f2
2f2
3f2
½f
A. f2
λ = α
λ = 90° - α
λ = α - 90°
λ = 180° - α
The area is divided into triangular figures
Control stations are located from which detailed surveys are carried out
Sides are not measured excepting the base line
All the above
When its altitude is maximum
When its azimuth is 180°
When it is in south
All the above
Positive for points above datum
Negative for points below datum
Zero for points vertically below the air station
All the above
80°
70°
60°
50°
Ursa Minor's remains always north of pole star
Polar star remains always north of Polaris
Polaris remains always north of Ursa Minor's
Ursa Minor's pole star and Polaris are the names of the same star
sin α = sin φ cosec δ
sin α = sin φ sec δ
sin α = cos φ sec δ
sin α = cos φ cosec δ
Isocenter
Principal point
Perspective centre
Plumb line
Satellite station
Subsidiary station
Pivot station
Main station
East of observer
West of observer
North of observer
South of observer
The standard meridian
The international date line
That of Greenwich
Both (a) and (c) of above
Greater than the longitude of the place
Less than the latitude of the place
Equal to the latitude of the place
None of these
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
Standard meridian
Greenwich meridian
Equator
180° longitude
1/3
1/2
3/4
5/4
Principal point coincides the isocenter
Iso-centre coincides the plumb point
Plumb point coincides the principal point
All the above
500 m
1000 m
1500 m
2000 m
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
58 mm
60 mm
62 mm
64 mm
Principal distance
Principal line
Isocentric distance
Focal length
S - 90°
S - 180°
S - 270°
S - 360°
δ - θ
θ - δ
θ + δ
(θ + δ)/2
30°
35°
40°
45°
cos δ/cos λ
cos (90° - δ)/cos (90° - λ)
sin (90° - δ)/sin (90° - λ)
tan (90° + δ)/tan (90° + λ)
Ground elevation
Flying height
Length of air base
All the above
sin z = sec φ . cos δ
cos z = sec φ . cos δ
tan z = sec φ . cos δ
None of these
Vernal equinox
Autumnal equinox
Summer solstice
Winter solstice
f sin θ
f cos θ
f tan θ
f sec θ
Reduction to mean sea level
Correction for horizontal alignment
Correction for slope
All the above
Mean sun
True sun
Vernal equinox
All the above