Showing posts with label map scale. Show all posts
Showing posts with label map scale. Show all posts

Sunday, 11 November 2018

QUESTION: Describe the methods of inverted staff reading & reciprocal levelling


1       Describe the methods of inverted staff reading & reciprocal levelling
 Image result for reciprocal levelling
                       In levelling there are other levelling method which is inverted staff reading and reciprocal levelling. Inverted staff it may be necessary to determine the reduced levels of points such as the soffit of a bridge, underpass or canopy. Generally, these points will be above the line of collimation. To obtain the reduced levels of such points, the staff is held upside down in an inverted position with its base on the elevated points. When booking an inverted it is entered in the levelling table with a minus sign, the calculation proceeding in the normal way, taking this sign into account. An inverted staff position must not be used as a change point since there is often difficulty in keeping the staff vertical and in keeping its base in the same position for more than one reading. An inverted staff position must be used as a change point because it is often difficult to keep the staff vertical and to keep iys base in the same position for more than one reading.
Image result for reciprocal levelling
                           True differences in height are obtained by ensuring that back sight and fort sight lengths are equal when levelling. This eliminates the effect of any collimation error that may be present in the level used and also eliminates the effects of curvature and refraction. There are certain cases, however, when it may be not be possible to take readings with equal sight lengths as, for instance, when a line of levels has to be taken over a wide gap such as river. In these cases, the technique of reciprocal levelling can be adopted.
Image result for reciprocal levelling
                     Figure down shows two point A and B on opposite sides of a wide river. The line of collimation has been assumed to be elevated above the horizontal plane. This may not be the case but does not affect the calculations. To obtain the true difference in level between A and B a level is placed at I1 about 5m from A, and a staff is held vertically at A and B . Staff readings are taken at A (a1) and B (b1). The level is next taken to position I2 where readings a2 and b2 are recorded. Since the observations are taken over the same sighting distances with the same level, the effects of the collimation error will be the same for both cases. When repciprocal levelling with one level, the two sets of observations must follow each other as soon as possible so that refraction effects are the same and are therefore eliminated. Where this not possible, two levels have to be used simultaneously. It must be realised  that the levels should have the same collimation error or the true height different will not be obtained.
                  


Image result for reciprocal levelling
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Monday, 13 February 2017

Topographic Map Scale

Another thing you need to understand about a topographic
map is scale. Obviously, maps aren't life-sized. Otherwise
we'd never be able to fit them in our backpacks. Instead,
cartographers plot maps on a ratio scale, where one
measurement on the map equals another larger amount in
the real world.
The first number of the scale is always one. It's your unit
of measurement, usually an inch. The second number is
the ground distance. For example, if your U.S. Geological
Survey (USGS) map has a scale of 1:24,000, it means that
one inch on the map is equal to 24,000 inches (2000 feet
or 609.6 meters) in the real world. Your map's scale legend
will always be at the bottom.
For USGS topographic maps, 1:24,000 is the scale most
often used. Maps based on metric units use a scale of
1:25,000, where one centimeter equals 0.25 kilometers.
You'll find most of the United States mapped at the
1:24,000 scale, with only a few exceptions. Puerto Rico, for
example, maps at 1:20,000 or 1:30,000 because the
country originally mapped at a metric scale. A couple of
states map at 1:25,000, and most of Alaska (due to its
size) maps at 1:63,360. The more populated areas of
Alaska, though, map at the typical 1:24,000 or 1:25,000.
A 1:24,000 map is large and provides a lot of detail about
the area -- it will include buildings, campgrounds, ski lifts,
among other things. You may also see footbridges and
private roads on a map of this scale.
It requires about 57,000 maps at this scale to cover the 48
contiguous United States, Hawaii and territories [source:
USGS]. However, you can find maps of various areas at all
different scales. The scale corresponds to its intended use.
For example, township engineers generally need extremely
detailed maps that show sewers, power and water lines,
and streets. The common scale for these maps is 1:600. If
you want to see one large area on a single sheet but with
less detail, a smaller scale map like 1:250,000 is better.