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Mud (probably from Middle Low German mudde, mod(de) 'thick mud', or Middle Dutch) [1] is loam, silt or clay mixed with water. Mud is usually formed after rainfall or near water sources. Ancient mud deposits hardened over geological time to form sedimentary rock such as shale or mudstone (generally called lutites ).
Choqa Zanbil, a 13th-century BCE ziggurat in Iran, is similarly constructed from clay bricks combined with burnt bricks. [1] Mudbrick or mud-brick, also known as unfired brick, is an air-dried brick, made of a mixture of mud (containing loam, clay, sand and water) mixed with a binding material such as rice husks or straw. Mudbricks are known ...
Straw is useful in binding the brick together and allowing the brick to dry evenly, thereby preventing cracking due to uneven shrinkage rates through the brick. [12] Dung offers the same advantage. The most desirable soil texture for producing the mud of adobe is 15% clay, 10–30% silt, and 55–75% fine sand. [13]
Volcanic ash already deposited on the surface can be transported as mud flows when mingled with water from rainfall or through eruption into a body of water or ice. [16] Particles of volcanic ash that are sufficiently hot will weld together after settling to the surface, producing a welded tuff. Welding requires temperatures in excess of 600 ...
Grey chunks of graptolitic argillite on Pakri Peninsula, Estonia; yellowish and white chunks are limestone. Argillite (/ ˈ ɑːr dʒ ɪ l aɪ t /) is a fine-grained sedimentary rock composed predominantly of indurated clay particles.
English: This mud-brick was stamped with a cuneiform text mentioning the name of the builder, the neo-Babylonian king Nebuchadnezzar II. The procession street at Babylon, Mesopotamia, Iraq, 6th century BC.
Rebuilding in this mud brick form is just going to create the next disaster in 20 or 30 years time," said Colin Taylor, emeritus professor of earthquake engineering at the University of Bristol.
In the Dunham classification (Dunham, 1962 [11]) system of limestones, a mudstone is defined as a mud-supported carbonate rock that contains less than 10% grains. Most recently, this definition has been clarified as a matrix-supported carbonate-dominated rock composed of more than 90% carbonate mud (<63 μm) component .
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