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datums, and − connection of national datums with a global geodetic
                  datum.
                        It is also used for geodetic control, namely for:
                        −  establishment  of  geodetic  control  for  national  networks,  −

                  installation  of  three-dimensional  homogeneous  networks,  −  analysis
                  and improvement of existing terrestrial networks, − establishment of
                  geodetic  connections  between  islands  or  with  the  mainland,  −

                  densification of existing networks up to short interstation distances.
                        In geodynamics satellite geodesy is used to show:
                        − control points for crustal motion, − permanent arrays for 3D-
                  control  in  active  areas,  −  polar  motion,  Earth  rotation,  and  −  solid

                  Earth tides.
                        In applied and plane geodesy it gives:
                        −  detailed  plane  surveying  (land  register,  urban  and  rural

                  surveying,  geographic  information  systems  (GIS),  town  planning,
                  boundary  demarcation  etc.),  −  installation  of  special  networks  and
                  control  for  engineering  tasks,  −  terrestrial  control  points  in

                  photogrammetry  and  remote  sensing,  −  position  and  orientation  of
                  airborne sensors like photogrammetric cameras, − control and position
                  information  at  different  accuracy  levels  in  forestry,  agriculture,

                  archaeology, expedition cartography etc.
                        In navigation and marine geodesy satellite geodetic technologies
                  are used to give:
                        −  precise  navigation  of  land-,  sea-,  and  air-vehicles,  −  precise

                  positioning  for  marine  mapping,  exploration,  hydrography,
                  oceanography,  marine  geology,  and  geophysics,  −  connection  and
                  control of tide gauges (unification of height systems).

                        With more satellite systems becoming operational, there is almost
                  no  limit  to  the  possible  applications.  Satellite  geodesy  also  made  a
                  substantial  contribution  to  the  deepening  perspective  in  which  men
                  could view their own planet. But the new perspective differed in an

                  interesting way from that provided in magnetospheric physics. For the
                  latter, rockets and satellites revealed a wide range of hitherto unknown
                  phenomena.  In  contrast the  subject matter  and problems  of  geodesy

                  were  well  known;  it  was  increased precision, the  ability  to  measure
                  higher  order  effects,  and the  means for  constructing  a  single  global
                  reference system that space methods helped to provide.





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