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Nine-banded armadillo (Dasypus novemcinctus). Cingulata is an order of armored placental mammals.Members of this order are called cingulates, or colloquially, armadillos.They are primarily found in South America, though the northern naked-tailed armadillo is found mainly in Central America and the nine-banded armadillo has a range extending into North America.
A traditional charango made of armadillo, today superseded by wooden charangos, in Museu de la Música de Barcelona. Armadillo shells have traditionally been used to make the back of the charango, an Andean lute instrument. In certain parts of Central and South America, armadillo meat is eaten; it is a popular ingredient in Oaxaca, Mexico.
The six-banded armadillo (Euphractus sexcinctus), also known as the yellow armadillo, is an armadillo found in South America. The sole extant member of its genus, it was first described by Swedish zoologist Carl Linnaeus in 1758. The six-banded armadillo is typically between 40 and 50 centimeters (16 and 20 in) in head-and-body length, and ...
The nine-banded armadillo has been rapidly expanding its range both north and east within the United States, where it is the only regularly occurring species of armadillo. The armadillo crossed the Rio Grande from Mexico in the late 19th century, and was introduced in Florida at about the same time by humans.
Two groups of cingulates much larger than extant armadillos (maximum body mass of 45 kg (100 lb) in the case of the giant armadillo [2]) existed until recently: pampatheriids, which reached weights of up to 200 kg (440 lb) [3] and chlamyphorid glyptodonts, which attained masses of 2,000 kg (4,400 lb) [4] or more.
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Hand anatomy of the giant armadillo. The giant armadillo is the largest living species of armadillo, with 11 to 13 hinged bands protecting the body and a further three or four on the neck. [6] Its body is dark brown in color, with a lighter, yellowish band running along the sides, and a pale, yellow-white head.
The Red Lake sinkhole in Croatia. A sinkhole is a depression or hole in the ground caused by some form of collapse of the surface layer. The term is sometimes used to refer to doline, enclosed depressions that are also known as shakeholes, and to openings where surface water enters into underground passages known as ponor, swallow hole or swallet.