Maryland Geological Survey 501 



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Woodmont Shale Member 'Sice's ^ 2^| 



Olive-green shale and sandstone. Dip 54° E 1554 29.4 1126 



Concealed 1514 105.5 1097 



Ravine 1364 



Concealed 1364 82.4 992 



Olive-green fissile shale. Strike N. 32° E 1247 12.9 919 



Fissile ash-colored and rusty-white shale 1230 5.6 906 



Fissile green shale showing sllckensides 1222 60 901 



Fissile ash-colored and rusty-white shale. Dip 50° E.... 1137 3.5 841 



Fissile green shale 1132 46.5 837 



Concealed 1066 191 791 



Railroad N. 89° W. 



Fissile olive-green shale 793 133.5 600 



Coarse olive-green arenaceous shale and bands of sand- 

 stone. BucMola speciosa fauna.. Dip 50° E 618 106 466 



Fissile shale, ash-colored and white. Dip 65° E 479 4.5 360 



Fissile green shale 474 125 356 



Coarse green shale breaking irregularly. Dip 45° E.... 297 17.5 231 

 Green fissile shale carrying Buchiola speciosa fauna. Dip 



45° E 272 93 213 



Hackly green shale and sandstone 140 32.5 120 



Concealed. N. 23° E. 60° E 102 55.2 88 



Ravine 38 



Oenesee Member 



Concealed. Some black shale seen on hillside. Genesee 



fauna 38 32.5 32 



Romney-Jennings contact 



ROMNEY FORJIATUJN 



Massive sandstone. 



The upper and lower conglomerates of the Chemung are well exposed, 

 the Tropidoleptus carinatus fauna recurring a short distance above the 

 latter. A conspicuous feature is the red bed of Catskill type seen in the 

 small hill near the mouth of Town Creek above which sediments of Jen- 

 nings type carrying marine fossils recur. 



