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palaeolongitude
palaeolongitude n. 
/ˌpalɪə(ʊ)ˈlɒŋdʒᵻtjuːd/, /ˌpeɪlɪə(ʊ)ˈlɒŋɡᵻtjuːd/, /ˌpeɪlɪə(ʊ)ˈlɒŋdʒᵻtjuːd/, /ˌpeɪlioʊˈlɑndʒᵻˌt(j)ud/ Geology the longitude of a place at some time in the past.
Brit. /ˌpalɪə(ʊ)ˈlɒŋɡᵻtjuːd/
, /ˌpalɪə(ʊ)ˈlɒŋɡᵻtjuːd//ˌpalɪə(ʊ)ˈlɒŋdʒᵻtjuːd//ˌpeɪlɪə(ʊ)ˈlɒŋɡᵻtjuːd//ˌpeɪlɪə(ʊ)ˈlɒŋdʒᵻtjuːd/U.S. /ˌpeɪlioʊˈlɔndʒᵻˌt(j)ud/
, /ˌpeɪlioʊˈlɔndʒᵻˌt(j)ud//ˌpeɪlioʊˈlɑndʒᵻˌt(j)ud/ΘΚΠ
the world > the earth > geodetic references > [noun] > longitude > in the past
palaeolongitude1964
1964 K. M. Creer in A. E. M. Nairn Probl. Palaeoclimatol. 274 Because of the assumed axial symmetry of the field, palaeomagnetic data cannot yield information about palaeolongitude.
1990 P. Kearey & F. J. Vine Global Tectonics xi. 261 Palaeomagnetic methods give no control on palaeolongitude.
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