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028W0390.TXT

ADMINISTRATIEVE & TECHNISCHE GEGEVENS
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Kaart nr.:		28W
PLAAT:		Antwerpen
Nr.:			390  (VIII, b)
Type Boring:	tijdelijke ontsluiting
Topografische kaart:	15/3
Uitgevoerd te:	Antwerpen – Zuidstation (VI A.R.)
Post nr.:		2000
Adres boorplaats:	E3 – kleine ring

Opdrachtgever:	
Boorfirma		 
Boordatum:		april 1966
Topografie:		
Stalen door:		
Boormethode:	
Lengte & doormeters: 	

Grondwaterstanden:	
1ste maal:		
Bij rust:		
Tijdens pompen:	
Debiet:		
Waterzaak nr.:	
Totale diepte:	6 m
Stalen bewaard:	
Maaiveld / ref. peil: 	1 m
X:			150680
Y:			210020
NIS code:	11002

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BOORBESCHRIJVING
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nr. * Basis * AARD DER GRONDLAGEN
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1	01.00m	Zand en dikke schelpenbank
2	06.00m	Zand met enkele kleilensjes en schelpjes
3	06.50m	klei
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BOORBESCHRIJVING uit PP 1976 nr 3
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AARD DER GRONDLAGEN
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"Quaternary":
yellow brown very coarse heterogenous sand with more or less massive layers of 
reworked shell and shell fragments; flint pebbles; in the A.R. section the 
shell layers with clay streaks and fossil wood. 

Edegem Sands:
Dark green fine clayey fossiliferous glauconitic sand, decalcified and more 
oxydated at the top; generally very rich in Mollusca, mostly dispersed in the 
sediment, rarely concentrated in nests (VI A.R. 7, A.R. 11) or thin layers (III 
A.R. 28-29), rare speciments of the guide fossil "Panopoea Menardi" (= panope 
angusta inflata GOLDFUSS, 1841) (VI A.R. 7 and 17, A.R. 5 and 14).
Burcht Gravel:
Fairly well developped gravel with dark small rounded flint pebbles, from the 
underlying clay reworked septaria, concentrated shell fragments and dark small 
shark teeth.

Boom Clay:
Dark green plastic silty clay
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STRATIGRAFISCHE INTERPRETATIE
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Top  * basis  * STRATIGRAFISCHE EENHEDEN
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00.00m – 01.00m	Kwartair
01.00m – 06.00m	Zand Van Edegem
06.00m – 06.50m	Boomse klei
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AUTEUR. 
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Referenties: Lithostratigraphy of Miocene sediments from temporary outcrops in 
the Antwerp city area, Professional Paper, 1976, nr3.
F. De Meuter, K. Wouters, A. Ringele


BELGISCHE GEOLOGISCHE DIENST

	028W/0390 (VIII, b)  KAARTBLAD: ANTWERPEN
p. 1/2
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