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Marl

Lower Saxony, Germany
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Freizeitbad Dummer Martin-Luther-Kirche Sette Dümmer Kirche Brockum Dummer-Museum Bright Side Tours Stemweder Berg Thielmannshorst

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DAMME    12 BOHMTE    13 DIEPHOLZ    14 STEINFELD    15 WAGENFELD    16 OSTERCAPPELN    17 RAHDEN    18 BAD ESSEN    19 HOLDORF    20 ESPELKAMP    21 PREUSSISCH OLDENDORF    22 LOHNE    22 DINKLAGE    26 BELM    26 LÜBBECKE    26 BARNSTORF    27 RÖDINGHAUSEN    27 VECHTA    28 BRAMSCHE    28 WALLENHORST    28

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Marl,  Lower Saxony, Germany

Marl - Lime-rich mud or mudstone which contains variable amounts of clays and silt

Population: 570 inh.
Region: Lower Saxony
Country: Germany
Continent: EU

"Marl or marlstone is a calcium carbonate or lime-rich mud or mudstone which contains variable amounts of clays and silt. The dominant carbonate mineral in most marls is calcite, but other carbonate minerals such as aragonite, dolomite, and siderite may be present. Marl was originally an old term loosely applied to a variety of materials, most of which occur as loose, earthy deposits consisting chiefly of an intimate mixture of clay and calcium carbonate, formed under freshwater conditions; specifically an earthy substance containing 35–65% clay and 65–35% carbonate. It also describes a habit of coralline red alga. The term is today often used to describe indurated marine deposits and lacustrine (lake) sediments which more accurately should be named 'marlstone'. Marlstone is an indurated rock of about the same composition as marl, more correctly called an earthy or impure argillaceous limestone. It has a blocky subconchoidal fracture, and is less fissile than shale. The term 'marl' is widely used in English-language geology, while the terms Mergel and Seekreide are used in European references. - Wikipedia"

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