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 48
Seite 156
... Setters formation is continuous from the sharply compressed nose near Hartley southwestward to Cub Hill . On the north side of Gunpowder Falls it is intruded by large amounts of Gunpowder granite . Its continuation southwestward to ...
... Setters formation is continuous from the sharply compressed nose near Hartley southwestward to Cub Hill . On the north side of Gunpowder Falls it is intruded by large amounts of Gunpowder granite . Its continuation southwestward to ...
Seite 159
... Setters and Wissahickon formations which have lent themselves to pegmatitic solu- tions . Here the dikes formed are nearly always concordant . They appear to be lenticular bodies having spread apart the schist on both sides . Pegmatites ...
... Setters and Wissahickon formations which have lent themselves to pegmatitic solu- tions . Here the dikes formed are nearly always concordant . They appear to be lenticular bodies having spread apart the schist on both sides . Pegmatites ...
Seite 185
... Setters formation seems closely attached , is of very much larger order of magnitude than minor folding in the gneiss complex below or in the marble and schist above . Major folds are overturned toward the north as well as to the south ...
... Setters formation seems closely attached , is of very much larger order of magnitude than minor folding in the gneiss complex below or in the marble and schist above . Major folds are overturned toward the north as well as to the south ...
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