The rudiments of physical geography for the use of Indian schoolsMacmillan, 1874 - 169 pages |
From inside the book
Results 6-10 of 24
Page 57
... Himálaya is made up of rocks more or less similar , and so is all the northern part of the Gáro and Khási Hills . When- ever a series of stratified rocks can be followed down to their lowest layer , as a rule the bottom layer is found ...
... Himálaya is made up of rocks more or less similar , and so is all the northern part of the Gáro and Khási Hills . When- ever a series of stratified rocks can be followed down to their lowest layer , as a rule the bottom layer is found ...
Page 60
... Himálaya , generally breaking into rocks of the metamorphic class . In appearance , and in the mine- rals that compose them , they much resemble these latter , except that they rarely show any trace of that layer - like arrangement of ...
... Himálaya , generally breaking into rocks of the metamorphic class . In appearance , and in the mine- rals that compose them , they much resemble these latter , except that they rarely show any trace of that layer - like arrangement of ...
Page 65
... Himálaya and the Punjab , which have been occupied by the sea , in part at least , through very long periods , consist of rocks which represent the majority of the formations enumerated in the Table . It is not in general so easy to ...
... Himálaya and the Punjab , which have been occupied by the sea , in part at least , through very long periods , consist of rocks which represent the majority of the formations enumerated in the Table . It is not in general so easy to ...
Page 74
... Himálaya . They are never met with in the middle of great river plains , where the deposits formed by the river are of considerable thickness . It would be in vain therefore to search for such springs in the rice fields of Lower Bengal ...
... Himálaya . They are never met with in the middle of great river plains , where the deposits formed by the river are of considerable thickness . It would be in vain therefore to search for such springs in the rice fields of Lower Bengal ...
Page 85
... Himálaya and the Andes . Another effect of this contor- tion and squeezing is a great change in the character of the rocks , viz . , that which was described in the fourth chapter as metamorphism . The rocks have been so heated by the ...
... Himálaya and the Andes . Another effect of this contor- tion and squeezing is a great change in the character of the rocks , viz . , that which was described in the fourth chapter as metamorphism . The rocks have been so heated by the ...
Other editions - View all
The Rudiments of Physical Geography for the Use of Indian Schools Henry Blanford Limited preview - 2023 |
The Rudiments of Physical Geography for the Use of Indian Schools Henry Blanford Limited preview - 2023 |
The Rudiments of Physical Geography for the Use of Indian Schools Henry Francis Blanford No preview available - 2016 |
Common terms and phrases
animals Asia atmosphere ball basin Bay of Bengal become Beng Bengal blows body bottom Calcutta carbonic acid carried channel CHAP chapter Chilka Lake clay coast cold contains cooled Cuttack delta deposited depth distance drainage drainage basin earth elevated Europe evaporation falls feet flood flows forests formation formed former geological glaciers GLOSSARY gneiss gradually gravitation greater heat height hills Himálaya India interior islands Khasi Hills kind lakes land layers learned live Mahánadi mass melted metamorphic rocks miles monsoon moon motion mountain ranges névé Northern ocean Physical Geography plains plants produced rain rainfall region river roches moutonnées rocks round salt sand sandstone sedimentary sedimentary rocks seen shells Sikkim slopes snow solid sometimes Southern stratified stream surface temperature termed Tibet tides tract trees tropical valley vapour vegetation volcano W. T. Blanford waves winds winter
Popular passages
Page 52 - THERE rolls the deep where grew the tree. O earth, what changes hast thou seen ! There where the long street roars, hath been The stillness of the central sea. The hills are shadows, and they flow From form to form, and nothing stands ; They melt like mist, the solid lands, Like clouds they shape themselves and go. But in my spirit will I dwell, And dream my dream, and hold it true ; For tho' my lips may breathe adieu, I cannot think the thing farewell.
Page 67 - The mind seemed to grow giddy by looking so far into the abyss of time; and while we listened with earnestness and admiration to the philosopher who was now unfolding to us the order and series of these wonderful events, we became sensible how much farther reason may sometimes go than imagination can venture to follow.
Page 92 - had the primeval world been constructed as it now exists, time enough has elapsed, and force enough directed to that end has been in activity, to have long ago destroyed every vestige of land.
Page 119 - What is this murmur ? Is it the sound of cannon in the distance ? Is Gandgarh bellowing? Is it thunder?' Suddenly some one cried out, ' The river's come.' And I looked and perceived that all the dry channels were already filled, and that the river was racing down furiously in an absolute wall of mud, for it had not at all the colour or appearance of water.
Page 119 - Khan. Part of the force was at that moment in hot pursuit, or the ruin would have been wider. The rest ran, some to large trees, which were all soon uprooted and borne away ; others to rocks, which were speedily buried beneath the waters. Only they escaped who took at once to the mountain side. About 500 of these troops were at once swept to destruction.