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) |
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Seite 109
... River , but extend westward into Harford County . Here they split into numerous tongues , the largest of which continues southwest from the river for a distance of nine miles . The easternmost mass ends in the town of Newark , Delaware ...
... River , but extend westward into Harford County . Here they split into numerous tongues , the largest of which continues southwest from the river for a distance of nine miles . The easternmost mass ends in the town of Newark , Delaware ...
Seite 116
... River and at the south contact on Stoney Run . Megascopically the rock is dark colored and fine grained . Foliation ... River . Between Rock Run ( east side ) and the northern contact of the metadacite over one hundred and fifty dikes of ...
... River and at the south contact on Stoney Run . Megascopically the rock is dark colored and fine grained . Foliation ... River . Between Rock Run ( east side ) and the northern contact of the metadacite over one hundred and fifty dikes of ...
Seite 159
... River to the vicinity of Davis where it crosses the river in a northwesterly direction ( Davis syncline ) . East of Rockland and Alberton large pegma- tite dikes follow the contact between the Baltimore gneiss and Setters formation . A ...
... River to the vicinity of Davis where it crosses the river in a northwesterly direction ( Davis syncline ) . East of Rockland and Alberton large pegma- tite dikes follow the contact between the Baltimore gneiss and Setters formation . A ...
Inhalt
Page | 19 |
Preface | 25 |
Primary Elements in Igneous Rocks of the Piedmont | 37 |
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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