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Dent Marble is a highly polished form of limestone which occurs in the Dentdale district of Cumbria in England. The stone is noted for the presence of fossils which gives it its distinctive look. The stone is actually a crinoidal limestone and is not a true marble, but is known as a marble because it polished quite well. Dent Marble has been ...
The dimension-stone industry classifies stone based on appearance and hardness as either "granite", "marble" or "slate". The granite of the dimension-stone industry along with truly granitic rock also includes gneiss , gabbro , anorthosite and even some sedimentary rocks .
It is high density, high magnesium dolomitic limestone. [2] It was originally classified as a marble in Oklahoma due to the fact that it would hold a high polish, hence Marble City. It is sold in slabs and as tiles, in a similar manner as marble would be. [3] This unit has many economic uses in Arkansas and Oklahoma.
Cotham Marble – Limestone variety from Great Britain (not a "true marble"; stromatolitic limestone) Cotswold stone – oolitic limestone used for building and roofing in the Cotswolds; Dent Marble (not a "true marble"; Crinoidal limestone) Frosterley Marble – northern England (not a "true marble") Hamstone – Building stone from Somerset
Lime – acts as a binder and contains particles of raw limestone and over burnt lime. Fuel ash – this pozzolanic material binds its constituent Si(OH) 4 with the Ca² ions in a pozzolanic reaction. It contains burnt wood or coal. Gypsum, to help with set; Clay with fragments of broken brick and tile, another pozzolanic material
Frosterley Marble is a black, bituminous coraliferous limestone containing fossil crinoids of the Lower Carboniferous (Mississippian ), some 325 million years ago. [ 1 ] [ 2 ] : 40 It outcrops in Weardale , County Durham , England, including near the village of Frosterley whence it is named.