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Landowners only granted permission to visit these sites to the organizers of the original trips for the designated dates of the conference. I The sediments are preserved in basins that are largely fault bounded (Fig. Thes^ include the Boston Basin, which contains late Proterozoic to Middle Cambrian con- glomerate, argillite, and volcanic rock (Kaye and Zartman, 1980; Kaye, 1981) , the Narragansett and Norfolk Basins which contain Carboniferous stream deposits that overlie trilobite-bearing Cambrian phyllites (Shaler and others, 1899; Skehan and others, 1979) , and offshore basins of Triassic to Jurrassic sandstone, siltstone, and basalt (Ballard and Uchupi, 1975) .

It is your responsibility to obtain permission for your visit. Especially when using older guidebooks in this collection, note that locations may have changed drastically. Locally common are Mesozoic dikes of diabase and lamprophyre.

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