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(geology) The direction in which stratigraphy becomes younger, for a particular formation quotations
Where well preserved, the pillows show cuspate lower boundaries and lobate upper contacts, defining stratigraphic younging (Fig. 3 E).
2001 May 11, Timothy M. Kusky et al., “The Archean Dongwanzi Ophiolite Complex, North China Craton: 2.505-Billion-Year-Old Oceanic Crust and Mantle”, in Science, volume 292, number 5519, pages 1142–1145
present participle and gerund of young examples