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7°05′ 09″S 110°24′18″E Sekolah Staf dan Komando Tentara Nasional Indonesia 6°55′ 48″ S 107°37′52″E Komando Daerah Militer Jayakarta 6°15′11″S 106°51′ 9″E Pusat Zeni Angkatan Darat 6°12′32″S 106°51′20″ E Mabes TNI AD 6°10'09.5"S 106°49'44.0"E Divisi Infanteri 1/Kostrad 6°25′54″S 106°50′23″E
Last version to support Mac OS X 10.6 Snow Leopard and Mac OS X 10.7 Lion; 7.3 July 2017 Google Earth Pro became the standard version of the desktop program. (A free license key was also publicly provided by Google for all the earlier Pro versions.) [67] The desktop application continues to be Google Earth Pro 7.3, with infrequent updates. 8.0
Geodetic latitude and geocentric latitude have different definitions. Geodetic latitude is defined as the angle between the equatorial plane and the surface normal at a point on the ellipsoid, whereas geocentric latitude is defined as the angle between the equatorial plane and a radial line connecting the centre of the ellipsoid to a point on the surface (see figure).
Assuming a spherical Earth, a meridian is a great semicircle on Earth's surface. Adopting instead a spheroidal or ellipsoid model of Earth, the meridian is half of a north-south great ellipse. The length of a meridian is twice the length of an Earth quadrant, equal to 20,003.93 km (12,429.87 mi) on a modern ellipsoid . [2]
The UTM system divides the Earth into 60 zones, each 6° of longitude in width. Zone 1 covers longitude 180° to 174° W; zone numbering increases eastward to zone 60, which covers longitude 174°E to 180°. The polar regions south of 80°S and north of 84°N are excluded, and instead covered by the universal polar stereographic (UPS ...
Similarly the third flattening of the section ellipse is bounded by the corresponding value for the spheroid, and for the spheroid we have ≅ 4.4 × 10 −9, and ≅ 7.3 × 10 −12. Therefore it may suffice to ignore terms beyond B 6 {\displaystyle B_{6}} in the parametric latitude series.
Equirectangular projection of the world; the standard parallel is the equator (plate carrée projection). Equirectangular projection with Tissot's indicatrix of deformation and with the standard parallels lying on the equator True-colour satellite image of Earth in equirectangular projection Height map of planet Earth at 2km per pixel, including oceanic bathymetry information, normalized as 8 ...
The division of Earth by the Equator and the prime meridian Map roughly depicting the Eastern and Western hemispheres. In geography and cartography, hemispheres of Earth are any division of the globe into two equal halves (hemispheres), typically divided into northern and southern halves by the Equator and into western and eastern halves by the Prime meridian.