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Arc measurement
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==Extensions== [[File:Clarke figure of the Earth 1860 (cropped).jpg|thumb|upright=2|right|Arc measurements used in Clarke's Figure of the Earth, 1858]] Additional arc measurements, at different latitudinal bands (each delimited by a new pair of standpoint and forepoint), serve to [[Earth ellipsoid#Determination|determine Earth's flattening]]. [[Friedrich Bessel|Bessel]] compiled several [[meridian arc]]s, to compute the famous [[Bessel ellipsoid]] (1841). [[Alexander Ross Clarke#Figure of the Earth, 1858|Clarke]] (1858) combined most of the arc measurements then available to define a new [[reference ellipsoid]].<ref>{{cite EB1911 | ref = {{harvid|Britannica|1911a}} | last = Clarke | first = Alexander Ross | last2 = Helmert | first2 = Friedrich Robert | author2-link = Friedrich Robert Helmert | wstitle = Earth, Figure of the | volume = 8 | pages = 801β814 }}</ref>
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