scholarly journals V.—Contributions to Ceylon Geology: Occurrence of Corundum In Sitû Near Kandy, Ceylon

1903 ◽  
Vol 10 (8) ◽  
pp. 348-350 ◽  
Author(s):  
A. K Coomáraswámy

The present notes are based on field observations made in 1900. The section described is now obscured.Corundum is abundant in the gem-bearing gravels of Ceylon, but with the exception of the case here described no localities are known where it occurs in sitû; the present occurrence is therefore of considerable interest, although not very satisfactory in itself.Crystals of corundum were found in the surface soil on a piece of land known as Tenna Hena, and situated east of Kandy, and three-quarters of a mile north-east of Talatnoya bridge. The exact spot is shown in a map accompanying a paper on the crystalline limestones of Ceylon (Quart. Journ. Geol. Soc, 1903, vol. lviii, pl. xiii). A small excavation had been made, and a few pounds of corundum extracted and sold for use as emery, before my visit to the spot. All the rock exposed was decomposed, and crumbled in the fingers, being in a condition resembling sand. I therefore carried on an excavation for two months, hoping to reach hard rock suitable for microscopic examination, but although a depth of about 30 feet was reached, no sufficiently hard rock was found.At the corundum pit the ‘beds’ of granulite dip northwards at a high angle. A conspicuous soft yellow micaceous band 7–3½ inches wide marks the position of the sapphire-bearing zone. The sapphires occur in fair abundance in a less decomposed felspathic rock occupying a few inches on either side of this yellow micaceous band in the upper part of the shaft, but on the south side only in the lower part. The associated types of granulite are chiefly acid leptynite.

1954 ◽  
Vol 49 ◽  
pp. 244-247
Author(s):  
A. J. B. Wace ◽  
F. H. Stubbings

In 1950 and 1952, in view of recent discussions about the date of the Grave Circle, we decided to make some fresh soundings in its supporting wall to see if any fresh evidence could be obtained. In the first year the work was confined to soundings in the battered supporting wall on the south side opposite the north-east corner of the House of the Warrior Vase, and was undertaken by Mr. Kenneth Rowe. In 1952 further soundings were made in the battered supporting wall, the wall at its base on the west was further examined, and a sectional cut was made across the double ring of standing slabs on the north-east side about midway between the entrance and the then surviving cover slabs. The work was then directed by Dr. F. H. Stubbings.At the time of Schliemann's excavations the western part of the double ring of vertical poros slabs of the Grave Circle, which rests on the battered supporting wall, was in a very ruinous condition. This can be seen clearly in Schliemann's illustration and in the photographs published later. After the close of Schliemann's and Stamatakes' excavations the supporting wall was restored both on the west and on the south, and the western half of the double ring of standing slabs was reconstructed. When Keramopoullos excavated the fallen rock in the centre of the circle the Greek Archaeological Service undertook some further work of conservation.


1945 ◽  
Vol 82 (6) ◽  
pp. 267-273 ◽  
Author(s):  
W. Anderson

Formerly there were several surface brine springs in the North-East Coalfield; to-day there are none. From the many accounts of their occurrence nothing has been learned of their exact position, and very little of the composition of their waters. The earliest record, made in 1684, described the Butterby spring (Todd, 1684), and then at various times during the next two centuries brine springs at Framwellgate, Lumley, Birtley, Walker, Wallsend, Hebburn, and Jarrow were noted. In particular the Birtley salt spring is often mentioned, and on the 6-in. Ordnance map, Durham No. 13, 1862 edition, it is sited to the south-east of the village. Although no record has been found there must have been either a brine spring or well at Gateshead, for the name of the present-day suburb, Saltwell, is very old, and brine springs are still active in the coal workings of that area.


Antiquity ◽  
1964 ◽  
Vol 38 (149) ◽  
pp. 38-44 ◽  
Author(s):  
F. Zorzi

The first objective in this area was the Grotta Paglicci (FIG. I), a cave opening into the cretaceous limestone on the south side of the great karstic plateau, just below the village of Rignano. Here, in 1957, three of the author's colleagues, Professors A. Pasa and S. Ruffo, and Sig. Messena collected bone and stone artifacts of Palaeolithic date from the tip of a vast excavation which a mad treasure hunter had been carrying out in the cave for several years. When I visited the site in 1960 to make the preparations for a proper excavation, I discovered to my dismay that in the meantime this same treasure hunter, in spite of dissuasion, had been continuing his devastation with the help of explosives and had caused the fmal collapse of the entrance to the cave, completely obscuring its natural morphology. With meagre hopes of finding any part of the deposit intact, a start was made in the following April 1961 patiently to clear the mouth of the cave to see what could be saved. Fortunately an area of undisturbed deposit was found sealed below some large blocks of the fallen roof and furthermore a passage was cleared through the treasure hunter's debris towards the interior of the cave.


Archaeologia ◽  
1903 ◽  
Vol 58 (2) ◽  
pp. 359-382
Author(s):  
E. Towry Whyte

About a mile and a half south from Penrith on the main road from Carlisle to York and on the Westmorland side of the river Eamont, which is the boundary between the two counties, stand the ruins of Brougham Castle, one of the most important strongholds of the great Clifford family, who owned no less than four castles in the county, namely, Brougham, Appleby, Brough (under Stanmore), and Pendragon, and also Skipton in Craven, Yorkshire. From comparatively early times the site of this castle has been a place of some importance, as the Romans had here a strong camp, the remains of which are still to be seen in the field to the south of the present building. The name of this camp was Brovacum, but it has been spelt in various ways. It was a rectangular parallelogram surrounded by a single ditch about 75 feet broad with rounded corners, and had a rampart on the inside. There has also been a berm or terrace between this rampart and the ditch below the main defensive works, which were of timber. No trace of the entries to the camp now remain. The ditch on the south side is still complete, and portions on the east and west. Mr. Gr. T. Clark, in a paper in the Proceedings of the Cumberland and Westmorland Archæological Society gives the area within the ditch as 113 yards by 134 yards at the present time, but says it was most likely 198 yards originally, as that was the proportion of the Brough camp. The reason for placing this camp where it is was to guard the ford across the river Eamont where the road from York to Carlisle crossed that river. This ford I think was a little further down the stream than the present bridge, at a point where it is very shallow in summer, but during the winter and spring it must have been often dangerous and at times impassable. Of course the bed of the river may have been quite different in Roman times, but probably its course was much the same as at present. If I am right as to the site of the ford, the Roman road was continued in a straight line from about the Countess's Pillar to the brow of the hill above the river, down which it went at a sharp angle to the water, and then straight across the marshy field until it meets the road as traced by the ordnance surveyors. The camp stands on the south side of the river about 30 feet above it on flat land; and if Mr. Clark's suggestion as to the original size be correct its north-east corner was about 50 yards distant from it. On the opposite side for some considerable distance must have been marsh land, probably often flooded, whilst still further north rose the conspicuous hill now known as Penrith Beacon, under the southern flank of which the Roman road ran in an almost straight line to the next important camp, Voreda, near the village of Plumpton, about five miles north-north-west of Penrith. The camp was also, in all probability, approached by another road, which ran past the present Brougham Hall and across the river Lowther near the bridge and on to Yanwath, where it joined the road that goes over High Street, Avhich in places attained an elevation of 2,200 feet. A third road I think led to the camp from the south, going over Crosby Ravensworth Fell and so on to Lancaster. The main road all the way from Brough Castle to Carlisle is a most wonderful piece of engineering, when the probable condition of the country when the Romans made it is considered. Its gradients are seldom excessively steep, and yet it keeps an almost straight line for miles; and this was surveyed and made at a time when the whole country was a dense forest and the surrounding hills inhabited by a warlike and hostile race. It is rather surprising, considering the military importance of Brovacum, that it has not yielded more important monuments than it seems to have done. Stukeley mentions that he saw many fragments of altars and inscriptions at the Hall (Brougham Hall), and in the wall by the Roman road beyond the castle and near the Countess's Pillar a pretty “buste,” part of a funeral monument, and further on another bas-relievo much defaced, so that in his time perhaps there were some monuments which are now lost; but Chancellor Ferguson in his History of Westmorland says it “has not yielded many inscribed stones, and those not of any great importance. A couple of altars to the local deity Belatucador and four or five fragments of tombstones.” A portion of an inscription remains on a slab in the ceiling of a doorway passage leading to the second floor of the keep; the only word I could read for certain was Titus.


2020 ◽  
Author(s):  
Hugo Moors ◽  
Miroslav Honty ◽  
Carla Smolders ◽  
Ann Provoost ◽  
Mieke De Craen ◽  
...  

<p>The geological extreme Dallol region, located around the Dallol volcano in the north-east of Danakil depression (Ethiopia), is considered as one of the harshest and hottest places on Earth. The geology is made up of years and years of evaporates accumulation. Volcanic activity generates ascending brines that may cross and mix with aquifers from inflowing meteoric water originating from the Ethiopian highlands on the east of the Danakil depression. When these mixtures reach the surface they can generate hydrothermal springs giving rise to waterbodies in the form of small ponds or lakes. During the Europlanet 2018 Danakil field expedition, ten of these saline waterbodies were extensively studied by <em>in situ</em> measurements and <em>ex situ</em> geo–physico-chemical and –microbiological analyses of collected samples, liquids as well as sediments.</p><p>The <em>in situ</em> physico-chemical measurements clearly indicated the extreme nature of all ten investigated lakes. Laboratory analyses of the collected batch samples of liquids and sediments confirmed the extreme character of the waterbodies and complements our geological survey of the region with valuable geo–chemical and –microbiological data.</p><p>Based on our analytical results, the relative small Dallol region can still be subdivided into three geological smaller areas: the outcrop zone, the volcanic base region and the distant south area. The outcrop zone is dominated by sodium, iron and potassium. Oxidation processes in the outflowing superheated ferrous and sulfidic rich brine give rise to some of the most acidic ponds on our planet. In the ponds and lakes of the volcanic base region, incredible high amounts of calcium and/or magnesium can remain in their dissolved form as the most dominant and quasi only available anion is chloride. This region is host for the most saline water body on Earth. Chemical analysis of the lakes of the distant south area show that sodium is by far the most dominant cation. It is therefore no surprise that the large Karum Lake in the south region is economically exploited for the mining of sodium chloride.</p><p>Our mineralogy analyses render results that are completely in line with the observed geochemistry of the waterbodies. Halite and sylvite are the most present minerals in the Dallol outcrop zone associated with some gypsum and in one case with anhydrite. The geology around the waterbodies of volcanic base zone are a little bit more divers. On the shores of the Gaet’ale Pond tachyhydrite, chloromagnesite, halite and sylvite is determined, while the Black Lake is surrounded by bischofite and carnalite. Logically, the mineralogy of the south area, the salt mining area, is dominated by halite and sylvite.</p><p>Apparently, the geochemistry of the outcrop zone and volcanic base region is so harsh that no extremophilic organism is able to survive in these areas. Only in the distant south area did we find indications of the presence of halophiles. Besides the bacterial genus <em>Salinibacter</em>, our 16S rDNA microbiological fingerprinting indicates the presence of halophilic archaea like:  <em>Halobaculum sp., Halobellus sp., Halomicroarcula sp., Halorientalis sp.</em> with the majority of the population being <em>Candidatus Nanosalina sp</em>.</p>


1924 ◽  
Vol 4 (2) ◽  
pp. 182-193 ◽  
Author(s):  
A. Leslie Armstrong

The excavations described in the Preliminary Report were, through the generosity of the Trustees of the Percy Sladen Memorial Fund, and with the co-operation of Dr. R. V. Favell, resumed in 1924 and further efforts made to discover evidence of the earliest mining activities at Grimes' Graves. Summarised briefly the work of 1923 had already established the following facts:—(1) The existence on the southern slope of the valley, north of the Graves, of primitive flint mines roughly circular in shape and sunk to the Floor-stone, at that point 12 feet 6 inches deep.(2) That the two pits examined were devoid of galleries, the shafts being belled out at the base to obtain as much flint as possible.(3) That Hand Picks of a form not hitherto recognised and formed of the long bones of animals, had been used for excavation purposes assisted by wedges and choppers of flint.(4) That Deer-antler picks, or fragments of deer antler were entirely absent.(5) That access had been gained to the pits by rude staircases cut in the shaft walls.(6) The nature of the valley deposits was established by a series of sections and the almost complete erosion there of the Floor-stone, by glacial agencies, proved.(7) The limits within which Floor-stone exists in situ on the south side of the valley was defined and an outcrop of contorted Floor-stone discovered.


2020 ◽  
Vol 23 (3-4) ◽  
Author(s):  
Jasper VERHAEGEN ◽  
Lander FREDERICKX ◽  
Marco SCHILTZ

Previous studies have shown that the Kasterlee Formation occurs as far south as the hilltops of Heist-op-den-Berg and Beerzel in the south of the province of Antwerp. In fragmentary outcrops on these hills, a clear threefold subdivision can be recognized. In the current study, a large temporary outcrop on the Heist-op-den-Berg hill was studied, providing a unique view into the small-scale vertical and lateral variations in the Kasterlee Formation. Based on field observations, grain size analyses and mineralogy, the characteristics of the three units could be clearly defined. Cone penetration test logs show that these units can also be traced further north in the basin. As the three units can be easily identified based on the parameters provided in this paper and as they occur over a wide area, it is proposed to introduce them as formal members of the clayey Kasterlee unit. The observations made in this outcrop also allowed to refine the paleogeographic model of the Kasterlee Formation, with deposition of sand-clay alternations in restricted lagoons, separated from the marine environment by a coastal barrier, during an overall regression. Coastal barrier deposits are found in the south and northwest, but in the northeast only deposition in restricted lagoons occurred.


1925 ◽  
Vol 45 (2) ◽  
pp. 210-228
Author(s):  
Arthur M. Woodward

This article attempts to summarise the results (1) of those excavations carried out in Greek lands in 1924 of which no report was available in time for my account printed in the last volume of the Journal, and (2) of the excavations of 1925 of which reports had come to hand before the end of September. This system will be followed in the accounts which I hope to contribute annually henceforward.American SchoolThe varied activities of the American School included excavations at the sites of Corinth, the Argive Heraeum, and Eutresis in Boeotia. At Nemea and Phlius, the opening campaigns at which sites were described in my report of a year ago, no further work was done in the summer of 1925. At Corinth, thanks to a generous subsidy by, and the personal enterprise of, Professor T. L. Shear, substantial progress was made with the Herculean task of clearing the theatre, where, on the south side of the orchestra, the depth of the deposit of earth proved to be 12 metres; before the season closed, over 5000 tons of debris had been removed to a dump a quarter of a mile away. In the west of the cavea the seats proved to be all destroyed, but a remarkable discovery was made, in the form of a wall, originally ca. 2·80 metres high, surrounding the orchestra. This where cleared was preserved to a height of 1·70 m., and was painted in fresco with scenes of life-sized figures engaged in combat with lions. One combatant, in action with a lion which charges him from the left, is clad in a long purple under-garment, with a white over-garment fastened at the knee; another wears a short garment which hangs down in front, leaving the legs bare to the hips, and white sandals; other figures, variously clad, and also fighting lions, appear in other scenes.


1925 ◽  
Vol 5 (3) ◽  
pp. 268-272
Author(s):  
Philip B. Chatwin

In the summer of 1923 several Anglo-Saxon graves were discovered at Emscote, on the right bank of the river Avon, one mile above Warwick, and fifty yards from the south side of the embankment of the Great Western Railway. The remains of five or six interments were found, the bones being very fragmentary and soft. They lay in a thick bed of gravel which has been gradually removed. As soon as Mr. Cleaver, the owner of the gravel-pit, realized that these were ancient interments and the objects probably of some interest, he reported the matter to the Mayor of Warwick (Dr. Hubert Tibbits), who communicated through our Secretary with Mr. John Humphreys, F.S.A., one of the Local Secretaries for Warwickshire. At the latter's request I kept in touch with the excavation work, but by that time all the important objects had been found; since then one more grave has been disturbed, in which only a spear-head was found with the bones. As the gravel-pit on this side is practically exhausted, it seems improbable that any further discoveries will be made in this direction.


2015 ◽  
Vol 16 (2) ◽  
pp. 889-903 ◽  
Author(s):  
Wesley J. Rondinelli ◽  
Brian K. Hornbuckle ◽  
Jason C. Patton ◽  
Michael H. Cosh ◽  
Victoria A. Walker ◽  
...  

Abstract Soil moisture affects the spatial variation of land–atmosphere interactions through its influence on the balance of latent and sensible heat fluxes. Wetter soils are more prone to flooding because a smaller fraction of rainfall can infiltrate into the soil. The Soil Moisture Ocean Salinity (SMOS) satellite carries a remote sensing instrument able to make estimates of near-surface soil moisture on a global scale. One way to validate satellite observations is by comparing them with observations made with sparse networks of in situ soil moisture sensors that match the extent of satellite footprints. The rate of soil drying after significant rainfall observed by SMOS is found to be higher than the rate observed by a U.S. Department of Agriculture (USDA) soil moisture network in the watershed of the South Fork Iowa River. This leads to the conclusion that SMOS and the network observe different layers of the soil: SMOS observes a layer of soil at the soil surface that is a few centimeters thick, while the network observes a deeper soil layer centered at the depth at which the in situ soil moisture sensors are buried. It is also found that SMOS near-surface soil moisture is drier than the South Fork network soil moisture, on average. The conclusion that SMOS and the network observe different layers of the soil, and therefore different soil moisture dynamics, cannot explain the dry bias. However, it can account for some of the root-mean-square error in the relationship. In addition, SMOS observations are noisier than the network observations.


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