The Lithostratigraphic Framework of the Hertfordshire County of Essay

The Lithostratigraphic Framework of the Hertfordshire County of England - Essay ExampleThe Hertfordshire County of England has a unsalted history geologically. The lithology of this area is largely composed of Quaternary and Tertiary deposits, with some glacial movement personal effects at its northern reaches. With the sandy conditions of the shores on its eastern side, you might say Hertfordshire is among a small rock and a big hard place. Formations, a principal mapping unit (enquire.com 2006), will be briefly described as to their importance in this report. The status of current ground conditions will as well be presented as they affect the analysis of the area. Then geohazards, or expected/probable problems, will be considered. The objective of this report is to provide information that subsequent investigations could use. As in opposite Home Counties, Hertfordshire shares a common pattern of development from the 17th century, except for its construction of the New River in the Lea valley that supplies London with water. The majority of settlements built in the times of the Normans were in the northeast. The Abbey of St. Albans, a major landowner, influenced land charge strongly, including the formation of hunting parks, which Hertfordshire has had in abundance. Agriculture displaced m all of these parks, and then they were wooded again. A boom in the 16th century of the country-house building came after lands were confiscated by the Crown. The number of palaces from the 1700s were many because of the rich soil and alimental air that attracted wealthy people. (enquire.com 2006) Other building came along the river valleys, slowly. But the industry of malting and brewing in the upstart 19th century created an era of strong development. The decades since the mid-1900s has seen major changes in the landscape of Hertfordshire.The development of Portland cement in the early 1900s, that uses gravel deposits in its composition, brought about quarries and i ndustry related to it (HGS 2005). Quarries have also been necessary for researching the strata of the land. new construction has been largely in the south/southwest part of the county. This report, focusing on Stevenage and Ware, is for development purposes in the northern sections of the county.Near Ashwell is the Steeple Morden Plantation Quarry that allows geologists to see the layers of rock. In trenches cut into the quarry, the color contrasts between Melbourn Rock and the soft chalk is obvious. The gray Plenus Marls and Melbourn Rock that were once thought to be the base of the heart Chalk (HGS 2005) is now considered the marker sight while shelly detrital rock is above that and smooth chalk above that. The eight beds of the Plenus Marls can be traced to the Paris Basin and used as a marker horizon across Europe, indicating a change in anoxic conditions (HGS 2005).There is a lack of clay-with-flints this quarry. Quarry section presentation chalky outwash gravel of Anglian age overlying river gravel of proto-Thames (photo by John Carr) (RIGS 2003) The formations and types of sediments in Hertfordshire will be discussed as they pertain to development, and also as they pertain to restrictions of use (RIGS 2003). Besides the geohazards possible in any construction site, there are also hazards to the geology of a site from construction. All this must be interpreted into consideration before building can begin. Former construction through the ages has not taken this into distinguish and there has been a degeneration of soils as well as destruction to the buildings by swallow holes and other phenomenon.