scholarly journals Discovery of the very large crater-facies kimberlite system of Tokapal, Bastar district, Chhattisgarh, India

2019 ◽  
Keyword(s):  
Large Crater

Large Crater Clustering tool

2017 ◽  
Vol 105 ◽  
pp. 81-90 ◽  
Author(s):  
Jason Laura ◽  
James A. Skinner ◽  
Marc A. Hunter
Keyword(s):  
Large Crater

The Large Crater Origin of SNC Meteorites

Science ◽  
1987 ◽  
Vol 237 (4816) ◽  
pp. 738-743 ◽  
Author(s):  
A. M. VICKERY ◽  
H. J. MELOSH
Keyword(s):  
Large Crater

scholarly journals The large crater on the small Asteroid (2867) Steins

Icarus ◽  
2010 ◽  
Vol 210 (2) ◽  
pp. 707-712 ◽  
Author(s):  
M.J. Burchell ◽  
J. Leliwa-Kopystynski
Keyword(s):  
Large Crater ◽  
Small Asteroid

An Attic Cistern Front at the British Museum

1928 ◽  
Vol 48 (1) ◽  
pp. 7-8
Author(s):  
W. R. Lethaby
Keyword(s):  
Original Work ◽  
Fourth Century ◽  
British Museum ◽  
Central Group ◽  
Large Crater ◽  
The Third ◽  
Water Trough ◽  
Herodes Atticus

In the Third Graeco-Roman Room is a long relief, numbered 2154 and entitled a Votive Relief. It is described in the catalogue (1904) as ‘Relief, perhaps votive, with Dionysos receiving a libation. The central group consists of Dionysos and a Maenad…. Behind the Maenad a large crater stands on the ground…. A moulding appears to have been tooled away above…. May be as early as the end of the fourth century. Athens: Elgin Collection. Height 2 feet 7 inches; length 5 feet 8 inches. Found among the ruins of the theatre of Herodes Atticus. Formerly in the possession of N. Logotheti. Stuart, ii, pp. 23, 45.…’Close to the ‘crater’ a hole about an inch in diameter has been carefully bored through the marble—so carefully that the presumption is that it is part of the original work, although it is suppressed in the old illustrations and is not mentioned in the descriptions. On looking behind the relief it at once appears that material at the two ends and the bottom has been cut away. The remnants of the parts which have been cut off suggest the two ends and bottom of a water trough or cistern. The hole mentioned above is situated an inch or so above what remains of the bottom, and thus conforms to the general tradition of stone water troughs such as several of granite which I have recently seen in Dartmoor farm-yards. From these evidences and the appropriate size it may not be doubted that the relief is the front of a water cistern.

Limits on large-crater production and obliteration on Callisto

1981 ◽  
Vol 8 (8) ◽  
pp. 891-894 ◽  
Author(s):  
Alex Woronow ◽  
Robert G. Strom
Keyword(s):  
Large Crater

Mineralogy of Marcia, the youngest large crater of Vesta: Character and distribution of pyroxenes and hydrated material

Icarus ◽  
2015 ◽  
Vol 248 ◽  
pp. 392-406 ◽  
Author(s):  
M.C. De Sanctis ◽  
A. Frigeri ◽  
E. Ammannito ◽  
F. Tosi ◽  
S. Marchi ◽  
...  
Keyword(s):  
Large Crater

scholarly journals Notes on some Late Cretaceous goniasterid starfish (Echinodermata, Asteroidea) from Belgium and Germany

2021 ◽  
Vol 73 (3) ◽  
pp. A030321
Author(s):  
John W. M. Jagt ◽  
Elena A. Jagt-Yazykova ◽  
Barry W. M. Van Bakel ◽  
René H. B. Fraaije
Keyword(s):  
New Species ◽  
Late Cretaceous ◽  
Type Species ◽  
Radial Line ◽  
Large Crater ◽  
Two New Species ◽  
Large Spine ◽  
Upper Maastrichtian ◽  
Upper Campanian

Both partially articulated specimens and dissociated marginal ossicles form the basis for erection of two new species of Late Cretaceous goniasterids from the Mons and Liège-Limburg basins (Belgium) and the Hannover area (Germany). Chomataster breizh sp. nov., which recalls the type species, Chomataster acules Spencer, 1913, but differs in several respects, is based on a partial external mould of the marginal frame of disc and arms in flint (upper Campanian Spiennes Chalk Formation; Mons Basin), as well as on a more or less complete individual, preserving small, spherical spines and granules and encased in a flint nodule from the upper Maastrichtian Nekum Member (Maastricht Formation; Liège-Limburg Basin). In Ch. breizh sp. nov., supero- and inferomarginals bear close-set granule pits, of varying sizes, as well as bivalved alveolar scars of pedicellariae; median superomarginals and all inferomarginals lack large, crater-shaped spine pits – such are found only in the disc/arm transition and along the arms. Dissociated supero- and inferomarginal ossicles from the lower and upper Campanian of the Hannover area and the upper Campanian of northeast Belgium, previously recorded either as indeterminate astropectinids or as Nymphaster obtusus (Forbes, 1848) var. nov. and as Nymphaster sp., respectively, here are assigned to Nymphaster mudzborgh sp. nov. This species is characterised by a row of 3–5 large spine pits on the aboral and lateral surfaces of superomarginals; inferomarginals have an angular profile and a close cover of granule pits. Nymphaster tethysiensis Villier, 2001, from the upper Campanian of Landes (southwest France; Villier and Odin, 2001) appears best accommodated in Chomataster as well, because in the arm superomarginals alternate rather than meet over the mid-radial line.

Giordano Bruno, the Moon's latest large crater

Nature ◽  
1976 ◽  
Vol 264 (5583) ◽  
pp. 212-213 ◽  
Author(s):  
David W. Hughes
Keyword(s):  
Large Crater ◽  
Giordano Bruno
Sign in / Sign up

Export Citation Format

Share Document