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Published: 02.07.2007.
Language: Latvian
Level: Secondary school
Literature: n/a
References: Not used

Zemes formu var uzskatīt par sfērisku tikai tuvināti. Precīzi ģeodēziskiem mērījumi rāda, ka tā nav ģeometriski ideāla lode, bet ir it kā saspiesta polos. Tādēļ ekvatoriālais un polārais nav vienāda garuma – polārais rādiuss ir par 21,4 km īsāks. Zemeslodes saplakums sastāda apmēram 1/298 no tās ekvatoriālā rādiusa. Zemeslodes izmēri šādi:
Polārais rādiuss – 6356,8 km
Ekvatoriālais rādiuss – 6378,2 km
Ekvatoriālais apkārtmērs – 40 076 km
Virsmas platība – 510 miljoni km2
Zemeslodes tilpums – 1183 miljardi km3…

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