The Scenery of Scotland: Viewed in Connexion with Its Physical GeologyMacmillan, 1887 - 481 páginas |
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Página 23
... continuous strip of sandy ridges along the western coasts of Bernera and North and South Uist . Again , on the west sides of the islands of Coll and Tiree , and in Macrihanish Bay , Cantire , similar accumulations may be seen . Even in ...
... continuous strip of sandy ridges along the western coasts of Bernera and North and South Uist . Again , on the west sides of the islands of Coll and Tiree , and in Macrihanish Bay , Cantire , similar accumulations may be seen . Even in ...
Página 28
... continuously across from side to side of the dell , thus again demonstrating that the gorge is not a mere fissure opened by some force acting from below ( see Fig . 79 ) . Behind the cascade , the face of rock is kept constantly dank ...
... continuously across from side to side of the dell , thus again demonstrating that the gorge is not a mere fissure opened by some force acting from below ( see Fig . 79 ) . Behind the cascade , the face of rock is kept constantly dank ...
Página 62
... continuous line of mural precipice . Its two dominant structures , bedding and jointing , manifest their influence everywhere in the character of these cliffs . The strata , for the most part gently inclined , consist of thin ...
... continuous line of mural precipice . Its two dominant structures , bedding and jointing , manifest their influence everywhere in the character of these cliffs . The strata , for the most part gently inclined , consist of thin ...
Página 68
... continuous tract of firm ground . Nay , it appears that during the ten years previous to 1816 , the channel had been worn down at least two feet . Probably no part of the British coast - line affords such striking evidence of the ...
... continuous tract of firm ground . Nay , it appears that during the ten years previous to 1816 , the channel had been worn down at least two feet . Probably no part of the British coast - line affords such striking evidence of the ...
Página 87
... continuous rampart , which is continually growing by the addition of fresh materials as the ice reaches its farthest limit . Should a period of milder temperature come and cause the glacier to retire up the valley , this rampart - like ...
... continuous rampart , which is continually growing by the addition of fresh materials as the ice reaches its farthest limit . Should a period of milder temperature come and cause the glacier to retire up the valley , this rampart - like ...
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TĂ©rminos y frases comunes
Ayrshire basalt basin beds boulder-clay boulders Caithness Carboniferous cliffs Clyde coast coast-line conglomerate conspicuous corries crags crest deep denudation deposits descend district drainage dykes east erosion escarpments feet Firth Firth of Clyde frosts geological structure Glacial glaciers Glen gneiss granite greywacke height high grounds Highlands hills hollow ice-sheet ice-worn island lake land landscape limestone Loch Loch Fyne Lomond Lower Old Red Lowlands marked mass Midland Valley miles moraines Moray Firth mounds mountains narrow northern Ochil Ochil Hills Old Red Sandstone once peat Pentland Hills Permian plain precipices present quartzite railway raised beach ravine region ridges rise river rocky runs sand scenery schists Scotland Scottish sea-lochs seen shores side Silurian Skye slopes smooth Southern Uplands stone strata stream striæ striking sub-aërial summit surface Sutherland table-land terrace traced tract volcanic rocks waste watershed western wide worn
Pasajes populares
Página 374 - As a huge stone is sometimes seen to lie Couched on the bald top of an eminence ; Wonder to all who do the same espy, By what means it could thither come, and whence; So that it seems a thing endued with sense : Like a sea-beast crawled forth, that on a shelf Of rock or sand reposeth, there to sun itself...‎
Página 7 - Be gather'd now, ye waters under heaven, Into one place, and let dry land appear. Immediately the mountains huge appear Emergent, and their broad bare backs upheave Into the clouds, their tops ascend the sky.‎
Página 316 - Urn-like it was in shape, deep as an urn ; With rocks encompassed, save that to the south Was one small opening, where a heath-clad ridge Supplied a boundary less abrupt and close ; A quiet treeless nook, with two green fields, A liquid pool that glittered in the sun, And one bare dwelling ; one abode, no more...‎
Página 72 - ... acclivity to a distance almost incredible. In the winter of 1802, a tabular-shaped mass, eight feet two inches by seven feet, and five feet one inch thick, was dislodged from its bed, and removed to a distance of from eighty to ninety feet.‎
Página 161 - Inscribed, as with the silence of the thought, Upon its bleak and visionary sides, The history of many a winter storm, Or obscure records of the path of fire.‎
Página 11 - If, indeed, a river consisted of a single stream without branches, running in a straight valley, it might be supposed that some great concussion, or some powerful torrent, had opened at once the channel by which its waters are conducted to the ocean; but, when the usual form of a river is considered, the trunk divided into many branches, which rise at...‎
Página 244 - From dark and icy caverns called you forth, Down those precipitous, black, jagged rocks, For ever shattered and the same for ever?‎
Página 59 - This massive structure, rising 112 feet above the sea-level, 'is literally buried in foam and spray to the very top during ground swells when there is no wind.' Experiments were made there from the middle of September 1844 to the end of March 1845, and the greatest recorded pressure was 3013 pounds on the square foot.‎
Página 59 - It is certain, however, that within a recent period the sea has made such an impression upon the sands of Barrey, on the northern side of the Tay, that the light-houses at the entrance of...‎