00940nam0 22002771i 450 UON0029300820231205103929.68483-211-0231-X20070418d1981 |0itac50 bapolPL|||| 1||||Twarze KsiegiAnna KamienskaWarszawaInstytut Wydawniczy Pax1981173 p.19cm.BibbiaUONC018742FIPLWarszawaUONL000573220BIBBIA21KAMIEŃSKAAnnaUONV165416693484Instytut Wydawniczy PaxUONV269938650ITSOL20250711RICASIBA - SISTEMA BIBLIOTECARIO DI ATENEOUONSIUON00293008SIBA - SISTEMA BIBLIOTECARIO DI ATENEOSI C 0388 SI EO 17144 5 0388 Twarze Ksiegi1251879UNIOR02316nam 2200601Ia 450 991095815400332120250812211855.097808166649551-4356-0553-5(CKB)1000000000479445(EBL)316596(OCoLC)182732628(SSID)ssj0000189559(PQKBManifestationID)12057536(PQKBTitleCode)TC0000189559(PQKBWorkID)10165617(PQKB)10038609(Au-PeEL)EBL316596(CaPaEBR)ebr10194309(OCoLC)437191361(MiAaPQ)EBC316596(EXLCZ)99100000000047944519871027d1983 uy 0engur|n|---|||||txtrdacontentcrdamediacrrdacarrierThe Holocene /H.E. Wright, Jr., editor1st ed.London Longman19831 online resource (xiv, 407 pages) illustrations, mapsLate-Quaternary environments of the United States ;2Description based upon print version of record.9780582301245 0582301246 Includes bibliographies.Contents; Contributors to This Volume; Preface; Introduction; Physical Geology; Paleoecology; Environmental Archaeology; ClimatologyTo many, the Pleistocene Epoch, which constitutes the earlier and major part of the Quaternary Period, is synonymous with the glacial ages and is viewed as a time of dramatic environmental change. Although there now is abundant evidence that glaciations occurred not only during the Pleistocene but through much of the Tertiary Period as well, and therefore are more appropriately considered as late-Cenozoic phenomena.Geology, StratigraphicQuaternaryCongressesGeologyUnited StatesCongressesGeology, StratigraphicGeology551.7/9/0973Wright H. E(Herbert Edgar),1917-1793016Porter Stephen C727091MiAaPQMiAaPQMiAaPQBOOK9910958154003321The Holocene4414140UNINA