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Topics related to "Catfishs name is no longer mud"

mud mud
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drilling mud drilling mud
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mud mound mud mound
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Mudejar Mudejar
Mudéjar , name given to the Moors who remained in Spain after the Christian reconquest but were not converted to Christianity, and to the style of Spanish architecture and decoration, strongly influenced by Moorish taste and workmanship, that they developed. In erecting Romanesque, Gothic,... Read more
snipe snipe
snipe common name for a shore bird of the family Scolopacidae ( sandpiper family), native to the Old and New Worlds. The common, or Wilson's snipe ( Capella gallinago ), also called jacksnipe, is a game bird of marshes and meadows. It has an unusual courtship dance, circling and diving in the air.... Read more
Kalisz Kalisz
Kalisz, Poland Calisia Founded on an ancient trade route, it was known to Ptolemy in the 2nd century as Calisia. The name may be derived from a Slavonic root element kal ‘mud’ to give the meaning of a ‘muddy place’. It is situated on the Prosna River.... Read more
flamingo flamingo
flamingo common name for a large pink or red wading bird, similar to the related heron, stork, and spoonbill but with a longer neck, webbed feet, and a unique down-bent bill. Flamingos are tropical birds, although large colonies have been observed high in the Andes. The American, or greater,... Read more
Keetmanshoop Keetmanshoop
Keetmanshoop, Namibia NuGoeis, Swartmodder The Afrikaans name Swartmodder ‘Black Mud’ from swart ‘black’, adopted in 1810, had the same meaning as the original Khoikhoin name. When a German Lutheran mission station was founded here in 1866, it was named after Johann ... Read more
shoebill stork shoebill stork
shoebill stork common name for a large (up to 54 in./122 cm) tall, storklike bird, Balaeniceps rex. Also known as the whalehead, it is noted for its large head and unusually long and wide, many-colored bill, which ends in a hooked tip. It has broad wings and long, strong legs with large, unwebbed... Read more
kame kame
kame , low, steep, rounded hill or ridge of layered sand and gravel drift, developed from glacial deposits. Kames were probably formed by streams of melting glacial ice that deposited mud and sand along the ice front. The subsequent retreat of the glacier left them as more or less isolated hills and... Read more

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