Annals of Philosophy, Том 22Baldwin, Cradock, and Joy, 1823 |
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Страница 20
... elevation above the lake amounts from 150 to 200 feet . On the south - east end of the lake , from Ickaan to the church of Rattwick , much granite is found with few and thin beds of limestone ; near the church of Rattwick , a bed of ...
... elevation above the lake amounts from 150 to 200 feet . On the south - east end of the lake , from Ickaan to the church of Rattwick , much granite is found with few and thin beds of limestone ; near the church of Rattwick , a bed of ...
Страница 94
... elevation of 60 or 70 feet above the level of the beach . The denuded face of this bunch of granite is 30 or 40 feet thick . Two or three veins appear to take their origin from this anomalous overlying mass . One spreads out in minute ...
... elevation of 60 or 70 feet above the level of the beach . The denuded face of this bunch of granite is 30 or 40 feet thick . Two or three veins appear to take their origin from this anomalous overlying mass . One spreads out in minute ...
Страница 95
... elevation , only a part of it . The quantity by which it has sunk expresses the weight of the stratum of air intercepted between the levels of the two stations . Considered in relation to the measure of height , it expresses the ...
... elevation , only a part of it . The quantity by which it has sunk expresses the weight of the stratum of air intercepted between the levels of the two stations . Considered in relation to the measure of height , it expresses the ...
Страница 96
... elevation will be marked in the barometer by successive depressions of the mercury so much the smaller as we rise higher . We perceive then that in a column of air supposed at a uniform temperature , the density of the strata decreases ...
... elevation will be marked in the barometer by successive depressions of the mercury so much the smaller as we rise higher . We perceive then that in a column of air supposed at a uniform temperature , the density of the strata decreases ...
Страница 97
... elevation : for then , taking the barometer to the two extremities of the measured height , and dividing the difference of the logarithms by the difference of elevation , we shall equally obtain the number we seek ; it will , however ...
... elevation : for then , taking the barometer to the two extremities of the measured height , and dividing the difference of the logarithms by the difference of elevation , we shall equally obtain the number we seek ; it will , however ...
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Albumen and salts ammonia angles animal Annals of Philosophy antimony appear ARTICLE atmosphere Aurora barometer barytes beds blood capric acid carbonate charcoal cleavage coal gas coefficient colour column common considerable contains copper correction crystals degree direction distance distilled earth effect elevation error experiments feet felspar formation globules granite greywacke heat height hydrogen inches instrument iron light lime limestone logarithm magnetic mean measurements mercury metallic method mineral molecules mountains muriatic acid nature nearly needle nitrate observations obtained octahedron oil gas Ordo oscillations oxide oxygen paper parallel phænomena pier planes platina plumbago potash primary form prism produced proportion quantity remarkable respect rhombic dodecahedron rhombic prism right ascension rocks sandstone silver slate solution species specific gravity stars substances sulphuric supposed surface tables temperature thermometer thick tion titanic acid trachyte vapour variation veins vibrations volcano wind
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