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Published byLorin Lambert Modified over 9 years ago
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CE 453 – Horizontal / vertical reference systems and mapping
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How Long was the route you designed? Were the coordinates based on the: International foot? ( 1m= 3.2808399 ft) (1 ft = 0.3048 m) or the Surveyor’s foot (1 m = 3.2808333 ft) (1m = 39.37”)
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What difference would that make? Effect over 20 miles 0.21 feet (check it out) Effect across the State of Iowa ~ 3.2 feet
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How long was the route you designed? Were the distances measured along horizontal planes, spheroidal surfaces, geodetic surfaces, or Ellipsoidal surfaces?
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How high was the route you designed? Were elevations from datums established in 1927 or in 1988?
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U.S. Reference datums - horizontal for State Plane coordinate conversions NAD27 Clark ellipsoid of 1866 (ft) NAD831980 GRS ellipsoid (metric) Later systems/sources include: World Geodetic System(1984) High Accuracy Reference System(HARN) International Terrestial Reference Frame Continuously Operating Reference Stations
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Computing State Plane coordinates: Lambert projection 10 Equations to determine zone constants - Basic components Ellipsoid major axis Eccentricity Grid origin (Latitude and longitude of the zone) Spot coordinates (latitude and longitude) False northing and easting of zone
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Mapping and data reference systems The following sequence of slides is intended to introduce various data reference systems. Several slides were obtained form a presentation from David Doyle, National Geodetic Survey
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