Resumen: This study uses luminescence and 14C accelerator mass spectrometry procedures to date relevant glaciofluvial and glacial deposits from the south-central and southeastern Pyrenees (Andorra–France–Spain). We distinguish two types of end-moraine complexes: (1) those in which at least a far-flung moraine exists beyond a frequently nested end-moraine complex (the most common) and (2) those in which a close-nested end moraine encompasses at least two glacial cycles. Both types formed within six distinctive glacial intervals: (1) A penultimate glacial cycle during Marine Oxygen Isotope Stage (MIS) 6 and older glaciofluvial terraces occurred beyond the range of the luminescence dating method. (2) An early glacial advance in MIS 5d (~97 −15/+19 ka) was followed by glacial retreat during MIS 5c (< 91 ± 9 ka). (3) The last maximum ice extent (LMIE) was in early MIS 4 (~74 ± 4.5 ka). (4) Unexpectedly, glaciers thinned during the second half of MIS 3 (~39 −6/+11 ka). (5) During the MIS 3–2 transition, glaciers subsequently fluctuated behind the LMIE limits. (6) The global last glacial maximum (LGM) started as early as ~26.6 ± 0.365 ka b2k, and the corresponding end moraines were built behind the LMIE limits or merged with it, forming close-nested moraines. Idioma: Inglés DOI: 10.1017/qua.2022.68 Año: 2023 Publicado en: Quaternary Research (United States) 113 (2023), [28 pp.] ISSN: 0033-5894 Factor impacto JCR: 1.7 (2023) Categ. JCR: GEOGRAPHY, PHYSICAL rank: 38 / 65 = 0.585 (2023) - Q3 - T2 Categ. JCR: GEOSCIENCES, MULTIDISCIPLINARY rank: 155 / 254 = 0.61 (2023) - Q3 - T2 Factor impacto CITESCORE: 4.7 - Earth and Planetary Sciences (all) (Q2) - Arts and Humanities (miscellaneous) (Q1) - Earth-Surface Processes (Q2)