 | Sir Charles Lyell - 1833 - 578 Seiten
...it is of great thickness, and contains hard beds of blue chert and limestone. Here, accordingly, we find that it produces a corresponding influence on...the foot of the chalk-hills, and constitutes a lower a, Chalk with flints. c, Upper green sauJ, or firestone. No. 67. b, Chalk without flints. ./, Gault.... | |
 | Sir Charles Lyell - 1833 - 570 Seiten
...it is of great thickness, and contains hard beds of blue chert and limestone. Here, accordingly, we find that it produces a corresponding influence on...the foot of the chalk-hills, and constitutes a lower o, Chalk with flints. r, Upper green saml, or firestone. No. 67. l>, Chalk without flints. ./, Gault.... | |
 | Sir Charles Lyell - 1834 - 422 Seiten
...it is of great thickness, and contains hard beds of blue chert and limestone. Here, accordingly, we find that it produces a corresponding influence on...in breadth from a quarter of a mile to three miles, i 3 and following the sinuosities of the chalk escarpment. * No. 120. a. Chalk with flints. b. Chalk... | |
 | Sir Charles Lyell - 1837 - 584 Seiten
...it is of great thickness, and contains hard beds of blue chert and limestone. Here, accordingly, we find that it produces a corresponding influence on...three miles, and following the sinuosities of the chalk escarpment.* Fig. 101. a. Chalk with flints. c. Upper green-sand, or firestone. b. Chalk without... | |
 | Sir Charles Lyell - 1841 - 946 Seiten
...thickness, and contains hard beds of blue chert and calcareous sandstone or firestone. Here, accordingly, we find that it produces a corresponding influence on...three miles, and following the sinuosities of the chalk escarpment.* Fig. 229. a. Chalk with Bints. b. Chalk without flint». c. Upper green-sand, or... | |
 | James Fenimore Cooper - 1844 - 516 Seiten
...ship lay might have covered a hundred and fifty acres in extent, the belt of land which encircled it, varying in breadth from a quarter of a mile to three miles. Most of the island was an open grove, lying at an elevation of from ten to thirty feet above the ocean... | |
 | James Fenimore Cooper - 1844 - 922 Seiten
...ship lay might have covered a hundred and fifty acres in extent, the belt of land which encircled it, varying in breadth from a quarter of a mile to three miles. Most of the island was an open grove, lying at an elevation of from ten to thirty feet above the ocean... | |
 | Sir Charles Lyell - 1851 - 540 Seiten
...thickness, and contains hard beds of blue chert and calcareous sandstone or firestone. Here, accordingly, we find that it produces a corresponding influence on...three miles, and following the sinuosities of the chalk escarpment.* Fig.**. a. Chalk with flinll. A Chalk without «ii.U. c. Upper greeusand, or firestone.*... | |
 | Sir Charles Lyell - 1851 - 602 Seiten
...thickness, and contains hard beds of blue chert and calcareous sandstone or firestone. Here, accordingly, we find that it produces a corresponding influence on...three miles, and following the sinuosities of the chalk escarpment.* Fig. 2»8. a. Chalk with flints. 6. Chalk without fiints. c. Upper grcensand, or... | |
 | James Fenimore Cooper - 1851 - 520 Seiten
...ship lay might have covered a hundred and fifty acres in extent, the belt of land which encircled it, varying in breadth from a quarter of a mile to three miles. Most of the island was an open grove, lying at an elevation of from ten to thirty feet above the ocean;... | |
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find that it produces a corresponding influence on the scenery of the country; for it runs out like a step beyond the foot of the chalkhills, and constitutes a lower terrace, varying in breadth from a quarter of a mile to three miles, and following the... 
