LEADER 02291nam  2200601Ia 450 
001 9910452154303321
005 20200520144314.0
010   $a0-8166-5528-6
010   $a1-4356-0553-5
035   $a(CKB)1000000000479445
035   $a(EBL)316596
035   $a(OCoLC)182732628
035   $a(SSID)ssj0000189559
035   $a(PQKBManifestationID)12057536
035   $a(PQKBTitleCode)TC0000189559
035   $a(PQKBWorkID)10165617
035   $a(PQKB)10038609
035   $a(MiAaPQ)EBC316596
035   $a(Au-PeEL)EBL316596
035   $a(CaPaEBR)ebr10194309
035   $a(OCoLC)437191361
035   $a(EXLCZ)991000000000479445
100   $a19871027d1983      uy             0
101 0 $aeng
135   $aur|n|---|||||
181   $ctxt
182   $cc
183   $acr
200 04$aThe Holocene$b[electronic resource] /$fH.E. Wright, Jr., editor
210   $aLondon $cLongman$d1983
215   $a1 online resource (424 p.)
225 0 $aLate-Quaternary environments of the United States ;$v2
300   $aDescription based upon print version of record.
311   $a0-8166-1171-8 
311   $a0-8166-1169-6 
320   $aIncludes bibliographies.
327   $aContents; Contributors to This Volume; Preface; Introduction; Physical Geology; Paleoecology; Environmental Archaeology; Climatology
330   $aTo 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.
606   $aGeology, Stratigraphic$yQuaternary$vCongresses
606   $aGeology$zUnited States$vCongresses
608   $aElectronic books.
615  0$aGeology, Stratigraphic
615  0$aGeology
676   $a551.7/9/0973
701   $aWright$b H. E$g(Herbert Edgar),$f1917-$0899346
701   $aPorter$b Stephen C$0727091
801  0$bMiAaPQ
801  1$bMiAaPQ
801  2$bMiAaPQ
906   $aBOOK
912   $a9910452154303321
996   $aThe Holocene$92077567
997   $aUNINA