S - 90°
S - 180°
S - 270°
S - 360°
B. S - 180°
H. f
H/f
f/H
H + f
58 cot α
58 tan α
58 sin α
58 cos α
- 8.8 cos α
+ .8 sin α
+ 8.8 cos α
- 8.8 cos α
24 hours 10 minutes
20 hours 25 minutes
24 hours 50 minutes
23 hours 50 minutes
At culmination
At elongation
Neither at culmination nor at elongation
Either at culmination or at elongation
Eastward
Westward
Northward
Southward
Eastward
Westward
Northward
Southward
Latitudes north of the equator are taken as positive
Latitudes south of the equator are taken as negative
Longitudes east of Greenwich are taken as negative
Longitudes west of Greenwich are taken as positive
The horizontal direction of the pole is called astronomical north
The angle between the direction of true north and the direction of a survey line is called astronomical bearing
The astronomical bearing is generally called azimuth
All the above
Positive for points above datum
Negative for points below datum
Zero for points vertically below the air station
All the above
Parallel projection
Orthogonal projection
Central projection
None of these
Gauss' Mid Latitude formula
D'Alembert's method
Legendre's method
Least square method
Do not follow any definite mathematical law
Cannot be removed by applying corrections to the observed values
Are generally small
All the above
Observation equation
Conditional equation
Normal equation
None of these
λ = α
λ = 90° - α
λ = α - 90°
λ = 180° - α
Meridian
Vertical circle
Prime vertical
None of these
Control points for surveys of large areas
Control points for photogrammetric surveys
Engineering works, i.e. terminal points of long tunnels, bridge abutments, etc.
All the above
Satellite station
Subsidiary station
Pivot station
Main station
Parallel to the principal line
Perpendicular to the principal line
Along the bisector of the angle between the principal line and a perpendicular line through principal plane
None of these
Vernal equinox
Autumnal equinox
Summer solstice
Winter solstice
One degree of longitude has greatest value at the equator
One degree of longitude has greatest value at the poles
One degree of longitude has the same value everywhere
One degree of latitude decreases from the equator to the poles
f sin θ
f cos θ
f tan θ
f sec θ
Refraction correction is zero when the celestial body is in the zenith
Refraction correction is 33' when the celestial body is on the horizon
Refraction correction of celestial bodies depends upon their altitudes
All the above
sin α = sin φ cosec δ
sin α = sin φ sec δ
sin α = cos φ sec δ
sin α = cos φ cosec δ
Sidereal time at any instant is equal to the hour angle of the first point of Aries
Local sidereal time of any place is equal to the right ascension of its meridian
Sidereal time is equal to the right ascension of a star at its upper transit
All the above
1°
2°
3°
4°
When its altitude is maximum
When its azimuth is 180°
When it is in south
All the above
Is the period of time taken by the earth in making a complete rotation with reference to stars
Is slightly shorter than an ordinary solar day
Is divided into the conventional hours, minutes and seconds
All the above
The sun's right ascension increases for 0 h to 24 h when it returns to the First point of Aries
The maximum declination of the sun increases up to 23 ½° N on about 21st June
The minimum declination of the sun is zero' on 22nd September
All the above
58 mm
60 mm
62 mm
64 mm