scholarly journals XI. An Account of Observations, made by Lord Webb Seymour and Professor Playfair, upon some Geological Appearances in Glen Tilt, and the adjacent Country

1815 ◽  
Vol 7 (2) ◽  
pp. 303-375 ◽  
Author(s):  
Webb Seymour

1. The river Tilt is a principal branch of the Tay, which rises on the borders of Aberdeenshire, and runs towards the south-west, through the north-eastern part of the county of Perth. A portion of the valley along its course, for about ten miles above Blair of Atholl, is called Glen Tilt.The adjacent country presents the common character of the Highlands. It is mountainous and rugged, and the surface, except in the lower parts of the valleys, is chiefly covered with heath. Peat-moss frequently occurs.

Starinar ◽  
2013 ◽  
pp. 269-286
Author(s):  
Perica Spehar ◽  
Natasa Miladinovic-Radmilovic ◽  
Sonja Stamenkovic

In 2012, in the village Davidovac situated in south Serbia, 9.5 km south-west from Vranje, archaeological investigations were conducted on the site Crkviste. The remains of the smaller bronze-age settlement were discovered, above which a late antique horizon was later formed. Apart from modest remains of a bronze-age house and pits, a late antique necropolis was also excavated, of which two vaulted tombs and nine graves were inspected during this campaign. During the excavation of the northern sector of the site Davidovac-Crkviste the north-eastern periphery of the necropolis is detected. Graves 1-3, 5 and 6 are situated on the north?eastern borderline of necropolis, while the position of the tombs and the remaining four graves (4, 7-9) in their vicinity point that the necropolis was further spreading to the west and to the south?west, occupying the mount on which the church of St. George and modern graveyard are situated nowadays. All graves are oriented in the direction SW-NE, with the deviance between 3? and 17?, in four cases toward the south and in seven cases toward the north, while the largest part of those deviations is between 3? and 8?. Few small finds from the layer above the graves can in some way enable the determination of their dating. Those are two roman coins, one from the reign of emperor Valens (364-378), as well as the fibula of the type Viminacium-Novae which is chronologically tied to a longer period from the middle of the 5th to the middle of the 6th century, although there are some geographically close analogies dated to the end of the 4th or the beginning of the 5th century. Analogies for the tombs from Davidovac can be found on numerous sites, like in Sirmium as well as in Macvanska Mitrovica, where they are dated to the 4th-5th century. Similar situation was detected in Viminacium, former capital of the roman province of Upper Moesia. In ancient Naissus, on the site of Jagodin Mala, simple rectangular tombs were distributed in rows, while the complex painted tombs with Christian motifs were also found and dated by the coins to the period from the 4th to the 6th century. Also, in Kolovrat near Prijepolje simple vaulted tombs with walled dromos were excavated. During the excavations on the nearby site Davidovac-Gradiste, 39 graves of type Mala Kopasnica-Sase dated to the 2nd-3rd century were found, as well as 67 cist graves, which were dated by the coins of Constantius II, jewellery and buckles to the second half of the 4th or the first half of the 5th century. Based on all above mentioned it can be concluded that during the period from the 2nd to the 6th century in this area existed a roman and late antique settlement and several necropolises, formed along an important ancient road Via militaris, traced at the length of over 130 m in the direction NE-SW. Data gained with the anthropological analyses of 10 skeletons from the site Davidovac-Crkviste don't give enough information for a conclusion about the paleo-demographical structure of the population that lived here during late antiquity. Important results about the paleo-pathological changes, which do not occur often on archaeological sites, as well as the clearer picture about this population in total, will be acquired after the osteological material from the site Davidovac-Gradiste is statistically analysed.


1876 ◽  
Vol 3 (4) ◽  
pp. 145-150 ◽  
Author(s):  
G. Linnarsson

In a paper on “The Physical Conditions under which the Cambrian and Lower Silurian Rocks were probably deposited over the European Area,” Mr. Hicks has recently put forth some opinions on the lowest fossiliferous rocks of Scandinavia and Russia, and their relations, as to age and stratigraphical characters, to those of Britain, which I think ought to be somewhat modified. The chief assertions in Mr. Hicks's paper are, that at the Pre-Cambrian period a large continent existed in Europe; that a subsidence began in the south-western part, and gradually extended to the north-eastern, which was not submerged until the Tremadoc group had been deposited over the western areas; and, finally, that the marine faunas migrated from the south-west. In order to prove these generalizations, Mr. Hicks makes a comparison between the most important Cambrian districts of Europe. He thinks that the British Cambrian rocks are the oldest, that the lowest Swedish beds are probably equivalent to the British Menevian group, and that the Russian are not older than the Arenig. Though the scantiness of the organic remains in some instances makes it very difficult, or, indeed, impossible to parallelize with certainty the oldest deposits of the various countries, it seems, however, from the palæontological facts already known, quite unquestionable that the lowest rocks of Scandinavia and Russia are older than Mr. Hicks has supposed them to be in comparison to those of Britain.


1937 ◽  
Vol 74 (7) ◽  
pp. 309-316 ◽  
Author(s):  
Inkermann Rogers ◽  
Brian Simpson

The deposit to be described is situated at Orleigh Court, in the parish of Buckland Brewer, some four miles west of south from Bideford, where it rests unconformably on the steeply dipping Upper Culm sandstones. Its greatest extent is from Orleigh Mill to Yeo Bridge, a distance of about three-quarters of a mile in a northwest to south-east direction, and from this line it extends to the south-west for an average distance of about one-third of a mile, only exceeding that amount to the south of the Higher Lodge. The only extensive section was seen in the Rookery, where 25 feet of material rest on a yellow clay. The highest point reached by the deposit, to the south-west of the Higher Lodge, is about 400 feet above O.D. From this point it slopes to the north-east, extending down to about the 100 ft. contour on the left bank of the River Yeo. It is possible that the north-eastern boundary does not reach such low levels as those indicated on the map, Text-fig. 1, for it is difficult to distinguish the original gravel from relatively recent hill wash; and, without a good deal of trenching or augering, it would not be possible to determine the boundary more closely than has been done in the present work.


2021 ◽  
Vol 26 ◽  
pp. 253-283
Author(s):  
Piotr Gotowko

The geographical and familial origins of the Teutonic Order’s officials Konrad von Kyburg and Rudolf von Kyburg   The researchers of the Teutonic Order have placed the brethren Konrad (before 1336 – 12. April 1402) and Rudolf (before 1337–1404) von Kyburg in the north-eastern part of present-day Switzerland – either in the castle of Kyburg near Winterthur in the eastern Canton of Zurich, or in the Canton of Turgovia, lying in the East of Canton Zurich and to the South of Lake Bodensee. Their family lost those areas by 1265, after a sudden death of Hartmann V von Kyburg (1263) and the childless death of his uncle, Hartmann IV (1264). The only successor, the minor daughter of Hartmann V, Anna von Kyburg, was not able to keep her inheritance, which was quickly taken by her nephew Rudolf IV von Habsburg, latter known as German King Rudolf I. He arranged a marriage between Anna and his relative, Eberhard von Habsburg-Laufenburg, leaving them only Burgdorf and Thun in the nowadays Canton Berne. Their son, Hartmann, had taken the name of the maternal dynasty, calling himself since 1297 Hartmann I von Kyburg. His son, Eberhard II  von Kyburg, succeeded him. He was the father of eleven children with Konrad von Kyburg and Rudolf von Kyburg among them. Despite their name, they came from Burgdorf and had joined the Teutonic Order because the poor parents could not guarantee them a subsistence. The carreer of Konrad von Kyburg started in the late 1380s. In 1392 he was promoted to the Comtur of Balga and from 1396–1402 had even reached the high rank of the Great Hospitaller. The carrier of his younger brother, Rudolf, was less impressive for he became 1391–1402 the Comtur of Rehden.


GEODYNAMICS ◽  
2011 ◽  
pp. 28-36
Author(s):  
G.P. Yarotskiy ◽  

Earthquakes on the south-west of Koryak highlands are connected with a block-key tectonics of lithosphere of marine transital of north-eastern margin of Eurasia and the block-key structure of its strata. The cloud of shocks of three strong earthquakes: Koryak`s (13.10.1988), Khailin`s (8.03.1991) and Olutor`s (20.04.2006) is located over the downfold of lithosphere bottom with drop of depths equal to 15-20 km. Preparation for the seismic events evolution to the north-eastward is possible.


1887 ◽  
Vol 4 (12) ◽  
pp. 546-552 ◽  
Author(s):  
Alfred Harker

In the northern half of Anglesey occur several intrusions of dark hornblendic rocks, some specimens of which were placed by Henslow in the collection made by him for the Woodwardian Museum. These rocks present a type unusual in Britain, and show some peculiarities which are of considerable interest.A few years ago Professor Bonney found on the south-west coast of the island some boulders of a rock which he described under the name of Hornblende-picrite. It was subsequently pointed out by Professor Hughes that the probable source of these rocks was to be found in certain intrusive masses near Llanerchymedd, and indeed such boulders are scattered about rather abundantly in that neighbourhood and to the south-west. The rock in question seems, however, to be the common type of the larger eruptive masses in the north of Anglesey, and brief notes on slides cut from selected specimens taken in place may be found not unprofitable. The rocks were noticed and megascopically described in Henslow's Memoir.


2016 ◽  
Vol 21 (1) ◽  
pp. 69-90
Author(s):  
Oleksandr Shelekhan ◽  
Oksana Lifantii ◽  
Yuriy Boltryk ◽  
Marcin Ignaczak

Abstract The article focuses on the research results of Severynivka hillfort fortifications. In 2009 a rampart and a moat on a cliff on the south floor-level side. In 2012-2013 there was made a rampart and escarp sections in the north-eastern part of the fortification. Separate stages of its construction are distinguished; the possible reconstruction of the defensive structures is suggested.


1862 ◽  
Vol 152 ◽  
pp. 1019-1038 ◽  

The little town or village of Bovey Tracey, in Devonshire, nestles at the foot of Dartmoor, very near its north-eastern extremity; it is situated on the left bank of the river Bovey, about two miles and a half above the point at which it falls into the Teign, and is about eleven miles from each of the towns Exeter, Torquay, and Totnes*,—bearing south-westerly from the first, north-westerly from the second, and northerly from the last. A considerable plain stretches away from it in a south-easterly direction, having a length of six miles from a point about a mile west of Bovey to another nearly as far east of Newton; its greatest breadth, from Chudleigh Bridge on the north-east to Blackpool on the south-west, is four miles. It forms a lake-like expansion of the valleys of the Teign and Bovey rivers, especially the latter, whose course it may be said to follow in the higher part, where it is most fully developed; whilst the Teign constitutes its axis below the junction of the two streams. Its upper, or north-western portion, immediately adjacent to the village, is known as “Bovey Heathfield,” and measures about 700 acres.


Diacronia ◽  
2016 ◽  
Author(s):  
Adina Dragomirescu ◽  
Alexandru Nicolae

This paper deals with two verbal forms which, despite being traditionally labelled as “non-finite”, display inflection/agreement. We will focus on the behaviour and origin of the inflected infinitive attested in Romance and in languages from other families, against which we analyse the novel inflected supine found in the north-eastern area where Romanian is spoken (comprising the Republic of Moldova, Ukraine and the north-eastern part of the Romanian province of Moldova). The goal of the paper is to identify the common paths of diachronic change of these verbal forms and to put forward a formal account of the observed diachronic changes. From a diachronic perspective, our analysis shows that the functional structure of non-finite forms may become more enriched, a conclusion that is at odds with traditional findings, which generally argue for simplification, not enrichment of functional structure. At the same time, the proposed analysis also offers some insights into the diachrony of the supine marker de.


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