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(The larger grains of coarse sand, gravel, and boulders are too large to be transported to the deep sea and therefore are not discussed here.) Physical weathering is caused by mechanical fracturing of rocks, such as that due to the freezing of water in cracks, and results in finer grained, compositionally similar examples of the original rock.On the other hand, chemical weathering, caused by the weak acid produced by the interaction of rainwater and atmospheric carbon dioxide, degrades the rock slowly and often produces fine-grained minerals that are compositionally distinct from the original rock.You will get more interest and responses here than all paid dating sites combined!Over 1,500,000 Daters login every day to Plentyoffish.com, we are the market leader in Canada, UK, Australia, US, Ireland and New Zealand, so come meet and chat with other Ocean City singles Register HERE The only 100% Free dating service.

The different combinations of each process' effectiveness result in a commensurate variety of sedimentation rates.The production of marine sediment is more complex than it may seem.Terrigenous sediment is produced by an interplay of chemical and physical weathering processes, which collectively serve to create small grains of material ranging in size from thousandths of millimeters to 1 or 2 millimeters(0.04 or 0.08 inch).Cosmogenic material is the remains of primordial material left over from the creation of the solar system (and perhaps from beyond) and, although very low in abundance, is ubiquitously distributed.The production of hydrogenous sediment is most difficult to visualize, but involves either the slow precipitation of dissolved chemicals from sea water or the leaching of chemical elements from rocks that have extremely hot sea water (greater than 300°C [572°F]) circulating through them along mid-ocean ridges.

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