Concretions
Dating back to the 18th century concretions have been known as geologic curiosity's 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 curiosity's I will try and enlighten you more on these in the following by explaining the process in which they are formed and explaining some locations where they can 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 different shapes and the most common of the shapes is spherical or disk shaped. Concretions are the most varied-shaped rocks of the sedimentary world. The way concretions come to be is the mineral matter concentrates around the nucleus 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 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 separation 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. In these iron stone concretions water dissolves the iron compounds from the inner portion of a block and then deposits the iron compounds as insoluble iron oxide or iron hydroxide in the outer parts of the block. As the water dissolves the iron hydroxide/oxide and deposits them in the outer portion it cements together grains in the original host rock to make that specific zone harder. One way to tell that it is an ironstone concretion is that there is often brown, yellow or red concentric ironstone bands inside the block. This process only takes place as long as the rock is below the ground water level. When the water level drops is when the drying and oxidation begin to take place. After this is when the concretion may be released from the surrounding softer rock due to weathering and also because the concretion is harder and more resistant. They will be found as separate objects on the ground or in the soil and as erosion takes place it wears down the edges and corners of the concretion giving it the typical round or disk shaped appearance. 2.) "Concretions Thunder Eggs and Geodes." www.austmus.gov.au/is/sand/geods.htm, Concretions are most commonly composed of calcite but sometimes can be composed of iron oxide or iron hydroxide such as goethite. But also concretions can be composed of other minerals ranging from siderite, ankerite, dolomite, pyrite, baryite and gypsum. 3.) "Naturally Weird Concretions." www.rcbm1.rcbm.gov.bc.ca/index.html,
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Approximate Word count = 1427
Approximate Pages = 6 (250 words per page double spaced)
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