Titlebook: Geology and Scenery in the Lake District; F. Moseley Textbook 1986Latest edition Macmillan Publishers Limited 1986 District.geology.lake

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书目名称Geology and Scenery in the Lake District影响因子(影响力)




书目名称Geology and Scenery in the Lake District影响因子(影响力)学科排名




书目名称Geology and Scenery in the Lake District网络公开度




书目名称Geology and Scenery in the Lake District网络公开度学科排名




书目名称Geology and Scenery in the Lake District被引频次




书目名称Geology and Scenery in the Lake District被引频次学科排名




书目名称Geology and Scenery in the Lake District年度引用




书目名称Geology and Scenery in the Lake District年度引用学科排名




书目名称Geology and Scenery in the Lake District读者反馈




书目名称Geology and Scenery in the Lake District读者反馈学科排名

iodides

abstemious

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).

繁殖

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

腼腆

Negotiate

Negotiate

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

生气的边缘

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 (

骚扰

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

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