III.—Note on a Small Anticline in the Geeat Oolite Series at Clapham, North of Bedford

1904 ◽  
Vol 1 (9) ◽  
pp. 439-441 ◽  
Author(s):  
Horace B. Woodward
Keyword(s):  

In the broad Alluvial tract which borders the Ouse between Oakley and Clapham, north of Bedford, there is a gravel-pit in which a small anticline of the Great Oolite was abruptly encountered amidst the regularly stratified river-deposits. The pit is situated immediately north of the Oakley road and east of the Midland Railway.

Archaeologia ◽  
1890 ◽  
Vol 52 (2) ◽  
pp. 315-388 ◽  
Author(s):  
Arthur John Evans

In November, 1886, being at Aylesford in company with my father Dr. John Evans and with Dr. Sebastian Evans, we paid a visit to the sand and gravel pit belonging to Messrs. Silas Wagon and Son, our immediate object being to search for palaeolithic implements which had been discovered at this spot. Our attention was then called to another and highly interesting discovery that had just been made whilst removing the surface earth, which here to a depth of about three feet covers the old river deposits. This consisted of a bronze pail or situla (fig. 11), and a small fragment of another, an ænochoê (fig. 14), a long-handled pan or patella (fig. 16), and two fibulæ (figs. 17, 18), also of bronze, together with calcined bones and fragments of earthenware vases. On examination the situla proved to be a characteristic example of that peculiar style of art which had taken root in Britain during the century or so that preceded the Roman Conquest, and to which Mr. Franks has given the name of “Late-Celtic.” The ænochoê, or bronze vase, the pan and fibulæ were also of great interest as representing imported specimens of late Greek or Italian fabrics. The earthenware vases themselves exhibited an elegance of form and a style of manufacture such as had not yet been associated with British remains in this country, and which, as I hope to show, point not less distinctly to Gaulish and in a somewhat remoter degree to North Italian connexions.


2005 ◽  
Vol 28 (1-4) ◽  
pp. 283-295 ◽  
Author(s):  
I. Blanco García ◽  
M. Rodas ◽  
C.J. Sánchez ◽  
M. Dondi ◽  
J. Alonso-Azcárate

1988 ◽  
Vol 23 (3) ◽  
pp. 1719-1723
Author(s):  
M. P. Cook ◽  
M. J. Burgis
Keyword(s):  
Pit Lake ◽  

1870 ◽  
Vol 7 (75) ◽  
pp. 410-413 ◽  
Author(s):  
E. Ray Lankester

The forms which Mr. Davidson in his invaluable Monograph has included under T. ovoides, are so various that it would be possible to refer the shells figured in the plate to that species, but since T. trilineata, from the Inferior Oolite, and T. lata and T. ovoides, from drift-blocks—which I shall endeavour to show are of the very latest Jurassic horizon—are very different in many respects, I prefer to give a new name to this form, which may find its place near T. ovoides and T. simplex. The specimen drawn, Fig. 1 and la, is from the collection of Mr. Roper of Lowestoft, who obtained it, with another specimen, from a gravel-pit at Thorpe in Suffolk. It has the general simple form of T. ovoides, but is remarkable for its great size. The imperforate valve is flattened in the mesial line, whilst the perforate valve is deep and raised into a well-pronounced keel in the mesial line extending from the beak; the foramen is small. The specimen figured is longer than the other in Mr. Roper's collection, which has the shorter, squarer form of Fig. 2, resembling T. simplex. This fine Terebratula may be known as T. rex.


1940 ◽  
Vol 5 (4) ◽  
pp. 334-335
Author(s):  
Vladimar Alfred Vigfusson

In recent years, the attention of some archaeologists has been directed to the Canadian Northwest with the expectation of finding some evidence or indication of the early migrations of man on this continent. That man reached North America by Bering Strait from Asia, is generally accepted, but the theory that the migrations took place in late Pleistocene times and by way of an open corridor between the Keewatin ice and the Rockies, requires confirmation. It is significant that Folsom and Yuma points from Saskatchewan, described by E. B. Howard, were found mainly in areas bordering the ancient glacial Lake Regina.As a further contribution to this problem, it seems desirable to present a brief description of a carved stone relic found in gravel in central Saskatchewan about three years ago.The stone was found about seven miles southeast of the town of D'Arcy in a gravel pit located on Sec. 9, Tp. 28, Rge. 18, W. 3rd Meridian, on the north bank of a ravine running east into Bad Lake.


1927 ◽  
Vol 7 (4) ◽  
pp. 438-464 ◽  
Author(s):  
E. Thurlow Leeds

At the end of April of last year the Rev. Charles Overy drew my attention to the presence of broken animal bones, flints, and sherds of pottery in a gravel-pit on the south side of the road from Abingdon to Radley, about a mile out of Abingdon (fig. 1).The pit lies on the very boundary of the parish of Abingdon in a field at about 200 ft. O.D., just over half a mile north of the Thames and some 30 ft. above the river. On its eastern and southern sides it is bounded by the wide trenches which in the days of the splendour of Abingdon Abbey formed part of the Abbey's fish-ponds ; on the north is the road, and on the east the ground drops to a little brook.


Water ◽  
2016 ◽  
Vol 8 (9) ◽  
pp. 409 ◽  
Author(s):  
Pauline Mollema ◽  
Marco Antonellini ◽  
Alwin Hubeek ◽  
Peter Van Diepenbeek

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