Time relation of the Watchung Basalt flows to the faulting in the Newark Graben

George T. Faust

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USGS · 70232919

Time relation of the Watchung Basalt flows to the faulting in the Newark Graben

George T. Faust

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Abstract

In graben structures, volcanic eruptions and faulting are seldom simultaneous and often are not localized in the same place. Field studies in the Triassic basin of New Jersey have supplied evidence supporting the nonsimultaneity of volcanism and faulting in the Newark graben.

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Journal of Research of the U.S. Geological Survey Article

Source-reported bounding extent: 39.977120098439634° to 41.10832999732831° latitude; -74.9871826171875° to -74.058837890625° longitude. This indicates report coverage, not an exact sampling location. View area on OpenStreetMap.

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George T. Faust. 1978. Time relation of the Watchung Basalt flows to the faulting in the Newark Graben. https://pubs.usgs.gov/publication/70232919

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