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

melancholy

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




書目名稱Geology and Scenery in the Lake District網(wǎng)絡(luò)公開度




書目名稱Geology and Scenery in the Lake District網(wǎng)絡(luò)公開度學(xué)科排名




書目名稱Geology and Scenery in the Lake District被引頻次




書目名稱Geology and Scenery in the Lake District被引頻次學(xué)科排名




書目名稱Geology and Scenery in the Lake District年度引用




書目名稱Geology and Scenery in the Lake District年度引用學(xué)科排名




書目名稱Geology and Scenery in the Lake District讀者反饋




書目名稱Geology and Scenery in the Lake District讀者反饋學(xué)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

靦腆

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

生氣的邊緣

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 (

騷擾

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

障礙物