Surveying MCQ Practice Set — 50 Questions with Answers
50 exam-oriented Surveying multiple-choice questions with the correct answer and a clear explanation for each. Frequently asked in AE Level Civil Engineering, JE Level Civil Engineering. Solve the full set below for free — no login required.
- 1SurveyingMEDIUM
A 'Digital Elevation Model' (DEM) is used in GIS for:
AOnly road network dataBTerrain analysis: slope, watershed delineation, viewshed, flood mapping, earthwork volumes — derived from elevation gridCAttribute data tables onlyDOnly underground utilities mappingAnswer: B. Terrain analysis: slope, watershed delineation, viewshed, flood mapping, earthwork volumes — derived from elevation grid
Explanation: DEM: raster representation of terrain elevation (one elevation value per grid cell). Applications: (1) Slope and aspect maps; (2) Watershed delineation (flow direction, flow accumulation, stream network extraction); (3) Viewshed analysis; (4) Solar radiation modelling; (5) Volume calculation for earthworks; (6) Flood inundation mapping. Sources: SRTM (90/30m), ASTER (30m), LiDAR (< 1m), Cartosat DEM (30m).
- 2SurveyingMEDIUM
'Contour interval' selection for a topographic survey depends on:
AOnly the surveyors'' experienceBMap scale, terrain relief, and purpose — large scale detailed engineering survey uses small CI; small scale planning uses large CICNumber of available survey instrumentsDOnly the drawing paper sizeAnswer: B. Map scale, terrain relief, and purpose — large scale detailed engineering survey uses small CI; small scale planning uses large CI
Explanation: Contour interval CI = difference in elevation between successive contours. Selection factors: (1) Scale of map (smaller scale → larger CI); (2) Nature of terrain (hilly = large CI, flat = small CI); (3) Purpose (detailed engineering = small CI 0.5–1 m; planning = 5–10 m); (4) Resources (time and cost). Typical: 1:1000 flat = 0.5–1 m CI; 1:50,000 hilly = 20 m CI. Small CI = more detail but more fieldwork.
- 3SurveyingEASY
The 'EDM' (Electronic Distance Measurement) instrument measures distances using:
AChain and tape stretched between two pointsBPhase difference (or time-of-flight) of modulated electromagnetic wave — accuracy ±3 mm + 2 ppmCAcoustic/ultrasonic signals under waterDMagnetic field strength variationAnswer: B. Phase difference (or time-of-flight) of modulated electromagnetic wave — accuracy ±3 mm + 2 ppm
Explanation: EDM: measures distance by timing phase shift of modulated electromagnetic wave (carrier: infrared/laser for short range; microwave for long range through rain/fog). Distance = phase difference × modulation wavelength / (4π). Accuracy: ± (3 mm + 2 ppm × D). At D=1 km: accuracy ≈ ± 5 mm. Total station integrates EDM + theodolite. GNSS more accurate for longer distances but EDM used in precise construction layout.
- 4SurveyingMEDIUM
The 'photogrammetric control' (ground control points) in aerial survey are required for:
AOnly for taking photographs from aircraftBAbsolute orientation and georeferencing — known ground coordinates to convert model to real-world coordinate systemCMeasuring pilot''s flight pathDCalibrating the aircraft compassAnswer: B. Absolute orientation and georeferencing — known ground coordinates to convert model to real-world coordinate system
Explanation: Ground Control Points (GCPs): surveyed points on the ground with known X, Y, Z coordinates, identifiable on photos. Used for: absolute orientation of stereomodel (scaling, rotating, levelling the model to ground), georeferencing, orthorectification. Minimum 3–4 GCPs per stereomodel (for 6 exterior orientation parameters). With GNSS direct georeferencing: fewer GCPs needed. Accuracy of map = accuracy of GCPs.
- 5SurveyingMEDIUM
The 'photogrammetric stereomodel' from two overlapping aerial photos allows determination of:
AOnly 2D planimetric positions without heightB3D ground coordinates (X, Y, Z) from parallax between two overlapping photos — enables DEM and full mappingCOnly colour informationDWind speed at flight altitudeAnswer: B. 3D ground coordinates (X, Y, Z) from parallax between two overlapping photos — enables DEM and full mapping
Explanation: Stereoscopic model: two photos with overlap (endlap 60%, sidelap 30%) form stereomodel when viewed simultaneously. From parallax differences: 3D coordinates of ground points measurable. Output: DEM (Digital Elevation Model), orthophoto, planimetric map. Base-height ratio (B/H) determines height accuracy: Δh = H × Δp / (B) where Δp = parallax measurement error. Analytical photogrammetry → digital photogrammetry (SfM).
- 6SurveyingMEDIUM
The 'corrections' applied to measured chain/tape lengths include all EXCEPT:
ATemperature correction for thermal expansionBColour correction (no such correction exists in chain/tape surveying — this is a distractor)CSag correction for tape hanging between supportsDSlope correction to reduce inclined to horizontalAnswer: B. Colour correction (no such correction exists in chain/tape surveying — this is a distractor)
Explanation: Tape corrections applied: (1) Temperature correction (thermal expansion); (2) Pull (tension) correction (elastic stretch above/below standard); (3) Sag correction (tape sags under gravity — reduces measured length); (4) Slope correction (measured along slope, reduce to horizontal). NOT applied: Colour correction (no such thing in surveying). All corrections may be + or − depending on field condition vs standard.
- 7SurveyingMEDIUM
The 'levelling staff' reading is corrected for 'curvature and refraction' by the formula:
ACurvature correction alone 0.0785 D² without refractionBCombined C−R = 0.0673 D² (metres, D in km) — curvature raises apparent staff reading, refraction partially offsets itCNo correction needed for any distanceD0.0673 D (linear, not squared)Answer: B. Combined C−R = 0.0673 D² (metres, D in km) — curvature raises apparent staff reading, refraction partially offsets it
Explanation: Combined correction for curvature (C) and refraction (R): C−R = 0.0673 D² (metres) where D = distance in km (combined, net correction is positive — staff reading too high due to curved Earth minus refraction bending ray down). Curvature alone: 0.0785 D². Refraction correction: −0.0112 D². Net: 0.0673 D². Important for precise levelling over long sights (> 200 m). Eliminated by equal backsight and foresight lengths.
- 8SurveyingMEDIUM
In GIS, a 'raster' data model differs from a 'vector' model in that raster:
AOnly stores points, not areasBUses regular grid cells for continuous spatial data; vector uses points/lines/polygons for discrete featuresCCannot store elevation dataDCan only be used for road networksAnswer: B. Uses regular grid cells for continuous spatial data; vector uses points/lines/polygons for discrete features
Explanation: Raster: divides space into regular grid cells (pixels), each with attribute value. Good for: continuous data (DEM, satellite imagery, slope, rainfall). Resolution = cell size. Vector: represents features as points, lines, polygons with precise coordinates. Good for: discrete features (roads, buildings, boundaries). Raster: fast overlay analysis, requires more storage for fine resolution; Vector: compact, precise boundaries.
- 9SurveyingMEDIUM
'Structure from Motion' (SfM) photogrammetry using a drone (UAV) automatically produces:
AOnly 2D planimetric map without heightBDense 3D point cloud, DEM, and orthophoto automatically from overlapping drone photos — cm accuracy with GCPsCOnly video recording without measurementDThermal infrared images of groundAnswer: B. Dense 3D point cloud, DEM, and orthophoto automatically from overlapping drone photos — cm accuracy with GCPs
Explanation: SfM photogrammetry: drone captures overlapping photos from multiple viewpoints; software (Agisoft Metashape, Pix4D) automatically: (1) Extracts feature points (SIFT algorithm); (2) Matches across photos; (3) Computes camera positions (bundle adjustment); (4) Generates dense point cloud; (5) Creates DEM + orthophoto. With few GCPs: cm-level accuracy. Rapid, cost-effective replacement for manned aircraft survey for small areas.
- 10SurveyingMEDIUM
The 'Global Navigation Satellite System' (GNSS) positioning accuracy can be improved by:
AUsing only one satelliteBDGPS correction from reference station, RTK (cm accuracy), or dual-frequency for ionospheric correctionCTurning off atmospheric correctionsDReducing the number of visible satellitesAnswer: B. DGPS correction from reference station, RTK (cm accuracy), or dual-frequency for ionospheric correction
Explanation: GNSS accuracy improvement: (1) DGPS (Differential GPS): reference station computes correction; broadcasts to rover (sub-metre accuracy); (2) RTK (Real-Time Kinematic): carrier-phase corrections from base to rover by radio (centimetre accuracy); (3) PPP (Precise Point Positioning): global correction service (few cm); (4) SBAS (Satellite-Based Augmentation: GAGAN for India — 1–3 m); (5) Dual-frequency to correct ionospheric error.
- 11SurveyingEASY
The 'GLONASS' satellite navigation system is operated by:
AUSA (same as GPS)BRussia — GLONASS constellation, uses FDMA (different frequency per satellite) vs GPS''s CDMACEuropean Union (this is Galileo)DIndia (this is NavIC/IRNSS)Answer: B. Russia — GLONASS constellation, uses FDMA (different frequency per satellite) vs GPS''s CDMA
Explanation: GLONASS (Global Navigation Satellite System): Russian counterpart to US GPS. Operational from 1995. 24 satellites in 3 orbital planes. Frequency division multiple access (FDMA) — different frequency per satellite (vs GPS: CDMA — same frequency, different code). GNSS receivers often combine GPS + GLONASS for better availability. Other systems: Galileo (EU), BeiDou (China), NavIC/IRNSS (India — 7 satellites, South Asia coverage).
- 12SurveyingEASY
'Contour lines' on a topographic map cannot:
ARepresent uniform slope on a hillsideBTwo contours of different elevation values can never merge or cross (except at a vertical cliff shown by special treatment)CShow valleys as V-shapes pointing uphillDBe closely spaced for steep terrainAnswer: B. Two contours of different elevation values can never merge or cross (except at a vertical cliff shown by special treatment)
Explanation: Contour properties: (1) Each contour represents constant elevation; (2) Contours never cross each other (except overhanging cliff — shown dashed); (3) Closely spaced = steep slope; (4) Widely spaced = gentle slope; (5) V-shape pointing uphill = valley; V pointing downhill = ridge/spur. Contours CROSS at overhangs. Two different contours with different elevations NEVER merge on flat ground (would imply same elevation at two adjacent contour values).
- 13SurveyingMEDIUM
The 'NavIC' (Navigation with Indian Constellation) system covers:
AWorldwide coverage like GPSBIndia and surrounding region within 1500 km — 7-satellite regional system by ISRO with < 5 m accuracyCOnly 50 km radius around DelhiDOnly in rural areas without mobile networkAnswer: B. India and surrounding region within 1500 km — 7-satellite regional system by ISRO with < 5 m accuracy
Explanation: NavIC / IRNSS (Indian Regional Navigation Satellite System): ISRO''s regional satellite navigation system. Constellation: 7 satellites (3 GSO + 4 IGSO). Coverage: India and 1500 km surrounding region (South Asia, Indian Ocean). Accuracy: < 5 m horizontal position. Services: Standard Positioning Service (SPS, civil) and Restricted Service (RS, military). Launched 2016 (full constellation 2018). Used in: shipping, aviation, emergency response in India.
- 14SurveyingMEDIUM
The 'hydrographic survey' is conducted to determine water body characteristics including:
AOnly topographic mapping of land area near waterBWater depths (soundings), shoreline, bottom type, and currents — nautical charts and bathymetric maps for ports, bridges, reservoirsCOnly groundwater quality testingDRainfall measurement over water bodiesAnswer: B. Water depths (soundings), shoreline, bottom type, and currents — nautical charts and bathymetric maps for ports, bridges, reservoirs
Explanation: Hydrographic survey: mapping of underwater (submarine) terrain and features. Components: (1) Water depths (soundings) using echo sounder or multibeam sonar; (2) Shoreline delineation; (3) Bottom sediment type; (4) Current velocity/direction; (5) Tidal levels. Products: nautical chart, bathymetric map. Equipment: DGPS for position + echo sounder for depth. Applications: port/harbour design, dredging, bridge pier location, reservoir capacity.
- 15SurveyingMEDIUM
The 'traversing' by 'Bowditch rule' (compass rule) distributes closing error:
AEqually to all traverse lines regardless of lengthBProportional to line length — longer lines get larger corrections (Bowditch/compass rule assumes error ∝ distance)COnly to the longest line (one correction)DProportional to the included angle at each stationAnswer: B. Proportional to line length — longer lines get larger corrections (Bowditch/compass rule assumes error ∝ distance)
Explanation: Bowditch (compass) rule: distributes closing error in latitude and departure proportionally to the length of each line. Correction to latitude of line i = −e_L × (l_i / Σl) where e_L = total latitude error, l_i = length of line i. Same for departure. Principle: measurement error ∝ length (longer line → more random error). Transit rule: correction ∝ latitude/departure (used when angles more accurate than distances). Bowditch: most commonly used.
- 16SurveyingEASY
The 'cadastral survey' is conducted primarily for the purpose of:
AOnly measuring elevation for highway designBDelineating land ownership boundaries and areas for legal records — conducted by State Revenue at 1:500 to 1:4000 scaleCWeather forecasting and atmospheric studyDMarine navigationAnswer: B. Delineating land ownership boundaries and areas for legal records — conducted by State Revenue at 1:500 to 1:4000 scale
Explanation: Cadastral survey: detailed large-scale survey of land parcels (fields, plots, villages). Establishes: ownership boundaries, areas of individual parcels, legal records. Output: cadastre (land record), mutation register, revenue maps (7/12 extract in Maharashtra, patta in WB). Scale: 1:500 to 1:4000 (large scale). Conducted by: State Revenue Departments (Survey Settlement Commissioner). Important for: land acquisition, property tax, water rights, dispute resolution.
- 17SurveyingHARD
'Lambert Conformal Conic' map projection is preferred for regions with:
ACountries with greater north-south extentBRegions of greater east-west extent (wide east-west coverage) — standard parallels placed at 1/6 and 5/6 of latitude rangeCOnly for equatorial regionsDOnly for polar regionsAnswer: B. Regions of greater east-west extent (wide east-west coverage) — standard parallels placed at 1/6 and 5/6 of latitude range
Explanation: Lambert Conformal Conic (LCC): conformal (shape preserved locally), standard parallels define zero distortion. Suitable for regions of GREATER east-west extent (wide but short N-S). Examples: US state plane coordinate (mid-latitudes), Indian national grid for wide countries. Transverse Mercator (TM): better for north-south extent. UTM = TM with 6° zones. India uses UTM (WGS84) for engineering and topographic maps. LCC used for: continental US, Canada, meteorological charts.
- 18SurveyingEASY
'Total Station' in surveying integrates:
AOnly horizontal angle measurementBTheodolite (angles) + EDM (distance) + microprocessor — single instrument gives 3D coordinates from one setupCGPS and barometric altimeter onlyDCamera and distance measurement for photography onlyAnswer: B. Theodolite (angles) + EDM (distance) + microprocessor — single instrument gives 3D coordinates from one setup
Explanation: Total station: combines: (1) Theodolite (horizontal and vertical angles); (2) EDM (Electronic Distance Measurement — distance to prism); (3) Microprocessor (computes coordinates, stores data, uploads to computer). Single setup: measures angle + distance → computes 3D point coordinates (E, N, elevation). Replaces: separate theodolite + chain/tape. Modern: robotic total station (auto-targets prism), scanning total station (no prism for short range). IS 8486 part covers field procedures.
- 19SurveyingMEDIUM
'LiDAR' (Light Detection and Ranging) from an airborne platform produces:
AOnly 2D satellite imagery with no elevationBDense 3D point cloud with multiple returns — separate DSM (surface) and DTM (bare earth) from first/last returnsCOnly colour photographs from the aircraftDTemperature map of land surfaceAnswer: B. Dense 3D point cloud with multiple returns — separate DSM (surface) and DTM (bare earth) from first/last returns
Explanation: Airborne LiDAR: laser pulses emitted, time to return measured → range R = c×t/2. Multiple returns: first return (top of canopy), last return (ground even under forest). Dense point cloud: 10–50 points/m². Products: (1) DSM (Digital Surface Model — top of everything); (2) DTM/DEM (Digital Terrain Model — ground after filtering vegetation/buildings); (3) Intensity image; (4) Building footprints. Accuracy: ±15 cm vertical, ±30 cm horizontal. Much faster than conventional survey for large areas.
- 20SurveyingMEDIUM
The resultant sound pressure level of two sound sources, each having a sound pressure level of 50 dB, is
A100 dBB120 dBC15.5 dBD53 dBAnswer: D. 53 dB
Explanation: When two equal sound sources each produce L dB, combined SPL = L + 10*log10(2) = L + 3 dB. General: L_combined = 10*log10(10^(L1/10) + 10^(L2/10)). Adding +3 dB per doubling of identical sources is the standard noise control rule of thumb. For two sources with different levels, the combined level is dominated by the louder source. Two 50 dB sources combine to 53 dB.
- 21Surveying and GeomaticsMEDIUM
Temperature correction in tape measurement is positive when field temperature is:
AHigher than standard temperatureBLower than standard temperatureCEqual to zero CelsiusDNot recordedAnswer: A. Higher than standard temperature
Explanation: Temperature correction Ct = αL(Tm−Ts). It is positive when field temperature Tm is higher than standard temperature Ts; it is negative when Tm is lower.
- 22Total Station GPSEASY
GPS positioning uses:
ALaser ranging to satellitesBPseudorange and carrier phase measurements to multiple satellites (≥4) for 3D position and timeCOnly 2 satellitesDCompass and dead reckoningAnswer: B. Pseudorange and carrier phase measurements to multiple satellites (≥4) for 3D position and time
Explanation: GPS: receiver measures travel time of signals from ≥4 satellites → 4 unknowns (X,Y,Z,time). Pseudorange accuracy ~10m; carrier phase (differential/RTK) → cm-level. Datum: WGS-84.
- 23Remote SensingHARD
Parallax in aerial photography is used for:
ADetermining ground resolutionBMeasuring heights of objects (differential parallax ΔP = B×Δh/H)CColour correctionDRemoving distortion onlyAnswer: B. Measuring heights of objects (differential parallax ΔP = B×Δh/H)
Explanation: Stereoscopy: two overlapping photos (60% endlap) give 3D view. Height: Δh = H×ΔP/(B+ΔP) where H=flying height, B=air base (overlap distance), ΔP=differential parallax. Used in photogrammetric DEM generation.
- 24LevellingMEDIUM
Reciprocal levelling is used to:
AAchieve higher precision on short distancesBEliminate errors due to curvature, refraction, and collimation error when levelling across wide obstacles (rivers, valleys)CFind RL of a distant hillDRun a closed traverseAnswer: B. Eliminate errors due to curvature, refraction, and collimation error when levelling across wide obstacles (rivers, valleys)
Explanation: Reciprocal levelling: take staff readings from both banks of a river/obstacle to both staffs. Average of two height differences eliminates curvature and refraction errors (they are equal and opposite). Collimation error also eliminated.
- 25Plane Table SurveyingMEDIUM
Two-point problem in plane table surveying is solved by:
AResection using 3 known pointsBFinding instrument station using 2 known plotted points — trial and error or mechanical solution (Bessel's method)CRadiation from 2 stationsDIntersection from 2 stationsAnswer: B. Finding instrument station using 2 known plotted points — trial and error or mechanical solution (Bessel's method)
Explanation: Two-point problem: locate table at unknown point using 2 known plotted points. Method: sight both known points, plot rays, move board until both rays pass through respective points on board. Three-point problem: uses Lehmann's or Bessel's method.
- 26Chain SurveyingEASY
An offset in chain surveying is:
ADistance measured along the chain lineBPerpendicular (right angle) or oblique distance from chain line to detailCHeight differenceDAngle measurementAnswer: B. Perpendicular (right angle) or oblique distance from chain line to detail
Explanation: Offset: lateral distance from chain line to object. Perpendicular offset most common. Oblique offset when perpendicular difficult to set out. Maximum offset length for 1:1000 scale: ~15m.
- 27Compass SurveyingMEDIUM
Magnetic declination is:
AAngle between true north and magnetic north at a given location and timeBDip of compass needleCError in compass readingDDifference between two bearingsAnswer: A. Angle between true north and magnetic north at a given location and time
Explanation: Magnetic declination (variation): horizontal angle between true (geographic) north and magnetic north. Changes with location and time. West declination: magnetic north west of true north → add to magnetic bearing for true bearing (if west).
- 28Compass SurveyingEASY
Local attraction in compass surveying is caused by:
AStrong windBPresence of magnetic materials (iron/steel objects) near compass → deflection of needle from magnetic northCIncorrect sightingDHigh elevationAnswer: B. Presence of magnetic materials (iron/steel objects) near compass → deflection of needle from magnetic north
Explanation: Local attraction: magnetic objects (iron structures, electric cables, steel bars) cause local deflection of compass needle. Detected by comparing FB and BB of a line: if they differ by ≠180°, local attraction at one/both stations.
- 29SurveyingMEDIUM
The 'ellipsoidal height' from GPS differs from the orthometric height (MSL) because:
AThey are identical (GPS gives MSL directly)BGPS gives ellipsoidal height h; orthometric H = h − N (N = geoid undulation from MSL to ellipsoid, varies ±70 m in India)CGPS gives depth below sea, not heightDEllipsoidal height is always 100 m less than MSL heightAnswer: B. GPS gives ellipsoidal height h; orthometric H = h − N (N = geoid undulation from MSL to ellipsoid, varies ±70 m in India)
Explanation: GPS measures ellipsoidal height h (above WGS84 reference ellipsoid). Orthometric (levelling) height H = height above geoid (MSL). Relationship: h = H + N (N = geoid undulation). In India: N ranges from −65 m (south) to −50 m (north) approximately. EGM2008 geoid model gives N with ±10–30 cm accuracy. Civil engineering needs orthometric heights (water flows downhill based on geoid, not ellipsoid).
- 30SurveyingMEDIUM
The 'traversing by radiation' (polar method) plots detail points by:
AMeasuring angles only along a chainBMeasuring angle and distance from traverse station to each detail point — polar coordinates converted to rectangular for plottingCOnly for levelling between stationsDConnecting two benchmarksAnswer: B. Measuring angle and distance from traverse station to each detail point — polar coordinates converted to rectangular for plotting
Explanation: Radiation: from one traverse station, angles and distances to all nearby detail points measured. Polar coordinates (distance + bearing/angle) → convert to rectangular (ΔN, ΔE). Advantage: can plot any number of detail points quickly. Suitable for: open terrain. Limitation: error in station position propagates to all detail. Used with total station (tachymetry) for rapid detail survey.
- 31SurveyingEASY
The 'scale of a map' 1:50,000 means:
A1 km on map represents 50 km on groundB1 mm on map represents 50 m (50,000 mm) on ground — 1:50,000 is medium scale for topographic mappingC50 features shown per square kilometreDMap size is 50,000 cm × 50,000 cmAnswer: B. 1 mm on map represents 50 m (50,000 mm) on ground — 1:50,000 is medium scale for topographic mapping
Explanation: Map scale 1:50,000 means 1 unit on map = 50,000 same units on ground. So 1 mm on map = 50,000 mm = 50 m on ground. 2 cm on map = 1 km on ground. Large scale: 1:5,000 (more detail, smaller area shown). Small scale: 1:250,000 (less detail, large area). SOI topographic maps: 1:50,000 (standard), 1:25,000 (detailed), 1:250,000 (overview).
- 32Surveying and GeomaticsHARD
If departure is positive and latitude is negative, the line lies in:
ASouth-east quadrantBNorth-east quadrantCSouth-west quadrantDNorth-west quadrantAnswer: A. South-east quadrant
Explanation: Positive departure means east, negative latitude means south.
- 33Surveying and GeomaticsMEDIUM
Swinging the telescope means rotating it about the:
ABubble tube axisBHorizontal axisCLine of collimationDVertical axisAnswer: D. Vertical axis
Explanation: Horizontal rotation of the telescope is called swinging.
- 34Surveying and GeomaticsHARD
In levelling, the arithmetic check in rise and fall method is:
ASum IS equals sum BSBSum FS equals sum ISCLast RL equals first BSDSum BS minus sum FS equals sum rises minus sum fallsAnswer: D. Sum BS minus sum FS equals sum rises minus sum falls
Explanation: Both differences should also equal last RL minus first RL.
- 35Surveying and GeomaticsEASY
In theodolite, face left and face right observations are taken to eliminate:
ATape sag onlyBAtmospheric pressure variationCInstrumental errors such as collimation errorDRandom booking errors onlyAnswer: C. Instrumental errors such as collimation error
Explanation: Reversing face cancels several systematic instrumental errors.
- 36Surveying and GeomaticsEASY
If fore bearing and back bearing differ by exactly 180 degrees, the line is free from:
ALocal attraction at the two stationsBRefraction onlyCCurvature correctionDSag correctionAnswer: A. Local attraction at the two stations
Explanation: Equal opposite bearings indicate no local magnetic disturbance at the stations.
- 37UTM ProjectionMEDIUM
The Universal Transverse Mercator (UTM) projection divides the world into zones each of:
A10 degrees longitude widthB6 degrees longitude width, numbered 1-60 eastward from 180 degrees longitudeC15 degrees latitude bandsD1 degree widthAnswer: B. 6 degrees longitude width, numbered 1-60 eastward from 180 degrees longitude
Explanation: UTM: 60 longitude zones of 6 deg each; zones numbered 1-60 starting from 180 deg W. India falls in zones 42-47. Within each zone, coordinates are measured in metres (Northing, Easting). Easting origin = 500,000 m (false easting). Northing: equator = 0 (N hemisphere). Scale factor at central meridian = 0.9996.
- 38Triangulation Base LineMEDIUM
In a triangulation survey, the base line is selected such that:
AIt is as short as possibleBIt is on level ground, its length can be measured accurately, and it is well-conditioned for angle measurement to the first trianglesCIt passes through the highest pointDIt avoids any obstaclesAnswer: B. It is on level ground, its length can be measured accurately, and it is well-conditioned for angle measurement to the first triangles
Explanation: Triangulation base line criteria: (1) On level or gently undulating ground for tape/invar wire measurement; (2) Free from obstacles (at least 3 m clearance for sights); (3) Located so first triangles are well-conditioned (angles 30-120 deg); (4) Length: 1/5 to 1/10 of the side of the first triangle.
- 39Bowditch Rule TraverseMEDIUM
In the Bowditch (compass) rule for balancing a closed traverse, the correction to each latitude or departure is:
AProportional to the angle at the traverse stationBProportional to the length of the corresponding survey lineCEqual for all sidesDProportional to the latitude or departure of that lineAnswer: B. Proportional to the length of the corresponding survey line
Explanation: Bowditch rule: correction to latitude (or departure) = (error in latitude / sum of lengths) x length of that line. This distributes error proportionally to side length. Transit rule distributes proportional to arithmetic sum of latitudes/departures (used when angles are more accurate than distances).
- 40Stadia Tacheometry FormulaMEDIUM
For inclined stadia tacheometry with vertical staff, the horizontal distance D between instrument and staff is:
AD = K x s + C (horizontal only)BD = K x s x cos2(theta) + C x cos(theta)CD = K x s x sin(theta)DD = K x s / cos(theta)Answer: B. D = K x s x cos2(theta) + C x cos(theta)
Explanation: Tacheometry formulas (inclined sight, vertical staff): Horizontal distance D = Ks cos2(theta) + C cos(theta); Vertical intercept V = (Ks/2) sin(2theta) + C sin(theta). Where K = stadia multiplier (usually 100), s = staff intercept, C = additive constant (usually 0 for modern telescopes), theta = angle of inclination.
- 41Magnetic DeclinationMEDIUM
If the magnetic declination at a place is 3 degrees East, and the magnetic bearing of a line is 48 degrees (WCB), the true bearing is:
A45 degreesB51 degreesC48 degreesD3 degreesAnswer: B. 51 degrees
Explanation: True Bearing = Magnetic Bearing + Declination (East) = 48 + 3 = 51 degrees (WCB). If declination is West: True bearing = Magnetic bearing - Declination. Magnetic declination changes slowly over years (secular variation) and varies with location (isogonic lines on maps).
- 42Perpendicular Offset Chain SurveyMEDIUM
In chain surveying, perpendicular offsets are preferred over oblique offsets because:
AThey are longer than oblique offsetsBPerpendicular offsets minimize the error in locating the object; a small error in measuring the offset foot position has minimum effect on the plotted object positionCThey require a larger chainDThey use fewer ranging rodsAnswer: B. Perpendicular offsets minimize the error in locating the object; a small error in measuring the offset foot position has minimum effect on the plotted object position
Explanation: Perpendicular offset (at right angle to chain line) minimizes position error because the object lies closest to the chain line. Oblique offsets are used when the perpendicular cannot be conveniently measured. Maximum length of offset should not exceed 15 m for 1:1000 scale surveys.
- 43GeneralMEDIUM
The resection method in plane table surveying is used to locate
Aposition of instrument station from known pointsBcontour intervalCchain correctionDnorth direction from magnetic declination onlyAnswer: A. position of instrument station from known points
Explanation: Resection fixes unknown station by sighting known plotted points.
- 44GeneralMEDIUM
Plane table surveying is especially suitable for
Aunderground sewer flow onlyBprecise first-order triangulationCGPS satellite orbit fixing onlyDsmall-scale mapping with details plotted in fieldAnswer: D. small-scale mapping with details plotted in field
Explanation: Field plotting is quick and convenient for details over small areas.
- 45GeneralMEDIUM
In tacheometry, stadia method is mainly used to determine
ABOD concentrationBsoil shear strengthCconcrete slumpDhorizontal distance and elevation differenceAnswer: D. horizontal distance and elevation difference
Explanation: Stadia readings with staff intercept yield distance and elevation.
- 46GeneralMEDIUM
The correction for curvature in levelling is
Aalways zeroBpositive to staff readingCequal to refraction correction exactlyDnegative to staff readingAnswer: D. negative to staff reading
Explanation: Curvature makes the line of sight above the level surface, so correction to reading is negative.
- 47Theodolite SurveyingMEDIUM
In a transit theodolite, transiting the telescope means rotating it through 180 degrees about the:
Avertical axisBline of collimation onlyChorizontal axisDmagnetic meridianAnswer: C. horizontal axis
Explanation: Transiting or plunging is rotation of the telescope in the vertical plane about its horizontal axis.
- 48Plane Table SurveyingHARD
In plane table surveying, the method of 'intersection' is employed to locate:
AThe instrument station when its position is unknownBInaccessible points visible from two already-plotted instrument stationsCDetail points by measuring distance and direction from a known stationDThe station position using three known plotted control pointsAnswer: B. Inaccessible points visible from two already-plotted instrument stations
Explanation: Intersection: two rays are drawn from two known plotted stations to an inaccessible point. Their intersection on the paper locates it without measuring distance. Radiation = known station + distance + direction. Resection = finding unknown station from known plotted points.
- 49Field SurveyingHARD
A transition curve is introduced to provide gradual change of:
AcurvatureBcement settingCsoil densityDbearing capacityAnswer: A. curvature
Explanation: Transition curve gradually changes curvature from zero to circular curve value.
- 50Field SurveyingHARD
The length of long chord of a simple circular curve is:
AR tan(Delta/2)B2R tan DeltaCR Delta/2D2R sin(Delta/2)Answer: D. 2R sin(Delta/2)
Explanation: The chord joining tangent points subtends central angle Delta, so long chord = 2R sin(Delta/2).