Subrounded pebbles and cobbles were probably derived from lower Paleozoic rocks that covered the Precambrian rocks of the present day Highlands to the northwest during the formation of the Newark Basin.
Subrounded pebbles and cobbles were probably derived from lower Paleozoic rocks that covered the Precambrian rocks of the present day Highlands to the northwest during the formation of the Newark Basin.
I used data from 3 seismograph stations:
1) PAL_LD in Palisades, New York
2) P61A_N4 in Hammonton, New Jersey
3) PSSK_PE in Schuylkill Haven, Pennsylvania
I used data from 3 seismograph stations:
1) PAL_LD in Palisades, New York
2) P61A_N4 in Hammonton, New Jersey
3) PSSK_PE in Schuylkill Haven, Pennsylvania