The Geological Observer

الغلاف الأمامي
Longman, Brown, Green, and Longmans, 1851 - 846 من الصفحات
 

المحتوى

Beaches on the shores of land at the time of the Silurian deposits and
548
Beaches at the time of the lias
554
Overlap of the inferior oolite Mendip Hills
560
Elevation of land over a wide area
566
Stems of plants in their positions of growth in the coalmeasures
578
Marine remains in part of the coalmeasures
593
Raised seabottom round British Islands
599
Elevation or depression of the bottom in the ocean
605
Effects of earthquakes on seabottoms
611
Distribution of organic remains
621
Infusorial remains
630
Fossils amid old igneous products
637
Relative geological date of the Wicklow and Wexford granites
646
Dates of the Cornish and Devonian elvans
654
Outline of the granite range of Wicklow
660
Serpentine and diallage rock of Cornwall
668
Resemblances and differences between the ordinary granitic and horn
675
General character of igneous rocks
682
Consolidation and adjustment of the component parts of rocks
683
Spheroidal concretions in the Silurian rocks
689
Variable deposits of detrital matter
695
Alteration of rocks near granitic masses
701
Cleavage of rocks
707
237
711
Relative dates of cleavage
713
Directions and range of joints
719
Complication of bedding jointing and cleavage
725
254
728
Directions of mountain chains
732
Bending and folding of deposits in the Appalachian zone North America
739
266
744
Faults
745
Fallacious appearance from a single movement shifting various fissures
754
Inclination of faults
760
Deposits from solutions in fissures
769
286
778
Flats of lead ore in limestone districts
784
Modification of the contents of mineral veins in their depth and range
790
Sulphurets of lead and zinc converted into carbonates in mineral veins
800
Partial removal or denudation of rocks
809
Mountain ranges viewed on the large scale
834
Quiet rise and subsidence of land
840

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الصفحة 386 - ... feet deep. The bottom was covered with lava, and the south-west and northern parts of it were one vast flood of burning matter, in a state of terrific ebullition, rolling to and fro its " fiery surge
الصفحة 832 - THE METALLIFEROUS DEPOSITS OF CORNWALL AND DEVON ; with Appendices on Subterranean Temperature ; the Electricity of Rocks and Veins ; the Quantities of Water in the Cornish Mines ; and Mining Statistics.
الصفحة 329 - ... of the dense enamel, the inference is plain that the ligneous fibre must have entered in a larger proportion into the food of such extinct species. Forests of hardy trees and shrubs still grow upon the frozen soil of Siberia, and skirt the banks of the Lena as far north as latitude 60°. In Europe arboreal vegetation extends ten degrees nearer the pole, and the dental organization of the Mammoth proves that it might have derived subsistence from the leafless branches of trees, in regions covered...
الصفحة 169 - ... several are found in one region which do not range into the next above, whilst they extend to that below, or vice versa. Certain species have their maximum of development in each zone, being most prolific in individuals in that zone in which is their maximum, and of which they may be regarded as especially characteristic. Mingled with the true natives of every zone are stragglers, owing their presence to the action of the secondary influences which modify distribution.
الصفحة 337 - Tigers as large again as the biggest Asiatic species lurked in the ancient thickets; elephants of nearly twice the bulk of the largest individuals that now exist in Africa or Ceylon roamed in herds ; at least two species of rhinoceros forced their way through the primaeval forest ; and the lakes and rivers were tenanted by hippopotami as bulky, and with as great tusks as those of Africa.
الصفحة 246 - A GLACIER is AN IMPERFECT FLUID, OR A VISCOUS BODY. WHICH IS URGED DOWN SLOPES OF A CERTAIN INCLINATION BY THE MUTUAL PRESSURE OF ITS PARTS.
الصفحة 171 - ... the brachiopoda, also gives a character of colour to the fauna of this zone ; the Crustacea found in it are red. In the sixth zone the colours become brighter, reds and yellows prevailing, — generally, however, uniformly colouring the shell. In the fifth region many species are banded or clouded with various combinations of colours, and the number of white species has greatly diminished. In the fourth, purple hues are frequent, and contrasts of colour common. In the...
الصفحة 329 - Elephant prefers, will not enable us to determine, or even to offer a probable conjecture concerning that of the extinct species." The molar teeth of the Elephant possess, as we have seen, a highly complicated, and a very peculiar structure, and there are no other quadrupeds that derive so great a proportion of their food from the woody fibre of the branches of trees. Many mammals browse the leaves ; some small rodents gnaw the bark ; the Elephants alone tear down and crunch the branches, the vertical...
الصفحة 250 - The stone thus appeared to rise above the level of the glacier, supported on an elegant pedestal of beautifully veined ice. Each time I visited it, it was more difficult of ascent, and at last, on the 6th August the pillar of ice was thirteen feet high, and the broad stone so delicately poised on the summit of it, (which measured but a few feet in any direction,) that it was almost impossible to guess in what direction it would ultimately fall, although, by the progress of the thaw, its fall in the...
الصفحة 17 - ... southern hemispheres. 3. That there is no notable difference in sea-water under different meridians. 4. That there is no satisfactory evidence that the sea at great depths is more salt than at the...

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