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![Bulletin of the Geological Society of America. Geology. STRUCTURE 665 lu contrast to tlie porous nature of the bedding planes in the Pottsville rocks mentioned above, the contact of the Niagaran Bulletin of the Geological Society of America. Geology. STRUCTURE 665 lu contrast to tlie porous nature of the bedding planes in the Pottsville rocks mentioned above, the contact of the Niagaran](https://c8.alamy.com/comp/RGFG6N/bulletin-of-the-geological-society-of-america-geology-structure-665-lu-contrast-to-tlie-porous-nature-of-the-bedding-planes-in-the-pottsville-rocks-mentioned-above-the-contact-of-the-niagaran-limestone-with-the-maqnoketa-shale-where-the-sand-is-absent-appears-to-be-impervious-and-for-this-reason-accumulation-of-oil-and-gas-takes-place-in-each-lens-inde-pendently-the-lower-part-of-the-sand-on-the-terrace-at-the-northeast-side-of-the-dome-is-filled-with-salt-water-as-is-also-the-portion-of-the-one-mile-figuke-4sketch-showing-significance-of-unconformities-and-the-quotspottyquot-c-RGFG6N.jpg)