LEADER 00854nam a22002291i 4500 001 991004158489707536 005 20020819105935.0 008 020819s1977 fr a||||||||||||||||fre 035 $ab1192584x-39ule_inst 035 $aocm00000006$9ExL 040 $aDip.to Filologia Ling. e Lett.$bita$cA.t.i. Arché s.c.r.l. Pandora Sicilia s.r.l. 100 1 $aBallif, Claude$0533045 245 10$aBerlioz /$cClaude Ballif 260 $aParis :$bEd. du Seuil,$cstampa 1977 300 $a187 p. :$bill. ;$c18 cm 490 0 $aCollections microcosme.$pSolfeges 907 $a.b1192584x$b28-04-17$c01-04-03 912 $a991004158489707536 945 $aLE008 L.L.I. Mus A IV 45$g1$i2008000466909$lle008$o-$pE0.00$q-$rl$s- $t0$u0$v0$w0$x0$y.i1219749x$z01-04-03 996 $aBerlioz$9913112 997 $aUNISALENTO 998 $ale008$b01-04-03$cm$da $e-$ffre$gfr $h0$i1 LEADER 02316nam 2200601Ia 450 001 9910958154003321 005 20250812211855.0 010 $a9780816664955 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(Au-PeEL)EBL316596 035 $a(CaPaEBR)ebr10194309 035 $a(OCoLC)437191361 035 $a(MiAaPQ)EBC316596 035 $a(EXLCZ)991000000000479445 100 $a19871027d1983 uy 0 101 0 $aeng 135 $aur|n|---||||| 181 $ctxt$2rdacontent 182 $cc$2rdamedia 183 $acr$2rdacarrier 200 04$aThe Holocene /$fH.E. Wright, Jr., editor 205 $a1st ed. 210 $aLondon $cLongman$d1983 215 $a1 online resource (xiv, 407 pages) $cillustrations, maps 225 0 $aLate-Quaternary environments of the United States ;$v2 300 $aDescription based upon print version of record. 311 0 $a9780582301245 311 0 $a0582301246 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$vCongresses 615 0$aGeology, Stratigraphic 615 0$aGeology 676 $a551.7/9/0973 701 $aWright$b H. E$g(Herbert Edgar),$f1917-$01793016 701 $aPorter$b Stephen C$0727091 801 0$bMiAaPQ 801 1$bMiAaPQ 801 2$bMiAaPQ 906 $aBOOK 912 $a9910958154003321 996 $aThe Holocene$94414140 997 $aUNINA