Report, Band 13John Hopkins Press, 1937 CONTENTS.--Vol. I (1897)--Vol. II (1898)--Vol. III (1899)--Vol. IV (1902)--Vol. V (1905)--Vol. VI (1906)--Vol. VII (1908)--Vol. VIII (1909)--Vol. IX (1911)--Vol. X (1918)--Vol. XI (1922)--Vol. XII (1928)--Vol. XIII (1937)--Vol. XIV (1941) |
Im Buch
Ergebnisse 1-3 von 35
Seite 157
... western end where it is cut out by a fault . Along the southwestern flank between Govans and Lake Montebello the presence of marble has been indicated by the character of the water and proven through excavations for the city water ...
... western end where it is cut out by a fault . Along the southwestern flank between Govans and Lake Montebello the presence of marble has been indicated by the character of the water and proven through excavations for the city water ...
Seite 168
... western two - thirds of the Phoenix dome linear struc- tures pitch gently to moderately westward ( 10 to 40 degrees ) . Within the eastern one - third of the dome the axes plunge gently eastward . This arrangement is very similar to ...
... western two - thirds of the Phoenix dome linear struc- tures pitch gently to moderately westward ( 10 to 40 degrees ) . Within the eastern one - third of the dome the axes plunge gently eastward . This arrangement is very similar to ...
Seite 170
... western and northeastern ends they vary from a northeast - southwest to a northwest - southeast trend , or 66 degrees within six miles . The bend of linear structures and corresponding change in strike of cross joints is coincident with ...
... western and northeastern ends they vary from a northeast - southwest to a northwest - southeast trend , or 66 degrees within six miles . The bend of linear structures and corresponding change in strike of cross joints is coincident with ...
Inhalt
Page | 19 |
Preface | 25 |
Primary Elements in Igneous Rocks of the Piedmont | 37 |
11 weitere Abschnitte werden nicht angezeigt.
Andere Ausgaben - Alle anzeigen
Häufige Begriffe und Wortgruppen
abundant amphibolite amygdules anticlines aplite axes of folding axis Baltimore gabbro Baltimore gneiss banding bedding biotite Bridge Chattolanee dome Chesapeake chlorite cleavage planes Conowingo Dam County Creek cross joints Crosswicks clay crystals deformation Delaware Deposit granodiorite complex diagrams dikes direction east Englishtown Englishtown sand epidote exposures fault feet feldspar flow cleavage flow lines flow structures foliation fossils fracture cleavage gabbro geologic Glenarm Glenarm Series grains granite porphyry granodiorite hornblende igneous rocks inclusions intrusive Jersey lamprophyre linear structures localities marble Marshalltown Marshalltown formation Maryland massive metamorphism metamorphosed mile minerals Mount Laurel Mount Laurel sand northeast occur orientation parallel pegmatite Piedmont planar Plate pluton Port Deposit Port Deposit granodiorite primary quarry quartz diorite quartzite recrystallization region relation schist schistosity sediments Setters formation shear specimen strike Susquehanna River syncline Towson dome transect unconformity Upper Cretaceous volcanics wall rock Wissahickon schist Woodstock dome