The Sea-Cliff Vegetation of Shetland

1975 ◽  
Vol 2 (4) ◽  
pp. 297 ◽  
Author(s):  
F. B. Goldsmith
Keyword(s):  
Vegetatio ◽  
1985 ◽  
Vol 62 (1-3) ◽  
pp. 309-317 ◽  
Author(s):  
Andrew J. C. Malloch ◽  
Joseph F. Bamidele ◽  
Anne M. Scott

2000 ◽  
Author(s):  
Charles B. Snell ◽  
Kenneth R. Lajoie ◽  
Edmund W. Medley
Keyword(s):  
El Niño ◽  
El Nino ◽  

2017 ◽  
Vol 38 (8-10) ◽  
pp. 2464-2479 ◽  
Author(s):  
John Barlow ◽  
Jamie Gilham ◽  
Ignacio Ibarra Cofrã
Keyword(s):  

1871 ◽  
Vol 8 (85) ◽  
pp. 303-312 ◽  
Author(s):  
D. Mackintosh

Boulder-scars.—From Maryport to Parkgate, the E. coast of the Irish Sea at intervals exhibits accumulations or concentrations of large boulders, which are locally called scars. They may be seen in all stages of formation, from the denudational area, where they are in course of being left by the washing away of the clayey matrix, to the depositional area, where they have become half-covered with recent sand and shingle. In many places (as between Seascale and near Silecroft) there are so many boulders within a small area as to show that a considerable thickness of the clay must have been removed. With the exception of having tumbled down as the cliffs were undermined and worn back by the sea, many of the boulders may still rest nearly in the positions they occupied in the clay, but (as is evidenced on the coast at Parkgate) others, up to a great diameter, may have been shifted horizontally. Some of the scars exist where the Boulder-clay would appear to have risen up into ridges or mounds, as no clay is now found opposite to them at the base of the sea-cliff. Others are clay and boulder plateaux, visibly connected with the cliff-line. Most of the scars, I believe, are remnants of the great Lower Brown Boulder-clay. The most conspicuous boulder in the scars S.W. of Bootle, is Eskdale-fell granite, accompanied by a little Criffell granite, and a great number of the usual felspathic erratics.


1996 ◽  
Vol 74 (4) ◽  
pp. 607-617 ◽  
Author(s):  
Victoria A. Nuzzo

Vegetational structure of exposed dolomitic cliffs in the driftless region of northwest Illinois was quantified from 186 quadrats on five cliffs. All cliffs were sparsely vegetated, with a total of 41 species (14 lichen and 27 vascular) recorded in the upper 6 m. On all cliffs, cover averaged 16.03%, with lichen contributing 10.23% cover and vascular vegetation 5.80% cover. Seventy percent of all vegetation grew within 3 m of the cliff top. Linear regression indicated that both cover and density of vascular, but not lichen, flora increased with increased fracturing and decreased with distance from the cliff top. TWINSPAN arranged the quadrats into five groups that differed in lichen and vascular cover and a sixth group that consisted of bare rock. Spatial distribution of the community groups occurred at a small scale, influenced by small scale differences in rock fracturing, slope, weathering, and likely moisture availability. Climbing significantly reduced lichen cover and lichen species density by 50%, from 13.7% cover and 2.4 species/0.25 m2 on unclimbed cliffs, to 6.7% cover and 1.2 species/0.25 m2 on climbed cliffs. Climbing did not have an apparent effect on vascular vegetation, which ranged from 2.74 to 10.62% cover on individual cliffs. Total plant cover averaged 19.7% on three unclimbed cliffs and 12.3% on two climbed cliffs, because of the impact on lichen cover. Although climbed cliffs had lower lichen cover, distribution of TWINSPAN-defined community groups was similar on both climbed and unclimbed cliffs, indicating that environmental and physical variables were the primary determinants of cliff flora on these vertical exposed cliffs. Keywords: cliff, vegetation, lichen, rock climbing, rock fractures.


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