. Annual Reports of the Department of the Interior for the Fiscal Year Ended June 30, 1900--Twenty-First Annual Report of the United States Geological Society. om the cliff ofEast Hill and its con- jtinuation to the south-ward, from the long cliff of gneiss which extends along the westernborder of the basin for a distance of nearly a mile in about the lati-tude of Pomperaug village (9j), or from the intermontane valley ofOrenaug Hill, where one may walk a full mile along cliffs that areinterrupted for but short intervals (see map, PI. X). The N. ± 31^^ ^Y. series.—A very good opportunity to me
. Annual Reports of the Department of the Interior for the Fiscal Year Ended June 30, 1900--Twenty-First Annual Report of the United States Geological Society. om the cliff ofEast Hill and its con- jtinuation to the south-ward, from the long cliff of gneiss which extends along the westernborder of the basin for a distance of nearly a mile in about the lati-tude of Pomperaug village (9j), or from the intermontane valley ofOrenaug Hill, where one may walk a full mile along cliffs that areinterrupted for but short intervals (see map, PI. X). The N. ± 31^^ ^Y. series.—A very good opportunity to measure thestrike of this series is afforded l)y one of the scarps (aj which arc soprominent on the eastern slope of the eastern Orenaug twin (PI. V,B). Other excellent opportunities are afforded ])y the ofexposures which line the Hotchkissville Valley on the northeast ()))and southwest (bg), and by the fault (n) which is indicated in a lineof low cliffs following the right bank of the brook entering Transyl-vania Brook frt)m the west a short distance below the cascade. The X. ± E. Series.—The direction of this series of faults may. -Northwestern bdniulai Kagland. 102 NEWARK SYSTEM OF POMPERAUG VALLEY, CONN.
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