10° N
50° N Latitude
Equator
5° S latitude
D. 5° S latitude
Equator
Celestial equator
Ecliptic
None of these
Positive for points above datum
Negative for points below datum
Zero for points vertically below the air station
All the above
The east point of the horizon
The west point of the horizon
The zenith point of the observer
All the above
θ = z + δ
θ = δ - z
θ = 180° - (z + δ)
θ = (z + δ) - 180°
f/H sec θ
f sec θ/H
f/H
f/H cos ½θ
Photo plumb point
Plumb point
Nadir point
Isocenter
The plane passing through the perspective centre of a stereo pair and a ground point, is known as basal plane
Each pair of image points on stereo pair have their own basal plane
Relative orientation means reconstructing the basal plane
All the above
Satellite station
Eccentric station
False station
Pivot station
The star's movement is apparent due to the actual steady rotation of the earth about its axis
The stars move round in circular concentrated parts
The centre of the circular paths of stars is the celestial pole
All the above
Gauss' Mid Latitude formula
D'Alembert's method
Legendre's method
Least square method
2 mm
4 mm
6 mm
10 mm
Ground principal point
Ground plumb point
Iso-centre
Perspective centre
Optical projection
Optical mechanism projection
Mechanical projection
All the above
Eastward
Westward
Northward
Southward
North end of the polar axis is known as North Pole
South end of the polar axis is known as South Pole
Point where polar axis when produced northward intersects the celestial sphere, is known as north celestial pole
All the above
Meridian
Vertical circle
Prime vertical
None of these
Correction for refraction is always negative
Correction for parallax is always positive
Correction for semi-diameter is always negative
Correction for dip is always negative
1 cm
2 cm
3 cm
4 cm
High oblique
Low oblique
Vertical
None of these
0.1 mm
0.5 mm
1.00 mm
1.1 mm
fB/(H - h)
fB/(H - h)2
fB/(H + h)
fB/(H + h)2
1 : 10,000
1 : 15,000
1 : 20,000
1 : 30,000
5100 nautical miles
5700 nautical miles
120 nautical miles
500 nautical miles
Northward
Southward
From south to north of the equator
From north to south of the equator
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
50 %
60 %
70 %
75 %
sin c sin B
cos c cos B
tan c tan B
sin c cos B
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
Vernal equinox
Autumnal equinox
Summer solstice
Winter solstice
When its altitude is maximum
When its azimuth is 180°
When it is in south
All the above