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Helix pomatia, known as the Roman snail, Burgundy snail, or escargot, is a species of large, air-breathing stylommatophoran land snail native to Europe. It is characterized by a globular brown shell. It is an edible species which commonly occurs synanthropically throughout its range.
Athearnia anthonyi is a rare species of freshwater snail in the family Pleuroceridae. Its common name is Anthony's riversnail . It is native to three rivers in the Tennessee River system in the United States: the main branch and the Sequatchie River and Limestone Creek.
Helicidae is a large, diverse family of western Palaearctic, medium to large-sized, air-breathing land snails, sometimes called the "typical snails."It includes some of the largest European land snails, several species are common in anthropogenic habitats, and some became invasive on other continents.
Beech River: Tennessee River: 38.3 mi (61.6 km) Lexington: Big Sandy River: Tennessee River: 60 mi (97 km) Bruceton: Big South Fork of the Cumberland River: Cumberland River: 76 mi (122 km) none (Big South Fork National River and Recreation Area) Blackburn Fork River: Roaring River: 14.5 mi [2] none (Cummins Falls State Park) Blood River ...
Freshwater snails are gastropod mollusks that live in fresh water. There are many different families. There are many different families. They are found throughout the world in various habitats, ranging from ephemeral pools to the largest lakes, and from small seeps and springs to major rivers.
The snail darter is quite literally the legal textbook case for the Endangered Species Act in the lawsuit Tennessee Valley Authority vs. Hill. Snail darters are no longer endangered. The tiny fish ...
The spiny river snail, scientific name Io fluvialis, is a species of freshwater snail, an aquatic mollusk in the family Pleuroceridae. This is the only species in the genus Io . [ 3 ] This species is endemic to the USA.
The Mississippi River as well as the Tennessee and Cumberland Rivers formed and cut deep into the valleys. The Nashville Basin , which in reality is a geologic dome , was pushed up from underneath by a mantle plume , exposing softer strata that with additional erosion on the Highland Rim surrounding the basin expanded the size of the basin.