes take shape in shallow areas between barrier islands and the mainland.

The one hundred miles of Georgia's coast has approximately one-half million acres of marshland, each marsh ranging from 4 to 8 miles wide. Georgia has the second largest amount of salt marshes in the United States and the marshland on Georgia's coast makes up an estimated one-third of all the salt marshes on the east coast.

The marsh is a harsh environment for wildlife. The temperature can quickly change with the shifting tides. The inconsistent influx of salt water causes the land to have irregular exposure to air and salt water. This makes it difficult for species to inhabit the marsh full time. Although the marsh is not home to many permanent residents, various land and aquatic species visit the marsh in order to feed and take shelter and the marsh's shallow tidal water is home to the young of many marine species before they return to the open sea.

Ecological Zones of the Marsh

The marsh can be divided up into ecological zones based on the time and depth of the tides.

Levee Marsh

The levee marsh is the habitat on the banks of tidal creeks. The soil is regularly bathed in seawater and the constant supply of water helps the area maintain consistent salinity and temperature. There is a continual flow of nutrients that supports vegetation on the banks, such as smooth cordgrass that can grow up to six feet.

Low Marsh

Beyond the levee is the low marsh. The low marsh zone makes up the majority of the southern marshlands. It is flooded for several hours of the day when the incoming tides overflow the banks of the small surrounding creeks. The shallow seawater gradually drifts over the black marsh mud and the sun shines directly on the water. The sun increases the water temperature and large quantities of organic matter are suspended in the water and mud, thereby reducing the amount of oxygen available to living organisms.

As the temperature of the water increases, it evaporates and leaves behind large amounts of salt causing a rise in salt concentration. In the low marsh, the cordgrass grows between 1 and 3 feet high. The irregular and transient conditions make the low marsh a poor living environment compared to the levee marsh.

High Marsh

After a slight rise in elevation, the low marsh gradually transforms into high marsh. The high marsh is characterized by a sandy soil that is barely covered with water during high tide. The surface is covered for an hour or less each day so the soil surface is exposed to air for long periods of time. Much of the surface water evaporates, which creates a high concentration of salt. The high salt concentration makes it difficult for plants to live in the high marsh. For example, the cordgrass is very small, 3 to 12 inches in height, or not present at all.

Instead, salt-resistant species such as glasswort, saltwort and salt grass thrive in the high marsh. Bare sandy areas, known as "salt pans," occur where the salt concentration has become great enough to prevent all plant life. The levee and low marshes are populated with species like the mud fiddler crabs, purple marsh crabs, oysters, ribbed mussels, polychaete worms and snails. The high marsh is home to sand fiddlers and wharf crabs.

Marsh Border

A zone known as the marsh border is habitat to plant communities. At a higher elevation than the high marsh, there are few seawater floods. The salt concentration is very low without the seawater rushing in and with the freshwater rain and runoff from nearby uplands. At an even higher elevation, additional plants like marsh elder grow. In depressions with small amounts of water, the largest of the fiddler crabs, the brackish-water fiddler, can be found.

Transition Zone

Cabbage palms signify a transition community from the marsh to the woody vegetation that leads toward the maritime forest. The same border communities are seen surrounding the marsh islands or hammocks. This transition community is an ideal area for mammals, birds and reptiles to feed. In some areas, there is a steep increase in elevation and instead of a transition community the forest sits on the edge of the marsh.

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Salt Marsh Ecology - UGA Marine Extension and Georgia Sea Grant

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Georgia has the second largest amount of salt marshes in the United States. Twice a day, the tides along the coast rise and fall 6 to 8 feet. The tide allows unique ecosystems to exist, such as the important salt... Full story

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GPB

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Georgia Outdoors examines a few of our most beloved sea creatures ... and a few that you may not know much about!

From horseshoe crabs mating in the Georgia surf to the populations of Atlantic bottlenose dolphins frolicking along the shoreline, we explore what's being done to help our native marine life flourish.

Web Resources

GA DNR - Coastal Resources Division
Visit the Georgia Department of Natural Resources Coastal Resources Division website for more information on Georgia's sea creatures, fishing regulations, and updates on the status of marine populations.

The Dolphin Project
The Dolphin Project is a non-profit organization devoted to censusing the populations of bottlenose dolphins on the Georgia coast.

Sea Turtles
For more information on the status of loggerhead sea turtles in Georgia and the Sea Turtle Rehabilitation center on Jeckyll Island.

Horseshoe Crabs
Information about the horseshoe crab life cycle and the "Green Eggs and Sand" Teacher Workshop Program.

Georgia Fishing Licenses
There are three ways to buy your fishing license. Visit this website to learn more.

Gray's Reef National Marine Sanctuary
Gray's Reef was designated in January 1981 and is one of the largest near-shore live-bottom reefs in the southeastern United States. The sanctuary is located 17.5 nautical miles off Sapelo Island, Georgia and is one of 13 marine sanctuaries that make up the National Marine Sanctuary System.

GA DNR Nongame & Endangered Species Program
Many of our state's most beautiful and fragile creatures, like bald eagles, manatees and red-cockaded woodpeckers, are threatened as their habitats vanish. For these animals as well as other nongame wildlife, management and habitat conservation are key to their survival. The GA DNR Non-Game and Endangered Species Program is charged with that mission.

The University of Georgia's Marine Education Center and Aquarium (MECA)
MECA provides resources for students, teachers, and the general public in matters related to Georgia's coastal marine environments.

target= "_blank"> PDF Transcript

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Georgia Outdoors examines a few of our most beloved sea creatures ... and a few that you may not know much about! From horseshoe crabs mating in the Georgia surf to the populations of Atlantic bottlenose dolphins frolicking along the shoreline, we explore what's being done to help our native marine life flourish.

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Animals Found in the Piedmont Region of GA

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Animals Found in the Piedmont Region of GA

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Some of the animals that exist in Georgia's Piedmont Region live in more than one area of the state. The Piedmont Region of Georgia is in the Blue Ridge Mountains and the Coastal Plain. Shelter for several animals comes from the oak trees as well as the hickory trees that make up the region's predominant vegetation.

Mammals of the Piedmont region live in several habitats such as wetlands, fields and forests. Raccoons live across the state including the Piedmont. They've adapted to environmental changes, including the loss of natural habitat. Usual food sources for this type of animal are acorns, insects, fruit and random food choices in garbage. The gray fox is another mammal that makes its habitat in the state of Georgia. Its name comes from its predominant gray fur color, though there are some that have reddish fur. The tailed deer is the smallest deer in North America and resides in forests as well as open fields. Opossums prefer to live in the area's pine forests. They feed on numerous food sources such as berries, insects and small rodents.

Great horned owls hunt by sight while using their talons and beaks to capture and hold prey. These owls actually have no horns but ears that resemble horns. Their habitats are forests or wooded sections. Blue jays and cardinals also reside in the region. Both live in forests with diets of fruit, nuts and insects. Other birds of the area include crows.

The venomous timber rattlesnake grows to 4 feet in length. It is considered an endangered species because of the dwindling habitat. Painted turtles exist in ponds or marshes. Another turtle in the region is the snapping turtle, which is among the world's largest type of aquatic turtles. The American toad as well as the bird-voiced tree frog are two of the toad species that live in the Piedmont. A marbled salamander lives in forest burrows or swamps and grows up to 5 inches.

There is a wide selection of fish in the Piedmont region. The shoal bass, spotted bass and largemouth bass are three examples. From the sunfish family, crappies and bluegills both represent freshwater fish varieties. The robust redhorse was thought to be extinct at one time but its rediscovery came in 1991. Catfish as well as walleyes are found in much of the area. The record as of 2011 for the largest walleye catch in the state of Georgia comes from the Richard B. Russell Lake in this region.

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Animals Found in the Piedmont Region of Georgia

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Some of the animals that exist in Georgia's Piedmont Region live in more than one area of the state. The Piedmont Region of Georgia is in the Blue Ridge Mountains and the Coastal Plain. Shelter for several animals comes from the oak trees as well as the hickory trees that make up the region's predominant vegetation.

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Georgia's mountain region is located in the Northern part of the state and includes the Blue Ridge Mountains, the Cohuttas, the Unakas, the Cumberland Plateau and part of the Applalachian Mountains. The mountain region attracts hikers, campers, fishers, naturists and vacationers in part because of the large number and high visibility of many native plants and animals.

Where to Find Wildlife in the Georgia Mountains

Animals venture out during the coolest parts of the day, so the best times to see native wildlife are in the early morning and in the evening. Scenic drives and picnic spots, especially those near forests, are great locations for spotting wildlife. Streams and rivers also attract animals because of the abundance of food and water available. Animals will stay away from loud noises and commotion, so the best chance of seeing wildlife is to sit quietly in an attractive location and wait.

About the Author

Maggie Worth has more than 18 years of marketing and business management experience. She has conducted training classes in resume, fiction and web writing and has written textbooks, resumes, professional and technical documents, ad copy, video scripts and articles for lifestyle magazines. She is director of marketing communications strategy and special projects for a university.

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Georgia's mountain region is located in the Northern part of the state and includes the Blue Ridge Mountains, the Cohuttas, the Unakas, the Cumberland Plateau and part of the Applalachian Mountains. The mountain region attracts hikers, campers, fishers, naturists and vacationers in part because of the large number and high visibility of many native plants and animals.

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New Georgia Encyclopedia

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New Georgia Encyclopedia

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Tropical and subtropical coniferous forests

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New Georgia Encyclopedia

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But the story of Georgia's geology is not just about the past. Georgia is rich in such geological resources as marble, granite, and kaolin; production of these resources accounts for a large proportion of Georgia's wealth. In addition, the geological beauties of rock, river, and mountain provide the attractions that annually draw thousands of tourists to Georgia's state parks and other recreational areas.

Running northeast to southwest through the center of the state, the Piedmont and Blue Ridge provinces are composed mainly of igneous rocks (formed by the cooling and crystallization of molten magma) and metamorphic rocks (caused by extremely high temperatures and pressures deep below the earth's surface). In the area around Elberton huge quarries mine world-famous bodies of granite, an igneous rock, while valuable deposits of slate and marble lie within the Piedmont rocks of central Georgia. Piedmont and Blue Ridge rocks not only have undergone intense metamorphism but also show the effects of having been bent, twisted, and contorted by tremendous compressional forces within the earth's crust, not once but many times. Large ancient faults, long inactive, that slice through the Piedmont area offer further evidence of these enormous forces.

Toward the end of the Paleozoic era, North America collided with the ancient continent of Gondwana to form the supercontinent Pangaea. When Pangaea broke apart due to continental drift during the Triassic period, the great Appalachian chain was also torn apart. Today, segments of the old Appalachians are found in northern South America, North America, northwestern Africa, Greenland, Great Britain, and the Scandinavian region of Europe.

To the west of the Cartersville Fault lie the Valley and Ridge province and the Appalachian Plateau. Rocks of these provinces are generally as ancient as those of the Piedmont but have not been subjected to the intense degree of metamorphism that the Piedmont has. For this reason, they still contain their original sedimentary textures, structures, and fossils. The rocks in these areas occur as layers (also called strata) and consist mainly of sandstones, shales, limestones, and dolostones.

Sedimentary rocks originally were deposited in horizontal layers, but in the Valley and Ridge area these layers have been folded and faulted, squeezed and deformed by the same continental collision event that pushed Piedmont metamorphic rocks westward up and over the Valley and Ridge strata along the Cartersville Fault. As a result, the layers are no longer horizontal but are bent into great folds. As these bent and folded layers of rock gradually weather and erode, they form the long winding ridges and valleys from which the province takes its name. Many of these rocks contain abundant fossils and are famous among paleontologists, both professional and amateur. From these fossils and the rocks that contain them, it is clear that most Valley and Ridge strata formed in ancient seas that inundated the interior of North America numerous times during the Paleozoic era. Views of these folded rock layers may be seen in the rock outcroppings along Interstate 75 between Cartersville and Chattanooga, Tennessee, as well as along many state and county roads in the area.

In the Appalachian Plateau, sedimentary layers are largely undeformed and therefore are still horizontal. At lower elevations, these rocks are mainly limestones and dolostones similar to rocks seen in the Valley and Ridge province. Forming the upland areas of the Plateau region, however, are Pennsylvanian-age sandstones, shale, and coal beds that formed along the coastline of an ancient seaway that extended at times from northwest Georgia all the way to Nevada. These rocks are also fossiliferous and contain beautifully preserved fossils of land-dwelling animals and plants that lived in those coastal forests, marshes, and river floodplains. These rock strata may be seen exposed at Lookout Mountain and Sand Mountain, particularly at Cloudland Canyon State Park just east of Trenton.

Looking at Georgia's geologic map, one can see a distinct change in the character of the land on either side of the fall line. The fall line crosses through the center of the state from Augusta in the east through Macon and on to Columbus in the west and marks the place where rivers flowing off the Piedmont and onto the Coastal Plain have prominent waterfalls and rapids (hence the term fall line). Technically, this line runs from Georgia to New York, forming the boundary between the hard, crystalline rocks of the Piedmont and Blue Ridge and the softer, more erodable strata of the Coastal Plain. The rapids and waterfalls that define the fall line are caused by the different characteristics of the rocks on either side. Rivers cannot erode very deeply into the hard rocks of the Piedmont, but they can easily erode the soft strata of the Coastal Plain. Rapids and falls are formed as the erosion of soft strata results in the streams' channels becoming steeper along the fall line.

South of the fall line are sedimentary strata of the Coastal Plain. In most areas of the Coastal Plain, the strata are undeformed and virtually unaltered. Indeed, in some places these ancient sedimentary strata are still soft, looking almost exactly as they did when they were first deposited. These strata contain fossils that clearly show their age, however.

The oldest Coastal Plain strata in the state are of Triassic, Jurassic, and Lower Cretaceous age. They cannot be seen at the surface, though, because they lie deeply buried beneath younger sedimentary layers. Even though they are buried, they can still be studied by an analysis of drill cores taken from them and by such remote-sensing technology as seismic profiling. From these types of studies geologists have learned that Georgia's deeply buried Coastal Plain sediments formed during the time when North America began to break away from the supercontinent, Pangaea.

The oldest Coastal Plain rocks that are exposed at the surface are of Upper Cretaceous age. These rocks are exposed at the surface in the region between Columbus and Macon and are composed mainly of sandstones, shales, and marls, many containing well-preserved fossils. These fossils and the nature of the sedimentary strata that contain them indicate that they formed in a coastal setting when the sea level was higher than it is today. The deposits accumulated in estuaries, tidal flats, lagoons, barrier islands, and in the shallow sea just offshore. As sea level fluctuated during the Cretaceous, the location of the shore shifted back and forth, leaving deposits all the way from Columbus to Lumpkin. The vertical, unconsolidated sandstone bluffs of Providence Canyon State Park, west of Lumpkin, represent the top formation of these Cretaceous strata. In the region from Macon to Augusta, Cretaceous strata are covered by younger rocks except in river valleys, where stream erosion has cut through the overlying strata to expose the Cretaceous underneath.

Fossils found in the Cretaceous deposits include large numbers of marine invertebrates, including clams, oysters, snails, and extinct Nautilus-like mollusks called ammonites. Also found is a rich collection of vertebrate fossils, notably the remains of duckbill dinosaurs, giant crocodiles, pterosaurs, and the recently discovered Appalachiosaurus montgomeriensis, a relative of the famous Tyrannosaurus rex.

Most of Georgia's Coastal Plain strata formed during the Paleogene period, which covers the time frame from the extinction of the dinosaurs up to what is commonly known as the Ice Ages. These deposits vary widely in their appearance and composition. In many areas, Paleogene Coastal Plain deposits are sandstone, shale, and mudrocks, which are very similar to the Upper Cretaceous rocks beneath them. Like those older deposits, Paleogene strata also formed at or near the ancient coast during times when the sea level was higher than it is today. During the Eocene epoch, sea level was particularly high, and limestone deposits formed extensively in southwestern Georgia; today, these rocks underlie the Dougherty Plain west and south of Albany. The Eocene limestones are very porous and form a major groundwater aquifer system that provides the main source of groundwater in the region. In the central and eastern Georgia Coastal Plain, Paleogene strata are represented by deposits that formed both in coastal and shallow-sea settings as well as in river floodplains adjacent to the coast.

Paleogene Coastal Plain strata are also fossiliferous and often contain well-preserved remains of ancient organisms. Indeed, the official Georgia state fossil is the tooth of the giant fossil shark, Carcharocles (formerly Carcharodon) megalodon. Also found are the remains of an ancient whale, which still retains remnants of hind legs from the time when the whale's ancestors lived on land.

Because Georgia's Coastal Plain strata all decline gently toward the modern coast, the youngest geological deposits in the state are in lowcountry, or coastal Georgia. These strata represent geological formation in coastal settings.

Georgia's coast consists of a chain of sandy barrier islands called the Sea Islands. These islands were inhabited by Native Americans long before the arrival of Europeans in the sixteenth century, and they were later the site of African American communities founded by fugitives from slavery. Today, Georgia's Sea Islands are important tourist destinations. The islands are mainly composed of beach and dune sand, which is constantly washed by waves and blown about by the persistent sea and land breezes. The islands are called barrier islands because they are separated from the mainland by shallow lagoons and marshes.

The highest tidal range along the southeastern shoreline from Cape Hatteras, North Carolina, to Miami Beach, Florida, occurs along the Georgia coast. For this reason tidal marshes and mud flats are extensively developed between the sandy Sea Islands and the mainland. The lagoons, marshes, and flats are of great importance to the coastal economy, both because they function as nurseries for young fish and because the sea grasses that grow on the tidal marshes provide a major source of nutrients to coastal fish.

Just inland from the coast are a series of low sand ridges running from north to south in lowcountry Georgia; these ridges represent former positions of the shore that formed at times of higher sea level during the Pleistocene epoch. The Pleistocene, also known as the Ice Ages, was a time of changing sea levels as the great continental glaciers of northern North America and Eurasia advanced and retreated. For this reason there are today in Georgia five or more of these low sand ridges, almost like stair-steps down to the sea.

In the Valley and Ridge Province, important geological resources include limestones and dolostones. These rocks are used in many ways, including as crushed stone and dimension stone. Limestones are of particular importance as a source of lime for the manufacture of cement and concrete. Both limestone and dolostone are also used in the chemical industry.

Pennsylvanian sandstones from the top of Sand Mountain and Lookout Mountain have been used as building and dimension stone. Perhaps of more importance are the coal deposits in the Appalachian Plateau province. Although these coals are not as thick or abundant in Georgia as they are in adjacent Alabama and Tennessee, they have been mined locally for many years. An unintended benefit of coal-mining is piles of waste rock, mainly shales, from the mining operations; in these shales preserved plant fossils may be found.

Another aspect of Georgia's geological bounty is the land itself. Georgia is widely known for its natural beauty, and visitors from around the nation and the world come every year to see and enjoy Georgia's scenery. Tourists visit the Sea Islands to bathe in the ocean, the Blue Ridge Mountains to gaze down into the spectacular Tallulah Gorge, southwest Georgia to visit Providence Canyon, or northwest Georgia to see Rock City or camp at Cloudland Canyons. Highlighting the state's natural beauty are the many state parks in Georgia.

A vital resource, though sometimes not thought of as geological, is water. Georgia has abundant clean-water resources, but groundwater is also a major resource in the state and is being utilized more and more as the needs of agriculture, industry, and Georgia's communities grow.

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But the story of Georgia's geology is not just about the past. Georgia is rich in such geological resources as marble, granite, and kaolin; production of these resources accounts for a large proportion of Georgia's wealth. In addition, the geological beauties of rock, river, and mountain provide the attractions that annually draw thousands of tourists to Georgia's state parks and other recreational areas.

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The New Georgia Encyclopeia

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Located

in the northwest corner of Georgia, Sand, Lookout, and Pigeon mountains belong to the geologic province known as the Appalachian, or Cumberland, Plateau. This plateau extends continuously from New York to Alabama and forms the western boundary of the Appalachian Mountains. The area has great economic significance because the vast Appalachian coalfield lies beneath it. Only a small segment of the plateau lies in Georgia, and yet this area is one of the most scenic in the state. A visit to Cloudland Canyon State Park, in Dade County, or to Point Park, on Lookout Mountain in neighboring Tennessee, provides spectacular views from the sandstone bluffs that form the edge of the plateau.

The rocks

of the Appalachian Plateau are sedimentary rocks of similar age and type to those found in the Valley and Ridge province to the southeast. The fossils they contain belong to the Paleozoic era and were deposited in shallow seas between the Cambrian and Pennsylvanian periods (540-300 million years ago). Like the rocks of the Valley and Ridge, the Appalachian Plateau was uplifted during the mountain building that formed the Appalachians. However, deformation was less severe, and the folds and faults so characteristic of the Valley and Ridge province die out under the plateau. The plateau is interrupted by several north-northeasterly trending valleys: Lookout Valley; McClemore Cove; Sequatchie Valley (longest of them all), which stretches further northwest into Alabama and Tennessee; and Wills Valley, which extends into Alabama. These valleys have been eroded into limestones and shales exposed along the crests of great folds. Dating from the Cambrian through Devonian periods (542-359 million years ago), these are the oldest rocks exposed in the plateau country. The plateaus, which are actually the flattened bottoms of giant folds of rock, preserve younger rocks from the Mississippian and Pennsylvanian

periods (359-299 million years ago).

At the base of the Mississippian-Pennsylvanian section is a distinctive black shale, the Chattanooga Shale, which dates to the Devonian. It is less than ten meters thick but forms a useful and distinctive marker for geologic mapping. Because of its weakness relative to the overlying limestones, low-angle thrust faults produced during folding commonly flattened out and propagated through the Chattanooga Shale. As a consequence, throughout the plateau country in Georgia, Mississippian and Pennsylvanian strata are detached from older strata by a major subhorizontal thrust fault.

The Mississippian rocks are dominantly limestones and house a famous labyrinth of caves that developed as a result of solution weathering by slightly acidic groundwater. The Pennsylvanian rocks, on the other hand, are mainly sandstones and shales. The resistant sandstones protect the high plateaus from erosion. The resulting topography is an exact reversal of the underlying rock structure; the upfolds form valleys, and the downfolds form the mountain plateaus.

Limestones

in the valleys are full of tropical marine fossils, but the fossils of Pennsylvanian sandstones and shales yield abundant plant leaves and stems. During Pennsylvanian times, shallow seas were being overwhelmed by deltaic sediments shed by the rising Appalachian Mountains. In some places, enough plant debris accumulated to form peat, which upon burial, heating, and compaction was converted to the coal of the Appalachian coalfield.

Other mineral commodities mined in the area include limestone, still mined for cement and aggregate, and ironstone, long since exhausted. Thus the plateau country offered a similar combination of iron ore, coal fuel, and limestone flux to that found near Birmingham, Alabama. In the early 1900s there were thriving blast furnaces at Chattanooga, Tennessee; Gadsden, Alabama; and Rising Fawn, Georgia. However, although similar in age and origin, the iron seams in Georgia were much thinner than those in Alabama and were soon depleted.

A curious natural feature of the plateau country is the development of rock towns. The most famous is Rock City, Tennessee, but the crest of Pigeon Mountain in Georgia is another excellent example. In both cases a jumble of sandstone blocks is separated by a

maze of "streets." Careful mapping shows that the sandstone layers are interbedded with shales. Given a gentle slope and water for lubrication, the sandstones break into blocks that slide slowly apart over the weaker shales. Around the edges of the plateau these blocks have often tumbled down the slopes as immense landslides.

For early settlers moving west into Tennessee and Kentucky, the Cumberland escarpment on the east side of the Appalachian Plateau formed a major obstacle. The southeast sides of Lookout and Pigeon mountains forms the equivalent feature in Georgia. However, in the southern Appalachians, the Tennessee and Coosa river valleys provide natural gaps and routes to the interior. Settlers utilized these gaps for access to rich farm lands in the limestone valleys (Lookout, Sequatchie, and Wills) and generally avoided the plateau country, where the soils were thin and acidic. Apart from a few old coal-mining communities, such as Durham in Walker County, most settlement occurred in such valleys as Trenton Valley in Dade County. This pattern continues to the present day but with increasing housing development along the scenic bluffs overlooking the valleys.

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Located in the northwest corner of Georgia, Sand, Lookout, and Pigeon mountains belong to the geologic province known as the Appalachian, or Cumberland, Plateau. This plateau extends continuously from New York to Alabama and forms the western boundary of the Appalachian Mountains. The area has great economic significance because the vast Appalachian coalfield lies beneath it.

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Site has unknown author

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Appalachian plateau is very diverse . Appalachian plateau is the smallest of the regions. A maze of limestone, caves and deep canyons. interesting
rock formation in the Appalachian plateau . far north western corner of the state. the hottest it gets in the region is 71 the lowest is 50 . lies between ridge and valley to the east and piedmont to the southeast . minerals are iron ore , limestone , petroleum, coal , and natural gases. with lows of 20 . some agriculture products that the Appalachian plateau makes is soybeans, hardwood, birch, corn , and sugar maple. mild summers and cold winters snow and ice. shallow- east moving streams with rapids. landform consist of northeast point of Georgia tip of Cumberland plateau. economy consist of hardwoods, pastures, land same corny soybeans.

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Appalachian plateau is very diverse . Appalachian plateau is the smallest of the regions. A maze of limestone, caves and deep canyons. interesting rock formation in the Appalachian plateau . far north western corner of the state. the hottest it gets in the region is 71 the lowest is 50 .

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*** tornado98/iStock/Getty Images

The Appalachian Mountains of eastern North America are split into several different provinces by geologic character. Among these is the Appalachian Plateau province, which, like the other sections of this ancient mountain belt, contains significant biodiversity.

The broader Appalachian Mountains, one of the world's oldest uplifts, dominate much of the eastern United States and a portion of southeastern Canada. The Appalachian Plateau is the farthest west of the Appalachian provinces and specifically runs from New York southwestward to northern Alabama. The valley and ridge province borders it at its eastern edge.

The plateau, defined mostly by Paleozoic sedimentary rocks, contains both rolling upland and eroded areas of significant relief, such as the Catskill, Pocono, Allegheny, and Cumberland mountains. Elevations typically range from 1,000 to 4,500 feet, with the eastern scarp being the highest portion.

The broad gradient in elevation of the Appalachians and their extended north-south orientation mean they contain a startling diversity of plant communities. The spruce-fir forests cloaking the higher peaks and ridges of the Appalachian Plateau have much in common with the boreal forests of northern Canada and contrast sharply with the rich cove woodlands along the lower drainages, lush with rhododendron, mountain laurel, and tulip trees.

Between these two ecological extremes are other vegetation zones: northern hardwood, oak-hickory, beech-maple, pine-oak, and northern riverine forests, as John C. Kricher and Gordon Morrison define them in their "Field Guide to Eastern Forests" (1998). The development of these vegetation aggregations, as well as more restricted micro-habitats such as talus crevices, depends on environmental factors such as elevation, slope, aspect, and moisture.

The largest mammals of the Appalachian Plateau are black bears and white-tailed deer, both of which are quite widespread and common. The former, restricted to North America, is today the most numerous bear species remaining in the world. Exceptional male black bears may tip the scales at over 800 pounds, but more typically adults weigh between 150 and 450 pounds. Like most of their relatives, black bears are devotedly omnivorous: They will feast on acorns and other mast nuts, shatter fallen logs to slurp up ants and grubs, nibble on berries and forbs, and, occasionally, prey on deer fawns and feral hogs. White-tailed deer favor lower forests and meadows and join the bears in mast harvest.

Other mammals include red and gray foxes, bobcats, fishers, raccoons, opossums, cottontails, and Seminole bats.

The upper-elevation forests of the Appalachian Plateaus bring bird species more associated with northern latitudes to the southern United States, such as ruffed grouse and common ravens. The diversity of habitats available along the Appalachian slope gradient results in significant avian diversity. Warblers flitter in the brush, wild turkeys stalk through woodland shadows, red-shouldered hawks stand sentinel in the canopy, and big, flashy pileated woodpeckers call wildly in between bouts of trunk-hammering.

The Appalachian Mountains as a whole contain North America's greatest diversity of salamanders; some 27 species inhabit the Southern Appalachians, where this variety reaches its zenith. One of the most striking of the Appalachian Plateau's amphibians is the continent's biggest salamander, the hellbender. This relative behemoth, which may exceed two feet in length, favors fast-flowing streams.

Reptiles range from common musk turtles and fence lizards to a variety of snakes, including venomous timber rattlesnakes, copperheads, and cottonmouths.

References

About the Author

Ethan Shaw is an independent naturalist and freelance outdoors/nature writer based in Oregon. He holds a B.S. in Wildlife Ecology and a graduate certificate in G.I.S. from the University of Wisconsin-Madison. His primary interests from both a fieldwork and writing perspective include landscape ecology, geomorphology, the classification of ecosystems, biogeography, wildlife/habitat relationships, and historical ecology. He's written for a variety of outlets, including Earth Touch News, RootsRated, Backpacker, Terrain.org, and Atlas Obscura, and is presently working on a field guide.

Photo Credits

tornado98/iStock/Getty Images

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The Appalachian Mountains of eastern North America are split into several different provinces by geologic character. Among these is the Appalachian Plateau province, which, like the other sections of this ancient mountain belt, contains significant biodiversity. Description The broader Appalachian Mountains, one of ...

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Stay Connected with what's happening in 3rd Grade!

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PPT

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5 Regions of Georgia Heather Robertson (1)

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A site listing all endangered and threatened species - this link is to Georgia (U.S.) page.

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Find out if there are any endangered species in your state, your country, island, etc. Browse endangered species listings according to area on our planet using the selection box below.

For a complete list of US endangered species, select United States below. Browse the different areas in the pulldown for other countries or specific US or Canadian states. For sea creatures and creatures found on islands in the oceans, we recommend browsing the oceania list.

Select an area:

Note/Disclaimer: This list is made possible through a database keyword search/filtering process which may not be 100% accurate. Therefore, all endangered species of Georgia (USA) may not be listed here. For a complete list of endangered species in North America, browse the North America endangered species list or see the complete United States List.

Endangered species found in Georgia (USA):

This list combines species from several endangered species lists. Using the total at the bottom of this page as an official count of endangered species of the world is not recommended. For more information on what creatures are listed on this site, please visit our About Us page.

Species Name

Scientific Name

Group

Range

103.

Red-cockaded Woodpecker

Picoides borealis

Birds

USA (southcentral and southeastern)

118.

Smalltooth Sawfish

Pristis pectinata

Fishes

Gulf of Mexico, Texas through Florida (USA), USA - Atlantic: North Carolina through Florida

142.

Wood Stork

Mycteria americana

Birds

Alabama, Florida, Georgia, South Carolina

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list of endangered animals in georgia (usa)

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list of endangered birds in georgia (usa)

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list of endangered plants in georgia (usa)

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list of endangered species in georgia (usa)

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endangered species list for georgia (usa)

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Endangered species of Georgia (USA) - List - Earth's Endangered Creatures

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Find out if there are any endangered species in your state, your country, island, etc. Browse endangered species listings according to area on our planet using the selection box below. For a complete list of US endangered species, select United States below. Browse the different areas in the pulldown for other countries or specific US or Canadian states.

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Georgia Department of Natural Resources Biodiversity Portal

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Georgia Department of Natural Resources Biodiversity Portal

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Georgia's Imperiled Native Plant Species

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Georgia's Imperiled Native Plant Species

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Seven hundred and fifty-one of Georgia's native plant species are of "special concern" on the State Heritage List. Some are critically endangered with no protection by law, even on state or federal land. The populations are rapidly dwindling and could very well go extinct if conservation actions do not quickly occur. We are working to ensure conservation of Georgia's imperiled plant diversity. You can help us!

At the Mimsie Lanier Center for Native Plant Studies, our core mission is to inspire people to value plants. We do this for all the reasons plants are important; for the survival of other species, for the potential of medicines, for the support of foods, for the sake of clean water, for the production of air, for the beauty they provide by simply existing. We are focused on "high priority species" that are at risk of extinction and in most critical need of conservation actions. We are a research, education and plant production center at the State Botanical Garden in Athens, Georgia, nestled between the prairie, floodplain and forest natural areas. With 2.5 acres of fenced space, we propagate native Georgia plants for habitat restoration, introduction to the gardening community, and endangered species recovery. We also promote the incorporation of Georgia natives into garden displays and right-of-way restoration projects to enhance local biodiversity that contributes to food security, health, emotional well-being and quality of life.

You Can Preserve Georgia's Native Plants

"Preserving Georgia's native plant species is the gift that we leave to future generations of Georgians."
- Mimsie Lanier

The Mimsie Lanier Center for Native Plant Studies has secure collections of ten high priority native plant species, and with your help we can ensure that they are preserved for future generations. A gift of $25,000 to the Mimsie Lanier Center for Native Plant Studies will support conservation efforts for your sponsored plant as well as increase our capacity to preserve and protect other endangered species. You'll become a valued partner in our preservation efforts. Each year we will report to you the progress made on your species, as well as other native plants in Georgia. Your support helps us to strengthen a conservation network across the state that benefits not only the ten species profiled in this effort, but all of Georgia's plant species diversity. As a very special thank you, the first ten Preservation Sponsors will receive an original painting of their species commissioned in their name.

For a limited time, a donor has offered to match the first ten $25,000 Preservation Sponsors -immediately doubling the impact! Won't you please consider joining us in preserving Georgia's native species before it's too late?

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Preserving Georgia's Imperiled Native Species - UGA State Botanical Garden

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Seven hundred and fifty-one of Georgia's native plant species are of "special concern" on the State Heritage List. Some are critically endangered with no protection by law, even on state or federal land. The populations are rapidly dwindling and could very well go extinct if conservation actions do not quickly...

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Georgia Info is an almanac with facts about the state of Georgia.