LEADER 02048oam  2200421zu 450 
001 996217168703316
005 20210807004638.0
010   $a1-118-66671-2
035   $a(CKB)3450000000004181
035   $a(SSID)ssj0000815145
035   $a(PQKBManifestationID)11459161
035   $a(PQKBTitleCode)TC0000815145
035   $a(PQKBWorkID)10802123
035   $a(PQKB)11019714
035   $a(NjHacI)993450000000004181
035   $a(PPN)188970932
035   $a(EXLCZ)993450000000004181
100   $a20160829d1989      uy              
101 0 $aeng
135   $aur|||||||||||
181   $ctxt
182   $cc
183   $acr
200 00$aAccreted Terranes of the North Cascades Range, Washington
210 31$a[Place of publication not identified]$cAmerican Geophysical Union$d1989
215   $a1 online resource (346 pages)
300   $aBibliographic Level Mode of Issuance: Monograph
311   $a0-87590-612-5 
330   $aThe Cascade Range is an active north-trending volcanic arc at the western edge of North America (Figure 1). At the northern end of the range, between 47°N and 49°N, the average elevation increases, peaks become sharper, numerous small glaciers survive on the higher slopes, and volcanic rocks of the Cascade arc are scarce. This region is the North Cascades Range. The North Cascades are bounded on the west by the fore-arc basin of the Puget Lowland, on the south by the arc volcanic rocks of the Central Cascades, and on the southeast by the back-arc flood basalts of the Columbia Plateau. The geologic identity of the range is not so clearly defined to the north, but it is geographically bounded on the northeast by the Okanogan Ranges and on the northwest by the Fraser River, which separates the Cascades from the Coast Mountains.
606   $aGeology
615  0$aGeology.
676   $a550
702   $aTabor
801  0$bPQKB
906   $aBOOK
912   $a996217168703316
996   $aAccreted Terranes of the North Cascades Range, Washington$91953666
997   $aUNISA