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Qu'est-ce (qui) est marl$46949$ - définition
Kueper marl; Keuper Marl
Marlite
![Geological profile along the tunnel as constructed. For most of its length the tunnel bores through a [[chalk marl]] stratum (layer)](https://commons.wikimedia.org/wiki/Special:FilePath/Channel Tunnel geological profile 1.svg?width=200 "Geological profile along the tunnel as constructed. For most of its length the tunnel bores through a [[chalk marl]] stratum (layer)")
![[[Scala dei Turchi]] coastal marl formation, southern [[Sicily]]](https://commons.wikimedia.org/wiki/Special:FilePath/Scala dei Turchi panorama.jpg?width=200 "[[Scala dei Turchi]] coastal marl formation, southern [[Sicily]]")
CALCIUM CARBONATE OR LIME-RICH MUD OR MUDSTONE WHICH CONTAINS VARIABLE AMOUNTS OF CLAYS AND SILT
Marlstone; Marlite; Marl stone; Marls; Mergel; Marlstones; Blue marl; Marl lakes; Buda Marl; Buda marl
·noun A variety of marl.
Marl
CALCIUM CARBONATE OR LIME-RICH MUD OR MUDSTONE WHICH CONTAINS VARIABLE AMOUNTS OF CLAYS AND SILT
Marlstone; Marlite; Marl stone; Marls; Mergel; Marlstones; Blue marl; Marl lakes; Buda Marl; Buda marl
Marl is an earthy material rich in carbonate minerals, clays, and silt. When hardened into rock, this becomes marlstone.
Marl
CALCIUM CARBONATE OR LIME-RICH MUD OR MUDSTONE WHICH CONTAINS VARIABLE AMOUNTS OF CLAYS AND SILT
Marlstone; Marlite; Marl stone; Marls; Mergel; Marlstones; Blue marl; Marl lakes; Buda Marl; Buda marl
·noun To overspread or manure with marl; as, to marl a field.
II. Marl ·vt To cover, as part of a rope, with marline, marking a pecular hitch at each turn to prevent unwinding.
III. Marl ·noun A mixed earthy substance, consisting of carbonate of lime, clay, and sand, in very varivble proportions, and accordingly designated as calcareous, clayey, or sandy. ·see Greensand.
Wikipédia
Keuper marl
Keuper marl is a former and now deprecated term for multiple layers of mudstone and siltstone of Triassic age which occur beneath parts of the English Midlands and neighbouring areas e.g. Cheshire, Nottinghamshire, Devon, eastern Worcestershire and northern Yorkshire.
Typically red, or occasionally green or grey, these strata are generally featureless and contain few fossils. In basin formations, thick halite-bearing layers, or rock salt deposits, are sometimes present at the base of the marl.
In modern nomenclature, Keuper marl is included within the Mercia Mudstone Group.
