Letters of karl Marx to Karl Blind

1938 ◽  
Vol 4 ◽  
pp. 153-160
Author(s):  
Gustav Mayer
Keyword(s):  
Karl Marx ◽  
Public Order ◽  
The South ◽  
South West ◽  
Diplomatic Immunity ◽  
First Time

Marx met the then 22 years old Blind) for the first time in May 1848, when he and Engels made their appearance in the revolutionary state of Baden (Germany), after the Neue Rheinische Zeitung had been suspended. At that time they declared to the members of the republican committee at Karlsruhe (Landesa usschuss), that they considered the revolt in the South-West of Germany irretrievably doomed to failure, if no decisive moves in Hungary or another revolution in Paris should come to its rescue. The only members of the committee who supported this opinion were, as stated by Engels), Karl Blind and Amand Gögg. Soon afterwards Marx and Blind met again in Paris. On September 5 Marx gave Blind's address to Freiligrath as his own. Blind had been sent to France by the revolutionary governments of Baden and the Palatinate as one of the members of the legation, which these two shortlived republics intended to establish there. But Louis Napoleon's government ignored this legation, and consequently did not respect Blind's diplomatic immunity, when the latter, soon after his arrival, proved to be involved in the abortive coup of Ledru-Rollin of June 13. Blind was placed under arrest and expelled from France on the same day, on the ground that his presence was “such as to disturb public order and calm”.

Protogeometric Vases from Amorgos in the Museum of the British School

1989 ◽  
Vol 84 ◽  
pp. 177-185
Author(s):  
R.W.V. Catling ◽  
R.E. Jones
Keyword(s):  
Chemical Analysis ◽  
Early History ◽  
The Other ◽  
The South ◽  
South West ◽  
British School ◽  
History Of ◽  
First Time

Two vases, a cup and an oinochoe, from Arkesine in south-west Amorgos are published for the first time. It is argued that both are probably Middle Protogeometric, one an import from Euboia, the other from the south-east Aegean; chemical analysis supports both attributions. Their implications for the early history of Amorgos are discussed.

Paramedics' perceptions and experiences of NHS 111 in the south west of England

2020 ◽  
Vol 12 (6) ◽  
pp. 227-234
Author(s):  
Joel S Phillips
Keyword(s):  
Structured Interview ◽  
Evidence Base ◽  
Ambulance Service ◽  
Telephone Triage ◽  
The South ◽  
Qualitative Research Design ◽  
South West ◽  
The Right ◽  
First Time ◽  
Gain Access

Background: NHS 111 is a non-emergency telephone triage service in England, where people with non-urgent health problems or questions can gain access to information and services. However, studies have demonstrated key problems with the burden it places on emergency and ambulance services. Aim: To add to the evidence base, this study explores the perceptions and experiences of paramedics who attend patients referred to the ambulance service by NHS 111. Methods: A qualitative research design was adopted and seven frontline paramedics who work in the south west of England were interviewed. Data were collected using semi-structured interview questions and thematically analysed. Findings: Key overarching themes identified included: non-clinical call handlers making clinical decisions; caution and liability; an unwarranted, increased demand on the ambulance service; inaccurate call prioritisation; and interprofessional conflict. Conclusion: Improvements need to be made to the NHS 111 service to ensure the triage software it uses is triaging and prioritising patients accurately and to minimise inappropriate referrals to the ambulance service, promoting the right care for patients the first time.

scholarly journals Ice-Shelf Flow at the Boundary of Crary Ice Rise, Antarctica

1988 ◽  
Vol 11 ◽  
pp. 8-13 ◽  
Author(s):  
R. A. Bindschadler ◽  
P. L. Vornberger ◽  
S .N. Stephenson ◽  
E. P. Roberts ◽  
S. Shabtaie ◽  
...  
Keyword(s):  
Surface Velocity ◽  
The South ◽  
Ice Shelf ◽  
West Side ◽  
North West ◽  
Ross Ice Shelf ◽  
South West ◽  
Lateral Tension ◽  
Free Block ◽  
First Time

Surface velocity and deformation, radar sounding, and aerial photography data are used to describe the flow of Ross Ice Shelf around Crary Ice Rise. A continuous band of crevasses around the ice rise now allows the complete boundary to be mapped for the first time. The dynamics of three distinctly different areas of ice flow are studied. Just up-stream of the ice rise, there is a region of ice rumples dominated by intense longitudinal compression (0.01 a−1) and lateral tension. On the south-west side of the ice rise, intense shear (0.03 a−1) dominates, with the boundary layer of affected ice-shelf motion extending over 20 km from the ice-rise edge into the ice shelf. North-west of the ice rise, a crevasse-free block of ice, 40 km × 7 km, appears to have separated from the main ice rise and is now moving with the ice shelf. We refer to such moving blocks of ice as rafts. The separation of this raft is calculated to have occurred 20 ± 10 years ago. Other possible rafts are identified, including one on the south-west side of the ice rise which appears to be in the process of separating. Mechanisms for the formation of rafts are discussed.

scholarly journals First record of shield-backed katydids in Madagascar with the description of a new genus and three new species (Orthoptera: Ensifera: Tettigoniidae: Tettigoniinae: Arytropteridini)

Zootaxa ◽  
2019 ◽  
Vol 4706 (4) ◽  
pp. 546-560
Author(s):  
SYLVAIN HUGEL
Keyword(s):  
New Species ◽  
New Genus ◽  
First Record ◽  
Taxonomic Position ◽  
The South ◽  
South West ◽  
Three New Species ◽  
First Time

Shield-backed katydids of tribe Arytropteridini Caudell, 1908 are recorded for the first time in Madagascar. The new genus Toliaridectes n. gen. is proposed to include three new species from the south west of the island: Toliaridectes meridionalis n. gen. n. sp., Toliaridectes wendenbaumi n. gen. n. sp. and Toliaridectes antsycurvis n. gen. n. sp.. Elements of biology of Toliaridectes n. gen. are given and the call of Toliaridectes antsycurvis n. gen. n. sp. is described. The taxonomic position of Arytropteridini is discussed.

scholarly journals II. On the lighting spectrum

1869 ◽  
Vol 17 ◽  
pp. 61-62 ◽  
Keyword(s):  
Continuous Spectrum ◽  
Peculiar Feature ◽  
The South ◽  
South West ◽  
Bright Flash ◽  
South West Monsoon ◽  
Variable Character ◽  
First Time ◽  
Similar Experience ◽  
West Monsoon

I have had two or three opportunities of seeing this spectrum to advantage of late. The storms at the period of the setting in of the south-west monsoon here are very frequent, and supply for a time almost incessant flashes, many of which are of course very brilliant. The first time I examined the light in the spectroscope I had no idea of measuring, but was content to realize the principal facts of a continuous spectrum crossed by bright lines; but subsequently I made several attempts (with some success) to obtain measures. That I was unable to do more in this line is due partly to the difficulty of utilizing the short-lived appearance, partly to that fascination of waiting for "one more” bright flash to verify the intersection, which can only be thoroughly appreciated by the aid of a similar experience. The principal features of the spectrum are a more or less bright continuous spectrum crossed by numerous bright lines, so numerous indeed as to perplex one as to their identity. This perplexity is increased by the constantly changing appearance due to a variable illuminating power. This variable character of the appearances is unquestionably the peculiar feature of the spectrum. It is not that the whole spectrum varies in brightness in the same degree, but that the relative intensities are variable, not only among the various lines, but between these and the continuous spectrum. The latter is sometimes very brilliant; and when that is the case, the red portion is very striking, though in general the spectrum seems to end abruptly at D + 0·34 (E = D + 1·38, Kirchhoff’s 120·7 = D + 0·55).

scholarly journals Cretaceous Orbitolinidae (Foraminifera) from Onshore and Offshore South-West England

1992 ◽  
Vol 11 (1) ◽  
pp. 21-30 ◽  
Author(s):  
M. D. Simmons ◽  
C. L. Williams
Keyword(s):  
The South ◽  
South West ◽  
Precise Identification ◽  
First Time ◽  
South West England

Abstract. The occurrence of orbitolinids in onshore and offshore South-West England is fully documented for the first time. Palorbitolina lenticularis is known from the Early Aptian — Late Barremian sediments of the offshore Fastnet Basin, and may also occur in the Aptian Farringdon Greensand. Late Albian Orbitolina sefini occurs in the Wolborough Limestone of Devon, whilst at Haldon, Devon, the orbitoline faunas are of Early Cenomanian age and referable to Orbitolina cf. concava. The orbitolinids from the Upper Greensand of the south-east Devon coast and the Fastnet Basin cannot be precisely identified, but belong to the Late Albian — Early Cenomanian O. sefini - O. concava plexus. Previous records of Orbitolina from the Upper Greensand at Wilmington are shown to be mistaken. These records are in fact referable to the sponge Porosphaera. The precise identification of some of the orbitolinids from South-West England supports the ages of the Wolborough Limestone and Haldon Sands suggested by Hamblin & Wood (1976). It is thought that orbitolinids migrated from Iberia to South-West England via the South-West Approaches during the Late Albian.

scholarly journals Ice-Shelf Flow at the Boundary of Crary Ice Rise, Antarctica

1988 ◽  
Vol 11 ◽  
pp. 8-13 ◽  
Author(s):  
R. A. Bindschadler ◽  
P. L. Vornberger ◽  
S .N. Stephenson ◽  
E. P. Roberts ◽  
S. Shabtaie ◽  
...  
Keyword(s):  
Surface Velocity ◽  
The South ◽  
Ice Shelf ◽  
West Side ◽  
North West ◽  
Ross Ice Shelf ◽  
South West ◽  
Lateral Tension ◽  
Free Block ◽  
First Time

Surface velocity and deformation, radar sounding, and aerial photography data are used to describe the flow of Ross Ice Shelf around Crary Ice Rise. A continuous band of crevasses around the ice rise now allows the complete boundary to be mapped for the first time. The dynamics of three distinctly different areas of ice flow are studied. Just up-stream of the ice rise, there is a region of ice rumples dominated by intense longitudinal compression (0.01 a−1) and lateral tension. On the south-west side of the ice rise, intense shear (0.03 a−1) dominates, with the boundary layer of affected ice-shelf motion extending over 20 km from the ice-rise edge into the ice shelf. North-west of the ice rise, a crevasse-free block of ice, 40 km × 7 km, appears to have separated from the main ice rise and is now moving with the ice shelf. We refer to such moving blocks of ice as rafts. The separation of this raft is calculated to have occurred 20 ± 10 years ago. Other possible rafts are identified, including one on the south-west side of the ice rise which appears to be in the process of separating. Mechanisms for the formation of rafts are discussed.

Close ny chollagh: an Iron Age fort at Scarlett, Isle of Man

1958 ◽  
Vol 24 ◽  
pp. 85-100 ◽  
Author(s):  
Peter S. Gelling ◽  
W. Potts
Keyword(s):  
Iron Age ◽  
Present Report ◽  
Viking Age ◽  
Southern Coast ◽  
The South ◽  
Isle Of Man ◽  
South West ◽  
History Of ◽  
First Time

Close ny chollagh lies on the southern coast of the Isle of Man (fig. 1), about one mile south-west of Castletown, and is one of the group of Manx fortified coastal sites. It is not on a promontory, having land adjacent to it on two of its four sides, but the deep gully to the south combines with an artificial ditch along the rest of the landward side to make it a position of some strength.When it was chosen for excavation in 1953 it was thought that the Manx promontory forts belonged to the Viking Age, and Close ny chollagh did indeed have a mediaeval level in which the principal building was a long-house of Scandinavian type. There was also, however, an Iron Age level, separated by a sterile layer from the later one, clearly demonstrating for the first time an Iron Age origin for one of the Manx promontory forts. It is to this Iron Age phase in the history of the fort that the present report is devoted.

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