‘Catch a falling star’: the Winchcombe meteorite fall of 2021

Geology Today ◽  
2021 ◽  
Vol 37 (6) ◽  
pp. 237-240
Author(s):  
Michael J. Simms
Keyword(s):  
Nature ◽  
1958 ◽  
Vol 181 (4623) ◽  
pp. 1613-1614 ◽  
Author(s):  
E. L. FIREMAN
Keyword(s):  

2011 ◽  
Vol 11 (1) ◽  
pp. 37-42 ◽  
Author(s):  
R. Fantucci ◽  
Mario Di Martino ◽  
Romano Serra

AbstractThis research deals with the fall of the Sikhote-Alin iron meteorite on the morning of 12 February 1947, at about 00:38 h Utrecht, in a remote area in the territory of Primorsky Krai in Eastern Siberia (46°09′36″N, 134°39′22″E). The area engulfed by the meteoritic fall was around 48 km2, with an elliptic form and thousands of craters. Around the large craters the trees were torn out by the roots and laid radially to the craters at a distance of 10–20 m; the more distant trees had broken tops. This research investigated through dendrocronology n.6 Scots pine trees (Pinus Sibirica) close to one of the main impact craters. The analysis of growth anomalies has shown a sudden decrease since 1947 for 4–8 years after the meteoritic impact. Tree growth stress, detected in 1947, was analysed in detail through wood microsection that confirmed the winter season (rest vegetative period) of the event. The growth stress is mainly due to the lost crown (needle lost) and it did not seem to be caused due to direct damages on trunk and branches (missing of resin ducts).


Geologos ◽  
2016 ◽  
Vol 22 (3) ◽  
pp. 251-258 ◽  
Author(s):  
Stanisław Fedorowicz ◽  
Wojciech T. J. Stankowski

Abstract The date of fall of the Morasko iron meteorite was determined by means of thermoluminescence measurements of the fusion crust and related local materials. Three small pieces, commonly referred to as ‘shrapnel’, were used. The results obtained are 4.5-5.0 ka, which is in good agreement with previous estimates of 4-6 ka on the basis of radiometric, do-simetric and palynological methods.


2021 ◽  
Author(s):  
Denis Vida ◽  
Damir Šegon ◽  
Marko Šegon ◽  
Jure Atanackov ◽  
Bojan Ambrožič ◽  
...  

2003 ◽  
Vol 38 (7) ◽  
pp. 1005-1021 ◽  
Author(s):  
J. BOROVIĈKA ◽  
H. W. WEBER ◽  
T. JOPEK ◽  
P. JAKEŜ ◽  
Z. RANDA ◽  
...  
Keyword(s):  

2004 ◽  
Vol 39 (S8) ◽  
pp. A163-A169 ◽  
Author(s):  
N. Laridhi Ouazaa ◽  
N. Perchiazzi ◽  
M. D'Orazio ◽  
P. Rochette ◽  
R. Clocchiatti ◽  
...  
Keyword(s):  

1998 ◽  
Vol 33 (S4) ◽  
pp. A177-A179 ◽  
Author(s):  
Yongheng CHEN ◽  
Daode WANG ◽  
Ruitian WANG
Keyword(s):  

2014 ◽  
Vol 49 (11) ◽  
pp. 1989-1996 ◽  
Author(s):  
Marc Fries ◽  
Lucille Le Corre ◽  
Mike Hankey ◽  
Jeff Fries ◽  
Robert Matson ◽  
...  

2012 ◽  
Vol 10 (H16) ◽  
pp. 167-167
Author(s):  
Hitoshi Yamaoka
Keyword(s):  

Though there are many forklore concerning meteorite falls, a few genuine meteorites have been identified. One of them, the Nogata meteorite is related to the oldest recorded meteorite fall (A.D. 861) (Shima et al., 1983).


1970 ◽  
Vol 37 (292) ◽  
pp. 880-887 ◽  
Author(s):  
G. J. H. McCall ◽  
P. M. Jeffery

SummaryThe fall of a shower of meteorites numbering several hundred fragments at Wiluna, Western Australia, on the night of 2 September 1967, has been investigated. Although the dispersion ellipse had been largely obscured by removal of fragments before a party of scientists were able to make a field investigation, it has, nevertheless, been possible to make a reasonable estimate of the shower distribution pattern. In spite of this removal of fragments, a number of pieces of meteorite were still found in situ. The bulk of the total recovery is in the collections of the Western Australian Museum, and the physical characteristics of these masses and their petrography is described. In all, some 490 individual fusion-crust coated stones and a large number of broken stony fragments are known to have been recovered. The meteorite is an olivine bronzite chondrite remarkably rich in discrete nodules of nickel iron, up to an inch across, commonly aggregated with troilite. A full chemical analysis of this fresh meteoritic material has been supplied by the British Museum (Natural History).


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