Determining the Paleoenviroment and Tectonic History of a Small Area

======== In this lesson to decide the cell planning and construction of the paleo environmental history, I tried to find the environment of the crustal deformation of the region at the Northumberland short beach, trying to find the environment of the ancient rock, Cocklawburn The beach is located in Berwick - OS map 75 is 50 meters south of -upon-tweed. It is mainly geological region mainly present in coal, limestone, interlayer multilayered sandstone, shale, limestone and coal.

The term construction refers to the study of the surface structure of the earth and how it changes with the passage of time. Convert convergence boundary, boundary or divergent boundary: Construction typically occurs between plate boundaries, plate boundaries occur in one of three types. The process of forming the terrain increased the surface of the earth rising by the hydrostatic press, modifying effectively, and effectively alleviating the deformation mechanism of obstacles and crustal thickening folded forms. It brings a steeper rise than the gradient, which increases the precipitation into the landscape, leading to a sharp increase in the final erosion rate associated with the river baseline level region. The topography and general undulations of a particular area determine the rate at which the surface runoff flows and ultimately determine the potential erosiveness of the spill.

For thousands of years, construction plates have identified changes in geophysical features, and they continue to do so today. These huge plates move under the surface of the ocean and continent, creating earthquakes, volcanoes and ridges. In this article, we discuss structural plates of composition, movement and history, not only plate tectonics and its history, but also the theory of structural plates influence the surface of the earth now and in the future. The earth is divided into three main layers: the core, the mantle and the Earth's crust. The core is further divided into a solid core and a liquid outer core. This layer is mainly iron and nickel and it is very hot. The mantle is divided into the lower mantle and the upper mantle, which are mainly composed of iron, magnesium, silicon and oxygen. The outermost layer including all life on Earth is the Earth's crust.

Plate tectonics theory, lithospheric is divided into a small number of floating (floating outside on the outer solid Earth) mantle and independently on the running plate. Most of earth's earthquake activity and volcanic activity, and most of mountain activity are generated at the boundary of these plates. The surface of the earth consists of about a dozen large plates and several small plates. In each sector, it is a ground crustal rock rigid body, and slight bending shows almost seismic activity and volcanic activity. 80% of the earthquakes in the world and a narrow volcanic zone define the edge of the plate. There are three kinds at the boundary. The first is a very narrow shallow seismic zone, caused by tensile stresses next to the 80 thousand kilometers (48 thousand miles) on the long active ridge. The second boundary type is displayed in the area of ​​these ridge offsets.