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is made technically easier because of the separation of the beds with alternating outcrops and fissures, because the fissures are vertical and the beds run roughly at right angles to them. As a result, it is possible to cut rectangular blocks of unfinished stone. The thickness of the quarry-able
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and its colours range from whitish to grey and yellowish grey. In the south of the area Cotta
Sandstone is medium-grained, whilst, in the north it is fine-grained. Around the village of Cotta itself the grain size is evenly sized at 0.1 to 0.22 millimetres and only very rarely as large as 0.3
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and
Gersdorf, which was larger-grained, was cut not only for use as building or sculpting stone, but also for millstones. Today (2008) Cotta Sandstone is used for solid window and door frames,
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work and high-profile stonemasonry. It is especially used in restoration, but also in new structures. Its most important use is for sculptures.
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sandstone beds varies from a ½ to 3 metres. The thickness of the deposits of Cotta
Sandstone ranges between 50 and 80 metres.
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The technical value of this natural stone varies considerably, because the quartz grains of Cotta
Sandstone are frequently
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and carbon elements. The carbon particles are arranged in clearly recognisable veins. They occasionally resemble
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Die nutzbaren
Gesteine Deutschlands und ihre Lagerstätten mit Ausnahme der Kohlen, Erze und Salze,
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323:. In: Geologica Saxonica Journal of Central European Geology 52/53 (2007), p. 143-204 (
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and in its numerous tributary valleys. Its main deposit lies in the west of the
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millimetres. The rock contains the smallest elements of mica minerals (
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160:(in the villages of Gottleuba and Berggießhübel), Langhennersdorf,
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Dienemann/Burre: Die nutzbaren
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Dienemann/Burre: Die nutzbaren
Gesteine Deutschlands, p. 303
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bonded, but it has many unevenly divided deposits of the
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38:Cotta Sandstone quarry in the Lohmgrund near Cotta
50:, Dresden, Door frames in sandstone of type:
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274:University of Arts, Berlin, Fasanenstraße
27:- west side in Dresden, sandstone type:
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92:, an area where the stone is quarried.
206:Formerly the sandstone quarried near
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84:. It is named after the village of
350:Technical data for Cotta Sandstone
100:Cotta Sandstone was formed in the
16:Type of sandstone found in Germany
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355:Information about Elbe Sandstone
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238:Reich Court building in Leipzig
227:Art-historic use of Cotta Stone
23:Stone sculpture relief on the
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316:Enke-Verlag, Stuttgart 1929.
345:Pictures of Cotta Sandstone
312:W. Dienemann und O. Burre:
158:Bad Gottleuba-Berggießhübel
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188:valley. The quarrying of
152:The stone is quarried in
415:Elbe Sandstone Mountains
296:Reinhardtsdorf Sandstone
184:(Ottendorf), and in the
96:Formation and properties
78:Elbe Sandstone Mountains
48:Palucca School of Dance
108:age. It is one of the
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46:Main entrance of the
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420:Quarries in Germany
372:Siegfried Grunert:
319:Siegfried Grunert:
330:2012-03-23 at the
286:List of sandstones
88:in the borough of
72:) is found in the
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66:Cottaer Sandstein
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301:Wehlen Sandstone
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332:Wayback Machine
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208:Langhennersdorf
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190:Elbe sandstones
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134:phyllosilicates
110:Elbe sandstones
104:, in the Lower
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58:Cotta Sandstone
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156:(Groß-Cotta),
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325:Digitalisat
202:General use
186:Krippenbach
130:siliceously
74:Elbe Valley
404:Categories
361:References
148:Extraction
125:textures.
115:glauconite
102:Cretaceous
410:Sandstone
262:TU Berlin
216:sculpture
172:south of
170:Lohmgrund
142:kaolinite
328:Archived
280:See also
182:Bahretal
178:Gersdorf
166:Neundorf
119:feldspar
106:Turonian
25:Altmarkt
307:Sources
222:Gallery
138:illite
123:marble
62:German
176:, in
174:Pirna
164:, at
154:Dohma
90:Dohma
86:Cotta
82:Pirna
52:Cotta
29:Cotta
180:and
168:and
140:and
197:Use
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