MODULE 1 CE 214 Fundamentals of Surveying
MODULE 1 CE 214 Fundamentals of Surveying
MODULE 1 CE 214 Fundamentals of Surveying
1. Topic
1. Introduction to Surveying
• What is surveying
• Functions of surveying
• Importance of surveying
• Objectives of surveying
• Uses of surveying
• General principles of surveying
2. Introduction
This module introduces the basics of surveying, its origin, concepts and
principles, thus, giving the students a foresight of the subject.
3. Learning Outcome
1. Students will be able to understand the importance of surveying.
2. Students will know the usage of surveying in real life.
3. Students will know the different disciplines and practices on different types
of survey.
4. Learning Content
What is surveying
Surveying
Surveying is the art and science of determining angular and linear measurements to
establish the form, extent, and relative position of points, lines, and areas on or near
the surface of the earth or on other extraterrestrial bodies through applied mathematics
and the use of specialized equipment and techniques. (Juny Pilapil La Putt)
Surveying is the art and science of civil engineering that determines the relative
(comparable) position of points on, above or beneath the surface of the Earth by
measuring the horizontal and vertical distances, angles, elevations and taking the
details of these points and by preparing a map or plan to any suitable scale.
(civilplanet.com)
For instance, if we are talking about our position in a hill station, we say we are at 3000
feet above mean sea level (vertical distance). When talking about our position in a city,
we refer to some landmarks near us (Horizontal distance).
Likewise, surveying identifies the position of points on or below the Earth’s surface by
referring to known points, such as benchmarks.
The data measurements gathered from surveying helps establish the plan
and design of all civil engineering projects such as tunneling, irrigation,
dams, reservoirs, waterworks, sewerage works, building, roads, bridges,
railways, irrigation canals, reservoirs etc.
During the project execution, any proposed structure is constructed along
the lines and points established by surveying (boundaries).
Surveying helps calculate the project’s possible alignment and the required
amount of earthwork. Example is in alignment of roads in cuts and backfills
in mountains and depressions and in the design of super elevation.
Surveying helps to assess the high-risk areas and hazards of a project.
Example is in identification and mapping of high-risk areas and hazards
(hazard maps).
Surveying helps to prepare the measurement data such as topography of
the site, adjacent structures, locations and sources available to kick-start the
architectural design conceptualization. (Project proposals and feasibility
studies)
Surveying helps to know the accurate soil profile, establish drainage paths,
and prepare contour surveys.
Surveying prepares the plan and map of an area occupied by the project,
also known as boundaries (legal boundaries).
Surveying helps to establish control points (benchmark)
Surveying helps to determine the economic feasibility by avoiding errors
during execution, saving time and money for an efficient project.
Surveying helps to fix national and state boundaries.
Surveying determines the required land acquisition.
Surveying helps to chart coastlines, navigable streams and lakes.
Surveying helps prepare a topographic map of the Earth’s land surface.
Surveying in road construction helps to identify the right location for the road
works along with optimal curve placements, materials, and methods to be
used.
Surveying in town planning determines the flexible land zone that is easy to
build in the construction, roads, railways, cable, drinking water plans, etc.
Even though the result of surveying supports the execution of the project,
we can quickly identify the hindrances at the earliest. (civilplanets.com)
Objective of surveying
Uses of surveying
Before starting any civil engineering work, regardless of branches, horizontal, vertical,
and angular measurements of the project (plan or map) is required.
Surveying is used in many branches according to the need. The following are the
primary uses of surveying.
Surveying is used to prepare Topographic maps, which represent the
accurate graphic representations of features on the Earth, such as rivers,
streams, lakes, woods, valleys, hills, towns, villages, forests, contours and
cliffs, and depressions.
Surveying is used to prepare Engineering maps representing the details of
engineering works such as dams, buildings, railways, road work, irrigation
canals, reservoirs, and transmission lines.
Surveying is used to prepare Cadastral maps representing the land
boundaries (property lines) and houses for legal purposes.
Surveying is used to prepare Military maps representing the road and
railway communications with different parts of a country and different
strategic points essential for the defense of a country.
Surveying is used in Urban Planning which helps to plan/locate the large-
scale extensions of the existing facilities such as streets, water supply,
sewer systems, and the layout of new roads.
Surveying is used to prepare Contour Maps representing the capacity of
reservoirs and the best possible transportation routes.
Surveying prepares Hydrographic Maps, which help plan navigation routes
on water bodies, water supply, and harbors or determine mean sea level.
Surveying is used to prepare Geological Maps, which help to determine the
different strata in the Earth’s crust.
Surveying is used to prepare Archaeological Maps, which help unearth
relics of antiquity.
Surveying is used in Astronomical Survey, which helps to determine the
latitudes and longitudes of any points on the Earth. It helps study planets’
movements and calculates local and standard times.
Surveying is used in Mining which helps to explore the minerals under the
Earth. (civilplanet.com)
From the above picture, C is new, which has to be fixed & point A, B are the given
point.
Now the point C can be fixed by measuring the distance of AC & BC; it is
one method of process.
A perpendicular line may be drawn from point C to baseline AB. Now we
have got two different possibilities to locate point C by the line CD.
(civilplanet.com)
Plane Surveying
In surveying, when the earth’s surface is assumed to be a plane, and the curvature of
the earth is omitted, it is called Plane Surveying.
The line connecting any two points is considered a straight line, and the
angle between any two lines is viewed as the plane’s angle. Any triangle
made by the plane survey is also called a plane triangle.
The Plane surveying method is suitable for surveying up to 250 km2 area.
The plane surveying methods are used in the construction of dams, bridges
& road work.
Geodetic Surveying
The earth’s surface is not considered as plane and curvature of the planet also taken
into account for measurement is called Geodetic Surveying.
The line joining 2 points will be The line joining 2 points will be
considered as a straight line. considered as a curved line.
The triangle formed by 3 points will be The triangle formed by 3 points will be
considered as a plane triangle. considered as a spherical triangle.
Classification of Surveying
The classification of surveying is dependent on the nature of the field, objective &
instruments.
Tacheometric Surveying
The tachymetric survey is used mainly in contour surveying.
The measurement of the distance can be taken in both horizontal & vertical
directions. The stadia distance and reduced level will be calculated for the distance
of the points.
Dumpy Level or Auto Level
The dumpy level or auto level instrument survey is mostly used where the earth’s
surface is uneven. The measurement can be measured in a 360-degree horizontal
direction.
The reduced level points are calculated by the height of the collimation or by the rise
and fall method.
Aerial Surveying
To discover the overview of an area, aerial surveying is carried out from the aeroplane
or helicopter. The photographs will be taken from an elevated position to identify the
object clearly from the top angle.
Total Station
The technology improvement of theodolite is a total station.
The total station is an electronic instrument that is mostly preferred for surveying at
present. The measurement of distances and angles are recorded in the device and can
quickly get the result through a computer. (civilplanets.com)
1. Astrolabe. The astrolabe of Hipparchus is considered to be one of the best known of the
measuring instruments that have come down from ancient times. It was developed sometime in
140 B.C., and further improved by Ptolemy. The instrument had a metal circle with a pointer
hinged at its center and held by a ring at the top, and a cross staff, a wooden rod about 1.25
meters long with an adjustable cross arm at right angles to it. The known length of the arms of the
cross staff allow distances and angles to be determined by proportion. It was originally designed
for determining the altitude of stars.
2. Telescope. The invention of the telescope in. 1607 is generally accredited to Lippershey. In
1609, Ga1ileo constructed a refracting telescope for astronomical observations. However, it was
only when cross hairs for fixing the line of sight were introduced, that the telescope was fixed in
early surveying instruments.
3. Transit. The invention of the transit is credited to Young and Draper who worked
independently from each other sometime in 1830. Both men were able to put together in one
instrument the essential parts of what has long been known as the universal surveying
instrument.
4. Semicircumferentor. An early surveying instrument which was used to measure and layoff
angles, and establish lines of sight by employing peep sights.
5. Plane Table. One of the oldest types of surveying instruments used in field mapping. It
consists of a board attached to a tripod in such a way that it can be leveled or rotated to any
desired direction.
6. Dioptra. The dioptra, which was perfected by Heron of Alexandria, was used in leveling and for
measuring horizontal and vertical angles. It consists essentially of a copper tube supported on a
stand and could be rotated in either a horizontal or vertical plane. For measuring horizontal
angles, a flat circular disc with graduations in degrees is used. An arm containing sighting
apertures at either end could be rotated to any desired position on the disc.
7. Roman Groma. The Roman surveyors used the groma instrument for aligning· or sighting
points. It consisted basically of cross arms fixed at right angles and pivoted eccentrically upon a
vertical staff. Plumb lines were suspended from the ends of the arms. By employing the groma
two lines at right angles to each other could be established on the ground where it is set up.
8. Libella. The Assyrians and Egyptians are believed to be the first users of the libella. The
instrument had an A-frame with a plumb line suspended from its apex and was used to determine
the horizontal. Archeologists are of the belief that the horizontal foundations of the great pyramids
of Egypt were probably defined by this device.
http://blog.oldwolfworkshop.com/2011/04/exploring-libella.html
9. Vernier. The vernier is a short auxiliary scale placed alongside the graduated scale of an
instrument, by means of which fractional parts of the smallest or least division of the main scale
can be determined precisely without having to interpolate. It was invented in 1631 by a
Frenchman name Pierre Vernier. Surveying instruments employ either a direct or retrograde
vernier.
10. Diopter. An instrument developed by the Greeks sometime in 130 B.C., and known to be their
most famous surveying instrument. The diopter was used for leveling, laying off right angles, and
for measuring horizontal and vertical angles. Since the telescope was not yet invented during the
time the diopter was used, peep sights were employed for sighting and in aligning the device.
https://en.wikipedia.org/wiki/Dioptra
11. Compass. The magnetic compass came into wide use during the 13th century for
determining the direction of lines and in calculating angles between lines. It was first introduced
for use in navigation. The compass consists of a magnetized steel needle mounted on a pivot at
the center of a graduated circle. The needle continues to point toward magnetic north and gives a
reading which is dependent upon the position of the graduated circle.
12. Gunter"s Chain. The Gunter's chain, which was invented by Sir Edmund Gunter in 1620,
was the forerunner of instruments used for taping distances. It is 66 ft long and contains 100
links, so that distances may be recorded in chains and in decimal parts of the chain. Each part,
called a link, is 0.66 ft or 7.92 inches long.
13. Chorobates. This instrument was designed for leveling work. It consisted of a horizontal
straight-edge about 6 meters long with supporting legs, and a groove 2.5 cm deep and,
1.5m long on top. Water is poured into the groove and when the bar is leveled so that
water stood evenly in the groove without spilling, a horizontal line is established.
http://www.romanaqueducts.info/aquasite/foto/lijntekchorobates.jpg
14. Merchet. The merchet was a device for measuring time and meridian. It was first used by the
Chaldeans in about 4,000 B.C. It consisted of a slotted palm leaf through which to sight and a
bracket from which a plumb bob was suspended. -By sighting through the 'slot and past the
plumb bob string, a straight line could be projected.
http://surveytypes.blogspot.com/2008/01/surveying-instruments-were-developed.html
Surveying measurements
A measurement is the process of determining the extent, size or dimensions of a
particular quantity in comparison to a given standard. In surveying, measurements may
be made directly or indirectly.
1. Direct measurements. A direct measurement is a comparison of the
measured quantity with a standard measuring unit or units employed for
measuring a quantity of that kind.
2. Indirect measurements. When it is not possible to apply a measuring
instrument directly to a quantity to be measured an indirect measurement
is made.
The meter
The international unit of linear measurement is the meter. This was proposed sometime
in 1789 by French scientists who hoped to establish a system suitable for all times and
all peoples, and which could be based upon permanent natural standards. Originally,
the meter was defined as 1/10 millionth of the earth’s meridional quadrant. In May 20,
1875, the meter was defined as the distance between two lines engraved across the
surface (near the ends) of a bar with an X-shaped cross-section, composed of 90%
platinum and 10% iridium, when the temperature of the bar is 0 degree Celsius.
In October 1960, the meter was redefined as a length equal to 1,650,763.73
wavelengths of the orange-red light produced by burning the element krypton (with an
atomic weight of 86) at a specified energy level in the spectrum.
Units of measurement
Common prefixes in SI units are listed below;
Mega- = 1,000,000 kilo- = 1,000 hecto- = 100 deca- = 10
Deci- = 0.1 centi- = 0.01 milli- = 0.001 micro- = 0.000 001
Nano- = 0.000 000 001
2. Angular Measurements.
The SI unit for plane angles is the radian. The radian is defined as an
angle subtended by an arc of a circle having a length equal to the radius
of the circle. 2 rad = 360 degrees, 1 rad = 57 degrees 17 minutes and
44.8 seconds or 57.2958 degrees.
a. Sexagesimal units – the sexagesimal units of angular measurement
are the degree, minute, and second. The unit of angle used in
surveying is the degree which is defined as 1/360 th of a circle. One
degree equals 60 minutes, and 1 minute equals 60 seconds.
b. Centesimal units – in this system, the circumference of a circle (360
degrees) is divided into 400 grads. The grad is divided into 100
centesimal minutes or 0.9 degrees and the minutes is subdivided
into 100 centesimal seconds or 0 deg 00 minutes 32.4 seconds.
Grads are usually expresses in decimals, for example, 194g 45c
82cc is expressed as 194.458 2 grads.
Significant Figures
By definition, the number of significant figures in any value includes the number of
certain digits plus one digit that is estimated and, therefore, questionable or
uncertain. For example, a line that is measured with a scale graduated in one
meter increments and recorded as 3.6 meters, the value has two significant
figures, 3 is the certain number and 6 is the estimated. If the same line is again
measured with a scale graduated in tenths of a meter and recorded with three
significant figures as 3.65 meters, the 3 and 6 are certain whereas 5 is estimated
or uncertain.
Rule 2. For values less than one, zeroes immediately to the right of the decimal
are not significant, they merely show the position of the decimal such as in the
following values which contain three significant figures; 0.00325, 0.000468, and
0.0230.
Rule 3. Zeroes placed at the end of decimal numbers are significant such as
169.30, 366.00, and 11.000. These values all have five significant figures.
Examples:
1. One significant figure
100 9 0.001
400 8000 0.000005
2. Two significant figures
24 0.020 0.0024
0.24 0.000065 3.6
3. Three significant figures
365 3.65 0.000249
12.3 10.1 0.0120
4. Four significant figures
7654 0.8742 0.00006712
32.25 15.00 364.0
5. Five significant figures
12345 100.00 40.000
0.86740 46.609 155.28
Types of notes
1. Sketches. A good sketch will help to convey a correct impression.
Sketches are rarely made to exact scale, but in most cases they are made
approximately to scale. They are drawn freehand and of liberal size. Many
features may be readily shown by conventional symbols. Special symbols
may be adapted for the particular organization or job. The student should
note that a sketch crowded with unnecessary data is often confusing.
2. Tabulation. A series of numerical values observed in the field are best
shown in tabulated format. Tabular forms prevents mistakes, allows easy
checking, saves time, makes the calculation legible to others, and
simplifies the work of the person checking the field notes.
3. Explanatory notes. Explanatory notes provide a written description of
what has been done in the field. These are employed to make clear what
the numerical data and sketches fail to do. Usually, they are placed on the
right- hand page of the field notebook in the same line with the numerical
data that they explain. If sketches are used, the explanatory notes are
placed where they will not interfere with other data and as close as
possible to that which they explain.
4. Computations. The portrayal of calculations should be clear and orderly
in arrangement in order that these will easily be understood by persons
other than the one who made the computations.
5. Combination of the above. The practice used in most extensive surveys
is a combination of the above types of notes. The surveyor should be able
to determine which type of combination would be most logical to use in
portraying the type of data gathered in the field.
Information found in the field notebooks
1. Title of the field work or name of project. The official name of the
project or title of the field work should always be identified. The location of
the survey and preferably its nature or purpose should always be stated.
2. Time of day and date. These entries are necessary to document the
notes and furnish a timetable as well as a reference for precision,
problems encountered and other factors affecting the survey.
3. Weather conditions. Temperature, wind velocity, typhoons, storms and
other weather conditions such as fog, sunshine and rain have an effect on
accuracy in surveying operations.
4. Name of group members and their designations. The chief party,
instrumentman, tapeman and other members of the survey party must be
identified. This information will be necessary for documentation purposes
and other future reference. From this information, duties and
responsibilities can easily be pinpointed among the survey party
members.
5. List of equipment. All survey equipment used must be listed, including its
make, brand, and serial number. The type of instrument used and its
adjustment all have a definite effect on the accuracy of a survey. Proper
identification of the particular equipment used helps in isolating errors in
some cases.
Errors
An error is defined as the difference between the true value and the measured value of
a quantity. Errors are inherent in all measurements and result from sources which
cannot be avoided. They may be caused by the type of equipment used or by the way in
which the equipment is employed. It may also be caused by the imperfections of the
senses of the person undertaking the measurement or by natural causes. The effects of
errors cannot be entirely eliminated; they can, however, be minimized by careful work
and by applying corrections.
Mistakes
Mistakes are inaccuracies in measurements which occur because some aspect of a
surveying operation is performed by the surveyor with carelessness, inattention, poor
judgement and improper execution. Mistakes are also caused by a misunderstanding of
the problem, inexperience, or indifference of the surveyor. A large mistake is referred to
as a blunder. Mistakes and blunders are not classified as errors because they usually
are so large in magnitude when compared to errors.
Among students of surveying mistakes which are frequently committed include; reading
the wrong graduation on the tape, omitting whole length of tape, transposition of figures,
reading a scale backward, misplacing a decimal point, incorrect recording of field notes,
adding a row or column of numbers incorrectly, etc.
Types of errors
1. Systematic errors. This type of error is one which will always have the
same sign and magnitude as long as field conditions remain constant and
unchanged. For instance, in making a measurement with a 30m tape
which is 5 cm too short, the same error is made each time the tape is
used. If a full tape length is used six times, the error accumulates and
totals six times the error (or 30 cm) for the total measurement. It is for this
reason that this type of error is also called a cumulative error. Such errors
can be computed and their effects eliminated by applying corrections,
employing proper techniques in the use of instruments, or by adopting a
field procedure which will automatically eliminate it.
2. Accidental errors. These errors are purely accidental in character. The
occurrence of such errors are matters of chance as they are likely to be
positive or negative, and may tend in part to compensate or average out
according to laws of probability. There is no absolute way of determining
or eliminating them since the error for an observation of a quantity is not
likely to be the same as for a second observation. An example of such an
error is the failure of the tapeman to exert the correct amount of pull on the
ends of a tape during measurement. Another example is in the reading of
an angle with a transit. Since the instrumentman cannot read it perfectly,
there would be times when he would read a value which is too large and in
another instance he may read a value too small.
In comparison to systematic errors, accidental errors are usually of minor
importance in surveying operations since they are variable in sign and are
of a compensating nature.
Sources of errors.
1. Instrumental errors. These errors are due to imperfections in the
instruments used, either from faults in their construction or from improper
adjustments between the different parts prior to their use. Examples of
instrumental errors are;
Measuring with a steel tape of incorrect length.
Using a leveling rod with painted graduations not perfectly spaced.
Determining the difference in elevation between two points with an
instrument whose line of sight is not in adjustment.
Sighting on a rod which is warped.
Improper adjustment of the plate bubbles of a transit or level.
2. Natural errors. These errors are caused by variations in the phenomena
of nature such as changes in magnetic declination, temperature, humidity
wind refraction, gravity and curvature of the earth. The surveyor may not
be able to totally remove the cause of such errors but he can minimize
their effects by making proper corrections of the results and using good
judgment. Common examples are;
The effect of temperature variation on the length of a steel tape.
Error in the readings of the magnetic needle due to variations in
magnetic declination.
Deflection of the line of sight due to the effect of the earth’s
curvature and atmospheric refraction.
Error in the measurement of a line with a tape being blown sidewise
by a strong wind.
Error in the measurement of a horizontal distance due to slope or
uneven ground.
3. Personal errors. These errors arise principally from limitations of the
senses of sight, touch and hearing of the human observer which are likely
to be erroneous or inaccurate. Typical of these errors are;
Error in determining a reading on a rod which is out of plumb during
sighting.
Error in the measurement of a vertical angle when the cross hairs of
the telescope are not positioned correctly on the target.
Making an erroneous estimate of the required pull to be applied on
a steel tape during measurement.
Precision refers to the degree of refinement and consistency with which any
physical measurement is made.
https://www.antarcticglaciers.org/glacial-geology/dating-glacial-sediments-2/
precision-and-accuracy-glacial-geology/
Theory of probability.
Probability is defined as the number of times something will probably occur over
the range of possible occurrences. In dealing with probability, it is assumed that
we refer principally only to accidental errors and that all systematic errors and
mistakes have been eliminated.
The theory of probability is based upon the following assumptions relative to the
occurrence of errors:
1. Small errors occur more often than large ones and that they are more
probable.
2. Large errors happen infrequently and are therefore less probable; for
normally distributed errors unusually large ones may be mistakes rather
than accidental errors.
3. Positive and negative errors of the same size happen with equal
frequency; that is, they are equally probable.
4. The mean of an infinite number of observations is the most probable
value.
x
mpv=Σ
n
where mpv is the most probable value, Σ x is the sum of the individual
measurements, and n is the total number of observations made.
Illustrative examples:
1. A surveying instructor sent out six groups of students to measure a
distance between two points marked on the ground. The students came
up with the following six different values: 250.25, 250.15, 249.90, 251.04,
250.50, and 251.22 meters. Assuming these values are equally reliable
and that variations result from accidental errors, determine the most
probable value of the distance measured. (250.51 m)
2. The angles about a point Q have the following observed value.
130º15’20”, 142º37’30”, and 87º07’40”. Determine the most probable
value of each angle. (130º15’10”, 142º37’20”, and 87º07’30”)
Residual.
The residual is referred to as the deviation, is defined as the difference between
any measured value of a quantity and its most probable value.
v=x−X
where v is the residual in any measurement, x is a measurement made of a
particular quantity, and X is the most probable value of the quantity measured.
Residuals and errors are theoretically identical. The only difference is that
residuals can be calculated whereas errors cannot because there is no way of
knowing true values.
Probable error.
The probable error is a quantity which, when added to and subtracted from the
most probable value, defines a range within which there is a 50 percent chance
that the true value of the measured quantity lies inside (or outside) the limits thus
set.
If errors are arranged in order of magnitude, it will be possible to determine the
probable error. This is the error that would be found in the middle place of the
arrangement, such that one half of the errors are greater than it and the other half
are less than it.
PEs =±0.6745
√ ∑ v2
(n−1)
PEm=± 0.6745
√ ∑ v2
n(n−1)
The determination and use of the probable error in surveying is primarily to give an
indication of the precision of a particular measurement. For example, if 235.50 m
represents the mean or most probable value of several measurements and 0.10 m
represents the probable error of the mean value, the chances are even that the
true value lies between 235.40 m and 235.60 m, as it is also probable that the true
value lies outside of these limiting values. To express the probable limits of
precision for this particular case, the quantity should be written as 235.50 ±0.10 m.
Interrelationship of errors
In some instances it is required to determine how the final result is affected when a
computation involves quantities that are subject to accidental errors. Two
commonly applied principles of the theory of errors involve the summation of errors
and the product of errors. These principles are given to provide the student a
better understanding of the propagation of errors.
1. Summation of errors. If several measured quantities are added, each of
which is affected by accidental errors.
PEs =± √ PE21 + PE22+ PE 23+ ….. PE2n
Where: PEs = probable error of the sum
PE 1 , PE 2 , etc = probable error of each measurement
n= number of values added
Illustrative examples:
1. The following values were determined in a series of tape measurements of a
line: 1000.58 ,1000.40, 1000.38, 1000.48, 1000.40, and 1000.46 meters.
Determine the following:
a. Most probable value of the measured length (1000.45 m)
b. Probable error of a single measurement and probable error of the mean (
± 0.05029 ¿, (± 0.02053 ¿
c. Final expression for the most probable length (1000.45 ± 0.02053 ¿
d. Relative precision of the measurement ( RPs=0.05/1000.45 ¿, (
RP m=0.02 /1000.45 ¿
5. The length of a line was measured repeatedly on three different occasions and
the probable error of each mean value was computed with the following results:
st
1 set of measurements = 1201.5 ±0.02 m
2nd set of measurements = 1201.45 ±0.04 m
3rd set of measurements = 1201.62 ±0.05 m
Determine the weighted mean of the three sets of measurements. (1201.50 m)
6. The three sides of a triangular-shaped tract of land are given by the following
measurements and corresponding probable errors: a = 162.54 ±0.03 m, b =
234.26 ±0.05 m, and c = 195.70 ±0.04 m. Determine the probable error of the
sum and the most probable value of the perimeter. (±0.07), (592.50 ±0.07 m)
7. The two sides of a rectangular lot were measured with certain estimated
probable errors as follows: W = 253.36 ±0.06 m and L = 624.15 ±0.08 m.
Determine the area of the lot and the probable error in the resulting calculation.
(±42.58 square meters), (158134.64 ±42.58 square meters)
5. References
1. La Putt, J.P., Elementary Surveying (3rd Edition) 2013 Reprint
2. https://civiltoday.com/surveying/86-objectives-of-surveying
3. https://www.britannica.com/technology/surveying
4. https://civilplanets.com/uses-of-surveying