Standard meridian
Greenwich meridian
Equator
180° longitude
D. 180° longitude
Principal point
Isocenter
Plumb point
Perspective centre
Parallel lines do not appear parallel in central projection
The two sides of a road meet at the vanishing point
The lines parallel to the negative plane are projected as parallel lines
All the above
30°
35°
40°
45°
Astronomical latitude
Astronomical longitude
Astronomical bearing
All of these
1°
2°
3°
4°
One minute arc of the great circle passing through two points
One minute arc of the longitude
1855.109 m
All the above
Eastward
Westward
Northward
Southward
At culmination
At elongation
Neither at culmination nor at elongation
Either at culmination or at elongation
The measured stereoscopic base of photographs is obtained by dividing the air base in metres by the mean scale of the photograph
The difference between the absolute parallax of two points depends upon the difference in their elevations
The line joining the principal point of a photograph and the transferred principal point of the adjoining photograph, is called stereoscopic base
All the above
δ - θ
θ - δ
θ + δ
(θ + δ)/2
Equator
Horizon
Pole
None of these
cos H = tan λ/tan δ
sin α = sin λ/sin δ
sin A = cos δ/cos λ
All the above
Parallel projection
Orthogonal projection
Central projection
None of these
1 : 10,000
1 : 15,000
1 : 20,000
1 : 30,000
f/H sec θ
f sec θ/H
f/H
f/H cos ½θ
Tension = (P - Ps)L/AE
Sag = L3w²/24P² where w is the weight of tape/m
Slope = (h²/2L) + (h4/8L3) where h is height difference of end supports
All the above
Visible horizon
Sensible horizon
Celestial horizon
True horizon
365
365.2224
365.2422
366.2422
Opposite corners of a photograph
Nodal points of the camera lens
Corresponding points on the ground and photograph
Plumb points of stereo pair of photographs
Nadir
Isocenter
Principal point
Plumb point
5100 nautical miles
5700 nautical miles
120 nautical miles
500 nautical miles
When the star momentarily moves vertically
When the angle at the star of the spherical triangle is 90°
When the star's declination is greater than the observer's latitude
All the above
Altitude and azimuth system
Declination and hour angle system
Declination and right ascension system
Declination and altitude system
Eastward
Westward
Northward
Southward
Aerial photographs may be either vertical or oblique
Vertical photographs are taken with the axis of camera pointing vertically downward
Vertical photographs are used for most accurate maps
All the above
March 21 to June 21
June 21 to September 21
September 21 to December 21
Both (a) and (b) of above
29 days
29.35 days
29.53 days
30 days
50 %
60 %
70 %
75 %
sin α = sin φ cosec δ
sin α = sin φ sec δ
sin α = cos φ sec δ
sin α = cos φ cosec δ
fB/(H - h)
fB/(H - h)2
fB/(H + h)
fB/(H + h)2