Proceedings of the Academy of Natural Sciences of PhiladelphiaAcademy of Natural Sciences of Philadelphia, 1883 |
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Page 13
... green sponge has , as yet , only been found in a branch of Cobb's Creek , a small stream whose waters reach the Delaware River below Philadelphia . It occupied the upper surface of large stones in the bed of the stream ; some of the ...
... green sponge has , as yet , only been found in a branch of Cobb's Creek , a small stream whose waters reach the Delaware River below Philadelphia . It occupied the upper surface of large stones in the bed of the stream ; some of the ...
Page 37
... green carpet . At times , whole blocks of dolomite are replaced by serpentine . Transverse striæ have been noticed only on very thin seams , yet here they are quite as distinct as upon the adjacent dolomite . Rhombic cleavage - planes ...
... green carpet . At times , whole blocks of dolomite are replaced by serpentine . Transverse striæ have been noticed only on very thin seams , yet here they are quite as distinct as upon the adjacent dolomite . Rhombic cleavage - planes ...
Page 48
... green to light brown mineral with a more or less pearly lustre . Prof. Prime has also sent it from a locality about two and one - half miles south of Blandon ; this specimen is of a pale green color with a somewhat silky lustre , H 2 ...
... green to light brown mineral with a more or less pearly lustre . Prof. Prime has also sent it from a locality about two and one - half miles south of Blandon ; this specimen is of a pale green color with a somewhat silky lustre , H 2 ...
Page 49
... green , glassy coatings on horn- blendic gneiss at a quarry on Mill Street , Germantown . The mineral has the usual mammillary or botryoidal surface , is perfectly transparent , and has a beautiful light green color . The color is due ...
... green , glassy coatings on horn- blendic gneiss at a quarry on Mill Street , Germantown . The mineral has the usual mammillary or botryoidal surface , is perfectly transparent , and has a beautiful light green color . The color is due ...
Page 51
... green masses , somewhat after the manner of the apatite of that locality . It has a scaly structure and a felspathic cleavage . It has a hardness of about 2.5 . Its color is pale apple - green , and when heated it turns dark gray . It ...
... green masses , somewhat after the manner of the apatite of that locality . It has a scaly structure and a felspathic cleavage . It has a hardness of about 2.5 . Its color is pale apple - green , and when heated it turns dark gray . It ...
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Common terms and phrases
Academy American Ammonites antennæ ants appears arises arm-plates base beds biotite Bloch border brachial branch calyx cent character Chester cretaceous crystals deposits described diameter distinct dopplerite Editor eocene exhibited F. V. Hayden fauna Flexor forms fossil Gabb genera genus Geological gneiss green head Heilprin Hematite hornblende humerus I. V. Williamson Fund inch inserted iron-ores Jeanes lateral LEIDY length limonite locality lower magnetite male flowers margin Maryland median MEEHAN mica mineral miocene molar muscle Museum Nearctic Nearctic region Neotropical nerve nest North Nummulites observed occur Odontomyia outcrop Palearctic peculiar persons present pinnules plates pliocene portion posterior Prof pseudomorphs quartz radial recent represented rocks Rüpp schists Sciences Scutellum serpentine side Société Society South Carolina species specimens spines surface Tejon tendon tertiary third thorax tibiæ transverse tree Underbasals upper Vaux veins Virginia width yellow yellowish
Popular passages
Page 148 - Robinson was elected a member of the Council, to fill the vacancy caused by the election of the Rev.
Page 204 - Five of the genera are peculiar to the Secondary. An Ammonite ranges entirely through the group to the top of the highest fossiliferous strata. The genera Perissolax, Gyrodes, Margaritella, and the sub-genus Anchura, of the genus Aporrhais, are all recognized as strictly characteristic of the Cretaceous ; so much so, that the presence of a single undoubted representative of either of these genera would be strong presumptive evidence of the Cretaceous age of any rocks in which it might be found.
Page 115 - It was one of the most ancient as well as one of the most interesting places in sacred record.
Page 239 - The body terminated in a caruncular point which, with the position of the two hind-legs, made a tridentate obstruction to the sand brought down by the retreating wave, and the water passing .around the points made the three toe-like grooves which resembled a bird's foot from one and a half to two inches long. The creatures in their scrambles for protection beneath the sand, managed to keep at fair distances from each other, and hence there was considerable regularity in the tracks as if they had...
Page 339 - The beds of argillaceous iron-ore, which spread so widely through New York and some of the other States west, could not have been formed in an open sea; for clayey iron-deposits do not accumulate under such circumstances. They are proof of extensive marshes, and, therefore, of land near the sea-level. The few fragments of Crinoids and shells found in these beds are evidence that they were, in part at least, salt-water marshes, and that the tides sometimes reached them.
Page 263 - orange-ant feeders' are provided with pig or goat bladders, which are baited inside with lard. The orifices of these they apply to the entrance of nests, when the ants enter the bags and become a marketable commodity at the orangeries.
Page 214 - I was not able to find a single cretaceous fossil, nor even any true cretaceous generic forms, in the entire formation ; and I am altogether of the opinion expressed by Mr. Conrad, many years before Mr. Gabb, in volume 5, of Pacific Railroad Explorations, pages 318, 320, et.
Page 237 - Jersey, where they were very abundant, and had proved a great pest in the cultivation of tobacco. The worms collected presented a number of well-marked varieties, which were supposed to be all of the same species. The principal ones were indicated as follows : 1. Pea-green or...
Page 260 - One of oval form measured 1 mm. long by 0.75 mm. broad. The smaller ones measured 0.75 mm. in diameter. After another day they appeared in good condition, but the rays were contracted so as to be about half the original length, and many had a minute granular ball at the end, apparently effete matter thrown off from them. At this time the animalcules were returned to the aquarium.
Page 345 - Origin of sedias to whether they were originally deposited as such, or in some other tit(?s- — form, and afterwards altered to magnetite. It seems possible that, in some cases, beds may have been formed by the accumulation of iron sands, just as they are forming in the Gulf of St. Lawrence to-day, the material being derived from the disintegration of pre-existing crystalline rocks.