How to find out t booka he dip & strike in contour problems pls reply
same
don't askme
The layers of rock (strata) we see on the Earth's surface are rarely found in their original flat orientation. Measuring dip and strike is pretty easy, all you need is a compass for the level direction, and a clinometer to measure the vertical angle. For basic dip measurements I use an angle finder from a hardware store costing a couple of pounds (about 3-4 dollars US). I expect your tutor will expect you to sing the praises of the expensive "Brunton" combined compass and clinometer. (I don't know why, I have never found the point of spending huge amounts of money on this - but they remain a venerated item min American geology) Why bother? Measuring dip and strike is a fundamental part of geological mapping as you can build up a picture of the tilting and folding of the rocks beneath the surface, and start to build up a three dimensional model of the geology from the two-dimensional information at the surface. This is useful in predicting such things as the location and depth of an underground coal seam, or of working out the geological history of an area. If you cannot measure dip and strike directly, by measuring it off the surface of an exposed outcrop, then you can calculate it by measuring the height and direction an outcrop of the same strata run on opposite sides of a hill or valley, and doing some trigonometry.
Earthquake is the result of a sudden release of energy in the Earth's crust that creates seismic waves.Tectonic earthquakes will occur anywhere within the earth where there is sufficient stored elastic strain energy to drive fracture propagation along a fault plane.There are three main types of fault that may cause an earthquake: normal, reverse (thrust) and strike-slip. Normal and reverse faulting are examples of dip-slip, where the displacement along the fault is in the direction of dip and movement on them involves a vertical component. Normal faults occur mainly in areas where the crust is being extended such as a divergent boundary. Reverse faults occur in areas where the crust is being shortened such as at a convergent boundary. Strike-slip faults are steep structures where the two sides of the fault slip horizontally past each other ; transform boundaries are a particular type of strike-slip fault. Many earthquakes are caused by movement on faults that have components of both dip-slip and strike-slip; this is known as oblique slip.Earthquakes often occur in volcanic regions and are caused there, both by tectonic faults and the movement of magma in volcanoes. Such earthquakes can serve as an early warning of volcanic eruptions.
CI Dip Pay
The name of the microscope slide with the dip in it is the hanging drop slide. The dip is a special concave, depression, in the center of the slide.
Dip and strike are a method of describing the orientation of a plane in three dimensional space. It is usually applied to the orientation of tilted layers of rock. Dip is the angle of tilt, measured from the horizontal. Think of the direction of dip as the direction that a ball would roll if placed on the surface. The angle of dip is measured in degrees. Strike is the direction of a level line on that tilted surface. It is more difficult to visualize, but easy to remember because it is always perpendicular to the direction of dip. To visualize use a book. Prop up one end on another book. Then examine the surface of the book. If you have a marble place it on the book and watch it roll down the dip. To see the strike kneel down and look at the book from the side so that you see either the binding or the pages. Now take a ruler and try to lay it on the book so that the marble will not roll along the edge of the ruler. When you have done that you will have found the strike, and it will be perpendicular to the dip. The strike is easy to find if you have a carpenter's level (of course, everyone has one of those lying around). Submitted by R. Brill, Professor of Natural Science, Honolulu Community College
Yes,angle of dip,or angle of inclination is the angle that a compass arrow direction or an axis of magnetic needle makes with plane of the horizon. Strike and dip are the terms of Geophysics and Geology applied them to determine the coordinates of the location of any geological object.
Dip-Slip fault is a bedding fault and its pattern is En-Echelon, while Strike Slip fault is strike fault and its pattern is Parallel.
don't askme
Dip-Slip fault is a bedding fault and its pattern is En-Echelon, while Strike Slip fault is strike fault and its pattern is Parallel.
We got ours from the ford dealership in our town.
has to do with the movement
No. It is a strike-slip fault.
There are two different right hand rules...American right hand rule: Looking to the strike direction, the bed dips to the right. In our example, that would fit with 000/45. So, looking to the north, the bed dips to the right, to 090 (east).British right hand rule: The thumb of the right hand indicates the dip direction, and the heal points to the strike direction. So in our example, we would record the orientation as 180/45. That is: Strike towards 180 (perfect south bearing), and dip of 45º towards 090.
Dip-slip faults is the term used for any fault that has movement in the vertical direction. One side moves up where as the other side moves down. Examples are Normal Fault and Reverse fault.
dip is angle of ore body from horizontal plan.and strike is perpendicular to dip.these are important parameters to represent orientation of ore body.
A fault that is a combination of dip-slip and strike-slip movements