標(biāo)題: Titlebook: Geology and Scenery in the Lake District; F. Moseley Textbook 1986Latest edition Macmillan Publishers Limited 1986 District.geology.lake [打印本頁(yè)] 作者: melancholy 時(shí)間: 2025-3-21 18:53
書目名稱Geology and Scenery in the Lake District影響因子(影響力)
書目名稱Geology and Scenery in the Lake District影響因子(影響力)學(xué)科排名
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書目名稱Geology and Scenery in the Lake District網(wǎng)絡(luò)公開度學(xué)科排名
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書目名稱Geology and Scenery in the Lake District讀者反饋學(xué)科排名
作者: iodides 時(shí)間: 2025-3-21 21:29 作者: abstemious 時(shí)間: 2025-3-22 03:39
Glacial and Solid Geology of the Buttermere Area (1:25 000 map NY11),geology and the solid rocks. It is not an arduous climb from Newlands Pass at 340 metres to High Snockrigg at 530 metres (NY 187 169), and it is an advantage to go on a clear day armed with binoculars when all the details of the topography can be picked out (figures 10, 11 and 12).作者: 繁殖 時(shí)間: 2025-3-22 06:25
The Borrowdale Volcanics of Fleetwith Pike and Honister (1:25 000 map NY21),rnscale Beck are composed of hard volcanic rocks which form steep crags and escarpments so that the base of the volcanics can be easily traced from Fleetwith Edge to Warn-scale Beck. The volcanic rocks are mostly lava flows with subsidiary tuffs, the lavas becoming dominant in the lower part of the 作者: 靦腆 時(shí)間: 2025-3-22 11:36 作者: Negotiate 時(shí)間: 2025-3-22 13:07 作者: Negotiate 時(shí)間: 2025-3-22 18:21
The Band to Bowfell (1:25 000 map NY20), then branches, with Crinkle Crags to the left and Bowfell to the right. Many years ago I recall walking along this path to Bowfell and being completely mystified by the geology of the Band, even though there are numerous outcrops. This is a problem which is resolved by distant views such as those o作者: 生氣的邊緣 時(shí)間: 2025-3-22 21:58
Helm Crag, Grasmere (1:25 000 map NY30),at the ascent of Helm Crag with its beautiful views all the way to the summit, is one of the best known. It is not an arduous walk; I have seen many a three-year-old cantering along the summit ridge, and it is easily accessible from Grasmere village. A convenient car park is indicated on figure 46 (作者: 騷擾 時(shí)間: 2025-3-23 05:24
Dove Crag (1:25 000 map NY31),strict that geological structure is not immediately apparent in the distant views of fellsides and has to be cultivated and reconsidered after careful inspection. Dove Crag is made of tuff, formerly volcanic ash, thrown out by the explosive activity of the Borrowdale Volcano and subsequently tilted 作者: 障礙物 時(shí)間: 2025-3-23 09:14 作者: 令人發(fā)膩 時(shí)間: 2025-3-23 10:18
Tarn Hows and the Coniston Limestone (1:25 000 maps NY30 and SD39),ooded, supplied with concealed car parks and well provided with footpaths, some of which cater for wheel-chairs. It is a place for a delightful family stroll, one which includes toddlers and grandparents. It is also a place of great geological interest. The junction between the Borrowdale Volcanics 作者: endure 時(shí)間: 2025-3-23 14:28
The Brathay Flags of Banishead, Coniston (1:25 000 map SD29),he dip is usually to the south-east at 30° to 40°, although there are a few minor folds in some areas, Tarn Hows for example. The lithology is unique in the Lake District, consisting of uniform, fine-scale alternations of paler silt and darker mud as shown on figure 58. It will be noticed that there作者: 貪婪地吃 時(shí)間: 2025-3-23 19:21 作者: DUCE 時(shí)間: 2025-3-23 23:26
The Coniston Grits and Bannisdale Slates of Shap (1:25 000 maps NY50 and NY60),hap Wells. The area south of Shap Summit described here is perhaps not so well known but it is interesting. The exposed rocks are Coniston Grits and Bannisdale Slates of Silurian age, outcropping in the major Bannis-dale Syncline which crosses the greater part of the Lake District. It will be notice作者: Limousine 時(shí)間: 2025-3-24 04:46 作者: heirloom 時(shí)間: 2025-3-24 07:48
Conclusion,ion. However, the topography and geology are diverse and there are areas and subjects I have not dealt with. The geological literature on the Lake District is enormous, and even before 1973, when the Cumberland Geological Society published R. A. Smith’s bibliography, there were more than 1000 books 作者: Foreknowledge 時(shí)間: 2025-3-24 12:37
,Einführung: Beispiele und Grundbegriffe,with at least some of the fundamentals. This is not necessarily so, however, and many who are expert in their own field can easily think that other disciplines are too specialised for their attention, that the subject matter may not interest them, or that there is little time in a busy life to maste作者: 配偶 時(shí)間: 2025-3-24 16:15 作者: gimmick 時(shí)間: 2025-3-24 19:09
,Erforschung der Differenzf?higkeit,geology and the solid rocks. It is not an arduous climb from Newlands Pass at 340 metres to High Snockrigg at 530 metres (NY 187 169), and it is an advantage to go on a clear day armed with binoculars when all the details of the topography can be picked out (figures 10, 11 and 12).作者: 合法 時(shí)間: 2025-3-25 00:10 作者: blight 時(shí)間: 2025-3-25 04:06 作者: 火車車輪 時(shí)間: 2025-3-25 07:40 作者: 尖牙 時(shí)間: 2025-3-25 14:36 作者: foodstuff 時(shí)間: 2025-3-25 19:06 作者: 希望 時(shí)間: 2025-3-25 23:20 作者: 鞠躬 時(shí)間: 2025-3-26 01:02 作者: 修飾語(yǔ) 時(shí)間: 2025-3-26 06:20 作者: minion 時(shí)間: 2025-3-26 11:45
Morphogenetic movements in plantshe dip is usually to the south-east at 30° to 40°, although there are a few minor folds in some areas, Tarn Hows for example. The lithology is unique in the Lake District, consisting of uniform, fine-scale alternations of paler silt and darker mud as shown on figure 58. It will be noticed that there作者: laceration 時(shí)間: 2025-3-26 14:26 作者: 承認(rèn) 時(shí)間: 2025-3-26 20:11 作者: MUMP 時(shí)間: 2025-3-26 22:47 作者: 尖叫 時(shí)間: 2025-3-27 03:41 作者: interference 時(shí)間: 2025-3-27 06:31
https://doi.org/10.1007/978-1-349-08762-4District; geology; lake作者: badinage 時(shí)間: 2025-3-27 12:37 作者: Demonstrate 時(shí)間: 2025-3-27 15:41 作者: macabre 時(shí)間: 2025-3-27 19:58
,Erforschung der Differenzf?higkeit,geology and the solid rocks. It is not an arduous climb from Newlands Pass at 340 metres to High Snockrigg at 530 metres (NY 187 169), and it is an advantage to go on a clear day armed with binoculars when all the details of the topography can be picked out (figures 10, 11 and 12).作者: 氣候 時(shí)間: 2025-3-27 22:52 作者: defibrillator 時(shí)間: 2025-3-28 05:39
Glacial and Solid Geology of the Buttermere Area (1:25 000 map NY11),geology and the solid rocks. It is not an arduous climb from Newlands Pass at 340 metres to High Snockrigg at 530 metres (NY 187 169), and it is an advantage to go on a clear day armed with binoculars when all the details of the topography can be picked out (figures 10, 11 and 12).作者: 羅盤 時(shí)間: 2025-3-28 09:15 作者: Valves 時(shí)間: 2025-3-28 12:10 作者: auxiliary 時(shí)間: 2025-3-28 16:28 作者: 黑豹 時(shí)間: 2025-3-28 21:24 作者: 喚醒 時(shí)間: 2025-3-29 00:03
The Brathay Flags of Banishead, Coniston (1:25 000 map SD29),in the Lake District, consisting of uniform, fine-scale alternations of paler silt and darker mud as shown on figure 58. It will be noticed that there are approximately 10 layers per centimetre. The indications are that these striped mudstones accumulated quietly and steadily in a clay-rich sea.作者: CLAIM 時(shí)間: 2025-3-29 06:27
The Bannisdale Slates of Blawith Common and Beacon Tarn (1:25 000 maps SD28 and SD29),he rocks fall within the Bannisdale Slate Formation of Silurian age. They are banded mudstones with occasional massive greywacke sandstone ribs, which are more resistant to erosion and form ridges as indicated on figure 60. The banding in the mudstones is caused by the numerous paler silty laminae.作者: 滔滔不絕地說(shuō) 時(shí)間: 2025-3-29 10:10
Whitbarrow and the Carboniferous Limestone (1:25 000 map SD48),opping to investigate. Indeed it compares in beauty with any part of the Lake District, but it is limestone scenery and therefore quite different in character from other areas. A delightful walk starts near Witherslack Hall, and follows the footpath through the woods and on to the limestone pavements of Whitbarrow summit (figures 69 and 70).作者: Dna262 時(shí)間: 2025-3-29 12:15 作者: 通便 時(shí)間: 2025-3-29 15:56
,Einführung: Beispiele und Grundbegriffe, they are kept simple and not confused by unnecessary jargon. I aim therefore to interpret the geological landscape of the Lake District so that those physically active members of our community who derive pleasure from fell walking will gain the added interest of knowing something of the ways in which the mountains were formed.作者: 牛馬之尿 時(shí)間: 2025-3-29 21:29 作者: 寬容 時(shí)間: 2025-3-30 02:35
,Differenzialgleichungen – wozu?,ften a question of ‘not being able to see the wood for the trees’, and I can think of a number of areas where the geology is obvious on aerial photographs but difficult to comprehend on the ground. On figure 24 the layers of rock can be seen to be inclined from left to right, that is towards the NNE at about 15° to 20°.作者: 希望 時(shí)間: 2025-3-30 06:53 作者: instate 時(shí)間: 2025-3-30 10:05
Performance Measurement in Supply Chains,is the deceiver; a compass and adequate clothing in a rucksack break the spell, and will also save Mountain Rescue teams a lot of bother. In winter, conditions can be Alpine with cornices overlapping the north-facing precipices, and suitable gear for these conditions is necessary.作者: Loathe 時(shí)間: 2025-3-30 14:26
Introduction, they are kept simple and not confused by unnecessary jargon. I aim therefore to interpret the geological landscape of the Lake District so that those physically active members of our community who derive pleasure from fell walking will gain the added interest of knowing something of the ways in which the mountains were formed.作者: Malcontent 時(shí)間: 2025-3-30 20:32
Styhead to Allen Crags (1:25 000 map NY20),ry’s Bridge Formation are acid lavas (dacites) and ignimbrites (figures 37 and 38). The Seathwaite Fells Tuffs rest on these rocks with a sharp junction which can be followed around Scafell and Bowfell and into Langdale where it traverses the higher parts of the Langdale Pikes (Moseley, 1983a, page 80).作者: 船員 時(shí)間: 2025-3-30 23:24 作者: Condescending 時(shí)間: 2025-3-31 02:51
The Band to Bowfell (1:25 000 map NY20), bed of lava or ignimbrite (see also figures 36 and 40). To examine the geology, the ascent of the Band should be accomplished in easy stages, otherwise interesting outcrops will be missed; it also provides a good excuse for more elderly geologists to pause for breath.作者: 樹木中 時(shí)間: 2025-3-31 07:55
