Universal Geography, Or, a Description of All Parts of the World, on a New Plan, According to the Great Natural Divisions of the Globe: Theory, or mathematical, physical, and political principles of geographyWells and Lilly, 1826 |
Vyhľadávanie v obsahu knihy
Výsledky 1 - 5 z 100.
Strana v
... manner as to furnish the reader with a lively picture of the whole terraqueous globe , with all its different countries - the memorable places which they contain - the tribes of men by which they have been successively peopled , and ...
... manner as to furnish the reader with a lively picture of the whole terraqueous globe , with all its different countries - the memorable places which they contain - the tribes of men by which they have been successively peopled , and ...
Strana vii
... manner ; — that in the more advanced seminaries it may be put into the hands of pupils ; -and that it will not be an unacceptable present to adults , who have long passed their period of tuition , and wish to acquire instruction by ...
... manner ; — that in the more advanced seminaries it may be put into the hands of pupils ; -and that it will not be an unacceptable present to adults , who have long passed their period of tuition , and wish to acquire instruction by ...
Strana ix
... manner . An order purely geogra phical must apparently have destroyed the political and moral connections of the different portraits which we had to present . An order purely political would have injured the physical delineation of the ...
... manner . An order purely geogra phical must apparently have destroyed the political and moral connections of the different portraits which we had to present . An order purely political would have injured the physical delineation of the ...
Strana xviii
... much interesting informa- tion as possible in the easiest manner , may peruse our work without suffering himself to be in any degree impeded by the references . CONTENTS OF VOL . I. BOOK I. Theory of Geography xviii PREFACE .
... much interesting informa- tion as possible in the easiest manner , may peruse our work without suffering himself to be in any degree impeded by the references . CONTENTS OF VOL . I. BOOK I. Theory of Geography xviii PREFACE .
Strana xxxv
... Manner in which the sea produces changes - Changes in the eastern part of the Mediterranean , Changes in the western part of the Mediterranean , Changes in the Atlantic Ocean - Changes upon the coast of Holland , • Changes upon the ...
... Manner in which the sea produces changes - Changes in the eastern part of the Mediterranean , Changes in the western part of the Mediterranean , Changes in the Atlantic Ocean - Changes upon the coast of Holland , • Changes upon the ...
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Iné vydania - Zobraziť všetky
Časté výrazy a frázy
according Africa amongst ancient angle animals appears Asia atmosphere axis basalt beds Bergmann BOOK calcareous called cause centre chains circle climate coasts cold colour consider contain countries crystals currents declivity Delamétherie direction distance earth east ecliptic elevated equal equator extent feet feldspar fluid fossil geography globe granite Haüy heat hemisphere Hippocrates horizon Iceland iron islands kind lakes land leagues less longitude marine masses measure Mémoires meridian metal monsoon moon motion moun mountains myriametres nature neral observed ocean parallel particles pass perpendicular Peru petrifactions Physique plains plane polar pole porphyry primitive principal projection pyrites quantity quartz racter radius rays regions right line rivers rocks schist Siberia side sometimes species sphere stereographic projection Strabo strata substances subterraneous sulphur surface tains talc terrestrial theory tion toises torrid zone trace tufa vapours vegetable volcanic Voyage winds
Populárne pasáže
Strana 473 - aurora borealis, reflected by the snow, dispels the darkness of the polar night. The days for several months, though of a monotonous magnificence, astonishingly accelerate the growth of vegetation. In three days, or rather three times twenty-four hours, the snow is melted, and the flowers begin to blow.
Strana 185 - greater number of the principal mountains have one of their sides very steep, and the other of a very " gradual slope.* The Alps, for example, are much more rapid in their descent on the Italian side than on that of Switzerland. On the contrary, the Dophrines, or Scandinavian Alps, have a much steeper declivity to the
Strana 502 - that the grounds near Ravenna has sunk to such a degree, that the pavement of the cathedral is only six inches above the level of high water; but, at the same time, the land is extended in such a manner that this town, formerly situate in the midst of marshes, and canals, and furnished with an
Strana 361 - causes which are local, and sometimes illusory. It is said that the Mediterranean Sea, in its upper part, has sometimes a purple tint. In the gulf of Guinea, the Sea is white, and around the Maldive Islands black. The Vermeille, or
Strana 6 - could only be represented by a grain of sand less than one-twentieth of an inch in thickness. Irregularities so imperceptible do not deserve to be taken into consideration. We shall see, in the following Book, that the true differences which exist between our globe
Strana 361 - a blue shade to distant mountains, and which give the atmosphere its azure hue. The rays of blue light, being the most refrangible, pass in the greatest quantity through the aquatic fluid, which, from its density and depth, makes them undergo a strong refraction. The other shades in the
Strana 472 - the proximity of very high mountains, covered with perpetual snow; the trade winds, and the periodical inundations, equally contribute to diminish the heat. This is the reason why, in the torrid zone, we meet with all kinds of climates. The plains are burnt up by the heat of the sun. All the eastern coasts of the great continents,
Strana 357 - true surface of our planet The only exception to this position, may perhaps be found in gulfs and inland seas, which have only a slight communication with the ocean. In these parts of the sea. the level of the water may sometimes be a little more elevated than in the ocean. It is alleged that the Dutch
Strana 24 - of the ecliptic causes the arc of the equator, which passes the meridian in the same time with the diurnal arc of the ecliptic, to be not always equal to it, but to be sometimes greater and sometimes less. With regard to the