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glacio-eustasy
glacio-eustasy n. 
/ˌɡleɪʃɪə(ʊ)ˈjuːstəsi/, /ˌɡlasɪə(ʊ)ˈjuːstəsi/, /ˌɡleɪʃioʊˈjustəsi/ changes in the sea-level caused by the waxing and waning of ice-sheets.
Brit. /ˌɡleɪsɪə(ʊ)ˈjuːstəsi/
, /ˌɡleɪsɪə(ʊ)ˈjuːstəsi//ˌɡleɪʃɪə(ʊ)ˈjuːstəsi//ˌɡlasɪə(ʊ)ˈjuːstəsi/U.S. /ˌɡleɪʃiəˈjustəsi/
, /ˌɡleɪʃiəˈjustəsi//ˌɡleɪʃioʊˈjustəsi/ΘΚΠ
the world > the earth > water > sea or ocean > region of sea or ocean > [noun] > sea level > changes in sea level
reliction1603
retrogression1815
regression1902
glacio-eustatism1935
glacio-eustasy1962
1962 New Scientist 2 Aug. 243/1 Given a few decades or millenia of warmer summers, and the glaciers melt; the hydrologic balance swings to the positive side and the ocean level rises. This is the phenomenon of ‘glacio~eustasy’.
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