From Wikipedia, the free encyclopedia

Geologic roots of artifacts and geologic influences on them

Geoarchaeologists are i.a. concerned with the geological facts that affect the ontstaan and the waardevermindering - affevtés of artifacts.

Archaeological geology (term coined by Werner Kasig 1980), a sub-field of geology, rather emphasises te value of earth constituents for human life.

_________

Archaeological geology

Archaeological geology (term coined by Werner Kasig 1980), is a sub-field of geology which emphasises te value of earth constituents for human life.

________

Some graves are marked by impressive monuments but the majority of grave markers are ordinary. These markers show the creativity of craftsmen stonecutters. The study of markers is an application of Archaeological geology.

This article concerns mainly the North East of the European continent, with some extension to Guilds of stonecutters.

File:Noorb 003 004 018 017 p3 27.jpg

The North East of the continent Information

Digging stone stimulated headstone traditions in the North East of the continent : a Boulonnais tradition, a Tournay- Ecaussines tradition, a Namur- Vesdre- Aachen tradition, a Wadden tradition, a Nievelstein tradition, a schiste tradition, a Liedberg tradition, a Siebengebirge tradition, a Mendig basalt tradition, a Lorraine tradition.

Geological base

Soil resources influenced constructing of buildings, as well as the creation of autonomous stone objects. And soil resources are linked to the relief.

In the North East of the European continent, a plain (several "B" 's on the map) is interrupted by a hill system ("M"+"Z"), which was uplifted during the Alpine orogeny: the rising of the Ardennes .

The geology of the "nose","M"+“Z”, can best be understood by means of the profile below, which corresponds to the vertical line "a" - "b" on the map.

The sand, the clay and the somewhat harder rocks of the “B"'s were used in constructing buildings and, to a modest extent, for small monuments.

"M" consists mainly of relatively hard rocks. Those were used for building blocks ( French: moellons, German : Bruchstein) and for small monuments.In the Neighborhood of Cologne ( German Köln) and of Koblenz, vulcanic activity during yy , provided respectivily the yy and the Basalt yy, which gave an yy to ther surroundings and sometimes wide in the ...

In the transient hem "Z", in German “Subvaristischer Saum”, the limestones and sandstones present themself as alternating waves. Those were beloved material for the building and have been appreciated for small autonomous, mostly monolithic monuments, such as headstones.

To the hem "Z" belons also the Ferques inlier ( French: "Boutonnière") in the Boulonnais, south of Calais, only some 60 km2 in surface, with layers from the Middle- Devonian (-385 Ma.) up to the Upper Visean (-325 Ma.). Those layers provided material for the building and for small monuments.

It is to notice that "M" has no such hem in the south, what is important for building and

freestanding small monuments.

The Namur- Vesdre- Aachen tradition

A group of stonecutters used carboniferous limsestone found along the Meuse River, from Namur until Liège (and as far as Aachen).

Guilds of stonecutters ? Information

Some discoidal crosses in the Pyrenees, on the Continent and in Kent resemble so much to each other, that a production by travelling craftssmen becomes probable, concordant to the uses in the mediaeval building yards.

references Information

  • Dreesen, Roland + Dusar, M. + Doperé, F., 2001. Atlas Natuursteen in Limburgse monumentenx- 2e druk. LIKONA. ISBN 90 - 74605 - 18 - 4
  • Groessens, Eric, 1993. Calcaires et grès mésozoiques exploités comme pierre de construction en Gaume ( Belgique) et dans le Gutland (Grand Duché de Luxembourg) in: Geologie, tijdschrift.
  • Groessens, Eric, 1991. Les matériaux de construction des formations d’age secondaire Belgo-Luxembourgeoises.
  • histopale , s.d. Les materiaux de construction du boulonnais = Mémoires du canton de marquise - l’ histoire des communes du canton de marquise mise a votre disposition par histopale. online: http://membres.lycos.fr/histopale/materio1.htm
  • Jonghe, Sabine de + Tourneur, Francis + Ducarme, Pierre + Groessens, Eric + e.a., , , 1996. Pierres à bâtir traditionnelles de la Wallonie - manuel de terrain. Jambes / Louvain la Neuve ucl,chab / dgrne / region wallonne.
  • Slinger, A. + Janse, H. + Berends, G. , 1980. Natuursteen in monumenten. Zeist / Baarn Rijksdienst voor de Monumentenzorg.

cfr. online.


From Wikipedia, the free encyclopedia

Geologic roots of artifacts and geologic influences on them

Geoarchaeologists are i.a. concerned with the geological facts that affect the ontstaan and the waardevermindering - affevtés of artifacts.

Archaeological geology (term coined by Werner Kasig 1980), a sub-field of geology, rather emphasises te value of earth constituents for human life.

_________

Archaeological geology

Archaeological geology (term coined by Werner Kasig 1980), is a sub-field of geology which emphasises te value of earth constituents for human life.

________

Some graves are marked by impressive monuments but the majority of grave markers are ordinary. These markers show the creativity of craftsmen stonecutters. The study of markers is an application of Archaeological geology.

This article concerns mainly the North East of the European continent, with some extension to Guilds of stonecutters.

File:Noorb 003 004 018 017 p3 27.jpg

The North East of the continent Information

Digging stone stimulated headstone traditions in the North East of the continent : a Boulonnais tradition, a Tournay- Ecaussines tradition, a Namur- Vesdre- Aachen tradition, a Wadden tradition, a Nievelstein tradition, a schiste tradition, a Liedberg tradition, a Siebengebirge tradition, a Mendig basalt tradition, a Lorraine tradition.

Geological base

Soil resources influenced constructing of buildings, as well as the creation of autonomous stone objects. And soil resources are linked to the relief.

In the North East of the European continent, a plain (several "B" 's on the map) is interrupted by a hill system ("M"+"Z"), which was uplifted during the Alpine orogeny: the rising of the Ardennes .

The geology of the "nose","M"+“Z”, can best be understood by means of the profile below, which corresponds to the vertical line "a" - "b" on the map.

The sand, the clay and the somewhat harder rocks of the “B"'s were used in constructing buildings and, to a modest extent, for small monuments.

"M" consists mainly of relatively hard rocks. Those were used for building blocks ( French: moellons, German : Bruchstein) and for small monuments.In the Neighborhood of Cologne ( German Köln) and of Koblenz, vulcanic activity during yy , provided respectivily the yy and the Basalt yy, which gave an yy to ther surroundings and sometimes wide in the ...

In the transient hem "Z", in German “Subvaristischer Saum”, the limestones and sandstones present themself as alternating waves. Those were beloved material for the building and have been appreciated for small autonomous, mostly monolithic monuments, such as headstones.

To the hem "Z" belons also the Ferques inlier ( French: "Boutonnière") in the Boulonnais, south of Calais, only some 60 km2 in surface, with layers from the Middle- Devonian (-385 Ma.) up to the Upper Visean (-325 Ma.). Those layers provided material for the building and for small monuments.

It is to notice that "M" has no such hem in the south, what is important for building and

freestanding small monuments.

The Namur- Vesdre- Aachen tradition

A group of stonecutters used carboniferous limsestone found along the Meuse River, from Namur until Liège (and as far as Aachen).

Guilds of stonecutters ? Information

Some discoidal crosses in the Pyrenees, on the Continent and in Kent resemble so much to each other, that a production by travelling craftssmen becomes probable, concordant to the uses in the mediaeval building yards.

references Information

  • Dreesen, Roland + Dusar, M. + Doperé, F., 2001. Atlas Natuursteen in Limburgse monumentenx- 2e druk. LIKONA. ISBN 90 - 74605 - 18 - 4
  • Groessens, Eric, 1993. Calcaires et grès mésozoiques exploités comme pierre de construction en Gaume ( Belgique) et dans le Gutland (Grand Duché de Luxembourg) in: Geologie, tijdschrift.
  • Groessens, Eric, 1991. Les matériaux de construction des formations d’age secondaire Belgo-Luxembourgeoises.
  • histopale , s.d. Les materiaux de construction du boulonnais = Mémoires du canton de marquise - l’ histoire des communes du canton de marquise mise a votre disposition par histopale. online: http://membres.lycos.fr/histopale/materio1.htm
  • Jonghe, Sabine de + Tourneur, Francis + Ducarme, Pierre + Groessens, Eric + e.a., , , 1996. Pierres à bâtir traditionnelles de la Wallonie - manuel de terrain. Jambes / Louvain la Neuve ucl,chab / dgrne / region wallonne.
  • Slinger, A. + Janse, H. + Berends, G. , 1980. Natuursteen in monumenten. Zeist / Baarn Rijksdienst voor de Monumentenzorg.

cfr. online.



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