{"id":1232,"date":"2016-08-01T09:52:43","date_gmt":"2016-08-01T13:52:43","guid":{"rendered":"http:\/\/caslabs.case.edu\/hyde-collection\/?page_id=1232"},"modified":"2016-08-01T09:52:43","modified_gmt":"2016-08-01T13:52:43","slug":"metamorphic-rock-structures","status":"publish","type":"page","link":"https:\/\/caslabs.case.edu\/hyde-collection\/metamorphic-rock-structures\/","title":{"rendered":"Metamorphic Rock Structures"},"content":{"rendered":"

 <\/p>\n

Gneiss<\/a>\u00a0 | \u00a0Marble<\/a>\u00a0 | \u00a0Slate and Slatey Cleavage<\/a><\/p>\n

 <\/p>\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n
<\/a><\/p>\n

GNEISS<\/h3>\n<\/td>\n<\/tr>\n

401.-.1<\/a><\/td>\nContorted gneiss, shore of Ottawa River, Canada.<\/td>\n<\/tr>\n
401.-.2<\/a><\/td>\nBoulder of contorted gneiss, Amherst, Massachusetts.<\/td>\n<\/tr>\n
401.-.3<\/a><\/td>\nPre-cambrian gneiss cutting Precambrian granite. Man is on granite; contact cuts gneiss squarely beneath foreground patch of soil. Kingston, Ontario. All hill and valley here shown are Pre-ordovician, disclosed by removal of earlier Paleozoic limestone. Slide 481.B.3 and 4 are at water level below dead tree.<\/td>\n<\/tr>\n
<\/a><\/p>\n

MARBLE<\/h3>\n<\/td>\n<\/tr>\n

407.-.1<\/a><\/td>\nMarble flowage effects produced by metamorphism. Georgian Bay, near Honey Harbor, Ontario.<\/td>\n<\/tr>\n
<\/a><\/p>\n

SLATE AND SLATEY CLEAVAGE<\/h3>\n<\/td>\n<\/tr>\n

409.-.1<\/a><\/td>\nAnticlinal fold. Axis dip and cleavage dip to west; beds thicken at summit; Castlemaine, Victoria.<\/td>\n<\/tr>\n
409.-.2<\/a><\/td>\nSlatey cleavage and its relation to bedding planes; 2 miles south of Walland, Tennessee.<\/td>\n<\/tr>\n
409.-.3<\/a><\/td>\nHill showing cleavage in granite. North side of Deep Spring Valley. Inyo County, California.<\/td>\n<\/tr>\n
409.-.4<\/a><\/td>\nWest end of ridge, giving nearer view of granite. Same locality as preceding slide.<\/td>\n<\/tr>\n
409.-.5<\/a><\/td>\nDiagram of pure shortening, after Van Hise.<\/td>\n<\/tr>\n
409.-.6<\/a><\/td>\nDiagram showing the development of fracture cleavage, after Van Hise.<\/td>\n<\/tr>\n
409.-.7<\/a><\/td>\nBlock showing development of fracture cleavage, after Van Hise.<\/td>\n<\/tr>\n<\/tbody>\n<\/table>\n

<\/p>\n","protected":false},"excerpt":{"rendered":"

 <\/p>\n

Gneiss<\/a>\u00a0 | \u00a0Marble<\/a>\u00a0 | \u00a0Slate and Slatey Cleavage<\/a><\/p>\n

 <\/p>\n

<\/a>
\nGNEISS<\/p>\n

401.-.1<\/a>
\nContorted gneiss, shore of Ottawa River, Canada.<\/p>\n

401.-.2<\/a>
\nBoulder of contorted gneiss, Amherst, Massachusetts.<\/p>\n

401.-.3<\/a>
\nPre-cambrian gneiss cutting Precambrian granite. Man is on granite; contact cuts gneiss squarely beneath foreground patch of soil. Kingston, Ontario. All hill and valley here shown are Pre-ordovician, disclosed by removal of earlier Paleozoic limestone. Slide 481.B.3 and 4 are at water level below dead tree.<\/p>\n

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