H. B. Cornwall

Summary

H. B. Cornwall,  Popular Science Monthly (1876)

“ The oil-bearing shales commonly show few vegetable remains, and Dana observes that the absence of distinct fossil animal and vegetable remains points to an abundance of delicate water-plants or infusorial or microscopic vegetable life as the source of the organic material contained in them. Limestones, on the other hand, are frequently full of animal fossil remains, showing an animal origin for the oil in them, although it is by no means agreed that the petroleum in certain limestones was derived from organic remains in the limestones and not from other strata below them. ”
Source: Wikisource

H. B. Cornwall,  Popular Science Monthly (1876)

“ Such a well, after standing a while would again yield oil on pumping, then perhaps water only, or water and oil, until it had had another rest. If the supply of gas is kept up by an open crevice, the well may continue to flow for some time. The pressure of neighboring water may also cause the oil to flow from a well. Generally the pumping-wells are pretty constant, although when a number of wells are bored near together they interfere with each other, and sometimes water poured down one well will appear in another, and this method has been pursued to bring rival well-owners to terms. ”
Source: Wikisource

H. B. Cornwall,  Popular Science Monthly (1876)

“ As regards the circumstances favoring the accumulation of petroleum, it appears that there should be a shale or other fine-grained rock forming to protect the organic matter during its deposition, a porous stratum above to be penetrated by the hydrocarbons resulting from the decomposition of the organic matter, and finally another shale or slate above, to prevent the further escape of the volatile products. If the sand-rock which usually forms the porous stratum is filled with fissures, large quantities of oil may collect in these. ”
Source: Wikisource

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