Concretions :: essays research papers fc

Dating back to the 18th century concretions have been known as geologic curiositys due to the various sizes, shapes and compositions. Concretions have also been thought to be dinosaur eggs, extra-terrestrial debris, human artifacts and animal and plant fossils. Due to these curiositys I will try and enlighten you more on these in the following by explaining the process in which they atomic number 18 formed and explaining some locations where they lowlife be found in large outcrops.     The word "concretion" is derived from the Latin "con"-- meaning "together" -- and "cresco" -- meaning "to grow."      Concretions are hard compact accumulations of mineral matter and are found inside sedimentary rocks. Some examples of this are Sandstone and in some weathered volcanic rock. Concretions come in many contrary shapes and the most common of the shapes is spherical or disk shaped. Concretions are the most va ried-shaped rocks of the sedimentary world. The way concretions come to be is the mineral matter concentrates around the centre of a host rock. The nucleus is often organic such as a tooth or leaf or shell or fossil. As the mineral matter concentrates around the nucleus it forms harder zones known as nodules.     Concretions are very odd in the sense that they very in size, shape, color and hardness. Often concretions are mistaken for bones, fossils, meteorites and other odd objects. They can be so small that it requires a magnifying glass to be visible or as large as 10 feet in diameter and weigh hundreds of pounds. Concretions can also have somewhat of regular shapes such as boxes, blocks, flat disks, pipes, cannon balls and have scour been known to resemble parts of a human body such as a foot or ribs.     Concretions are most commonly sedate of calcite but sometimes can be composed of iron oxide or iron hydroxide such as goethite. But a lso concretions can be composed of other minerals ranging from siderite, ankerite, dolomite, pyrite, baryite and gypsum.     Concretions form in many different ways. The box shape of some ironstone concretions most often depend on the way a sandstone or shale bed breaks up due to the action of weathering into regular blocks of various sizes. The way in which this disengagement takes place along natural planes of weakness in a rock such as a horizontal bedding surface and vertical joints. Before this process of separation, as well as during the separation ground water soaks into the rock and circulates through the planes of weakness making the rock more porous.