scholarly journals XVIII.—Ants from North and South-West Australia (G.F. Hill, Rowland Turner) and Christmas Island, Straits Settlements.—Part II

1915 ◽  
Vol 15 (86) ◽  
pp. 232-239 ◽  
Author(s):  
W.C. Crawley
Keyword(s):  
Christmas Island ◽  
South West ◽  
North And South

TBE in United Kingdom

2020 ◽  
Keyword(s):  
United Kingdom ◽  
Clinical Disease ◽  
England And Wales ◽  
Probable Case ◽  
The United Kingdom ◽  
South West ◽  
Louping Ill ◽  
The Uk ◽  
North And South ◽  
South West England

Until 2019, TBE was considered only to be an imported disease to the United Kingdom. In that year, evidence became available that the TBEV is likely circulating in the country1,2 and a first “probable case” of TBE originating in the UK was reported.3 In addition to TBEV, louping ill virus (LIV), a member of the TBEV-serocomplex, is also endemic in parts of the UK. Reports of clinical disease caused by LIV in livestock are mainly from Scotland, parts of North and South West England and Wales.4

The Petrography of the Sands of the Upper Lias and Lower Inferior Oolite in the West of England

1924 ◽  
Vol 61 (6) ◽  
pp. 246-264 ◽  
Author(s):  
P. G. H. Boswell
Keyword(s):  
Mineralogical Composition ◽  
Fine Sand ◽  
General Character ◽  
Reciprocal Relation ◽  
The South ◽  
The West ◽  
South West ◽  
North And South ◽  
Pale Green

The main conclusions of the paper may be briefly stated thus:—1. The deposits, which are of neritic facies, possess a characteristic and peculiar mechanical and mineralogical composition, differing therein from any other British deposit.2. They exhibit a general constancy in grade from the Dorset coast to the Cotteswolds. Within this limit they conform to two chief types containing respectively 40 to 50 and 60 to 80 per cent, of the very fine sand grade (greater than 0·05 and less than 0·1 mm.). No variation of mechanical composition with hemeral change can be observed.3. The sands are blue and glauconitic in depth. At the surface they are decalcified and are yellow and brown as a result of oxidation. Minerals such as pyrite and pyrrhotite occur only in depth.4. The mineralogical composition indicates an abundance of highly angular brownish-pink to colourless garnets (possibly derived from rocks like those of the Lizard), but few red or purplish-red varieties; also of micas (including a pseudo-uniaxial, pale-green to colourless variety), together with chlorite, chloritoid, kyanite, staurolite, orthoclase, and microcline.5. Tourmaline is only moderately common and is always the grey-brown variety.6. The abundance of titanium-minerals is characteristic of the deposits. Red and yellow varieties of rutile and sagenite-webs are exceedingly abundant, and anatase, brookite, and sphene are locally so. A reciprocal relation may exist between the occurrence of sphene, ilmenite, and the oxides of titanium.7. Epidote and glaucophane are rare.8. Chlorite, chloritoid, glaucophane, kyanite, and staurolite increase in quantity as the deposits are traced southwards.9. A change in lithology and mineralogy sets in as the deposits are followed north-eastwards into the Midlands and Yorkshire.10. The sands differ markedly in petrology from the various Palæozoic rocks of Wales and the West Country, from the Trias, and from the Cretaceous and Eocene of Devon and Dorset.11. The Ordovician, Domerian, Toarcian, and Aalenian of Normandy and Brittany have been examined petrologically for purposes of comparison, but show little resemblance to the sediments under discussion, having been derived locally from the Palæozoic and pre-Cambrian rocks.12. It is concluded that the Lias–Inferior Oolite sands have been derived from the south or south-west, notably from rocks like those of western Brittany.13. The rise of the Mendip axis was not sufficiently complete at this time to cut off the supply of sediment from the south or south-west. The deposits north and south of the ridge have the same general character.

scholarly journals Celtic spirituality and contemporary environmental issues

2015 ◽  
Vol 71 (3) ◽  
Author(s):  
Graham Duncan
Keyword(s):  
20Th Century ◽  
Environmental Issues ◽  
Environmental Crisis ◽  
Ethical Perspective ◽  
Religious Traditions ◽  
The North ◽  
South West ◽  
Key Aspects ◽  
North And South

Celtic spirituality has a long and distinguished ancestry with its origins in pre-Christian times. It was inculturated among peoples in the far west of Europe, particularly in Ireland, Scotland and the north and south-west of England. It was different from Roman Christianity in distinct ways until the mid-7th century CE when Roman Christianity became the norm in Britain and Ireland. This spirituality has endured throughout the centuries and has experienced a revival from the latter half of the 20th century. From its inception, it has been closely linked to the environment. Over the years many key aspects of Celtic spirituality have been integrated in many religious traditions and shows similarities with and can contribute to a new ethical perspective on environmental issues. This article investigates the current environmental crisis from a faith perspective and attempts to draw lessons from Celtic traditions of spirituality in a scientific age.

scholarly journals Incipient Glacier Development within Katmai Caldera, Alaska

1957 ◽  
Vol 3 (21) ◽  
pp. 13-17
Author(s):  
E. H. Muller ◽  
H. W. Coulter
Keyword(s):  
Sea Level ◽  
Wall Rock ◽  
Crater Wall ◽  
The South ◽  
The Past ◽  
The North ◽  
South West ◽  
Direction Of Movement ◽  
North And South

AbstractAn unusual opportunity for the study of glaciers in the process of development is afforded in Katmaicaldera in south-western Alaska. A violent eruption in 1912 destroyed the summit of glacier-clad Mount Katmai, creating a caldera 4 km. wide and 800 m. deep. Ice cliffs produced by beheading of the glaciers have since thinned and shrunk away from the rim of the caldera, except in the south-west. There, local reversal of direction of movement has resulted in an ice fall which descends part way down the crater wall. In the past thirty years two small glaciers have formed, near 1525 m. above sea level, within the caldera on large masses of slumped wall-rock below the north and south rims respectively. Elsewhere the sheer walls of the crater descend so steeply to the level of the caldera lake that permanent snowbanks cannot accumulate. The lake, which continues to rise at a rate of more than five meters per year, is at present the primary deterring factor in glacier development in the caldera.

I 10, 10-11: Casa Degli Amanti

1997 ◽  
Author(s):  
Roger Ling ◽  
Paul Arthur ◽  
Georgia Clarke ◽  
Estelle Lazer ◽  
Lesley A. Ling ◽  
...  
Keyword(s):  
The Other ◽  
Central Axis ◽  
The South ◽  
The West ◽  
The North ◽  
Small Window ◽  
South West ◽  
Dining Room ◽  
North Wall ◽  
North And South

The casa degli amanti (house of the lovers), at the south-west corner of the insula, falls into two fairly distinct halves: the atrium complex, oriented on the street to the west, and the peristyle with its surrounding rooms, oriented on the street to the south and on the property boundary to the east. In the atrium complex, the atrium is misplaced to the south of the central axis, allowing space for two large rooms to the north, one of which was possibly a shop or workshop (5.50 m. × 4.70 m.), with a separate entry from the street (I 10, 10), while the other (5.80 m. × 4.50 m.), decorated with mythological wallpaintings and provided with a wide opening on to the peristyle, must have been a dining-room or oecus (room 8). Each of these had a segmental vault rising from a height of about 3.50 m. at the spring to slightly over 4 m. at the crown. In the first the vault is missing, but the holes for some of its timbers are visible in the east wall and a groove along the north wall marks the seating for the planking attached to them; at a higher level, in the north and south walls, are the remains of beam-holes for the joists of the upper floor or attic (see below). The arrangements in room 8 are now obscured by the modern vault constructed to provide a surface for the reassembled fragments of the ceiling-paintings; but the shape of the vault is confirmed by the surviving plaster of the lunettes, while a beam-hole for the lowest of the vault-timbers is visible above the corner of the western lunette in an early photograph (Superintendency neg. C 1944). The shop I 10, 10 had a small window high in the street wall to the south of Its entrance; whether there were any additional windows above the entrance, it is impossible to say, since this part of the wall is a modern reconstruction. Room 8 was lit by a splayed window cut in the angle of the vault and the eastern lunette, opening into the upper storey of the peristyle.

scholarly journals Celtic spirituality and the environment

2015 ◽  
Vol 71 (1) ◽  
Author(s):  
Graham Duncan
Keyword(s):  
New Age ◽  
Christian Spirituality ◽  
History Of Christianity ◽  
The North ◽  
South West ◽  
History Of ◽  
New Age Spirituality ◽  
North And South

Celtic spirituality has a long and distinguished ancestry with its origins in pre-Christian times. It was inculturated amongst peoples in the far west of Europe, particularly in Ireland, Scotland and the north and south west of England. It was different from Roman Christianity in distinct ways until the mid-7th century CE when Roman Christianity became the norm in Britain. It has experienced various revivals during the history of Christianity, with two contemporary expressions in New Age spirituality and Christian spirituality. From its inception, it has been closely linked to the environment.

scholarly journals Incipient Glacier Development within Katmai Caldera, Alaska

1957 ◽  
Vol 3 (21) ◽  
pp. 13-17 ◽  
Author(s):  
E. H. Muller ◽  
H. W. Coulter
Keyword(s):  
Sea Level ◽  
Wall Rock ◽  
Crater Wall ◽  
The South ◽  
The Past ◽  
The North ◽  
South West ◽  
Direction Of Movement ◽  
North And South

Abstract An unusual opportunity for the study of glaciers in the process of development is afforded in Katmaicaldera in south-western Alaska. A violent eruption in 1912 destroyed the summit of glacier-clad Mount Katmai, creating a caldera 4 km. wide and 800 m. deep. Ice cliffs produced by beheading of the glaciers have since thinned and shrunk away from the rim of the caldera, except in the south-west. There, local reversal of direction of movement has resulted in an ice fall which descends part way down the crater wall. In the past thirty years two small glaciers have formed, near 1525 m. above sea level, within the caldera on large masses of slumped wall-rock below the north and south rims respectively. Elsewhere the sheer walls of the crater descend so steeply to the level of the caldera lake that permanent snowbanks cannot accumulate. The lake, which continues to rise at a rate of more than five meters per year, is at present the primary deterring factor in glacier development in the caldera.

Sign in / Sign up

Export Citation Format

Share Document