ST rock: Difference between revisions
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|dimension=height 4 m, width 3 m | |dimension=height 4 m, width 3 m | ||
|condition=damaged | |condition=damaged | ||
|date_derivation=natural science | |date_derivation=natural science | ||
|site=Brandenberg | |site=Brandenberg | ||
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== Commentary == | == Commentary == | ||
Further references more related to the inscriptions: {{bib|Vetter 1957}}; {{bib|Prosdocimi 1971}}. The inscriptions date to the [[index::chronological classification|La Tène period]].<br>The find place is located in the [[index::Steinberg am Rofan|Steinberg]] / Achensee region which is part of the Northern Limestone Alps. This mountain range is made of lighter and more porous rock at which the major component is limestone. Additionally dolomite, marl, sandstone or comparable components appear. | Further references more related to the inscriptions: {{bib|Vetter 1957}}; {{bib|Prosdocimi 1971}}. The inscriptions date to the [[index::chronological classification|La Tène period]].<br>The find place is located in the [[index::Steinberg am Rofan|Steinberg]] / Achensee region which is part of the Northern Limestone Alps. This mountain range is made of lighter and more porous rock at which the major component is limestone. Additionally dolomite, marl, sandstone or comparable components appear. | ||
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{{bibliography}} | {{bibliography}} |
Revision as of 16:35, 12 October 2018
Object | |
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Classification: | rock |
Material: | limestone |
Size: | height 4 m, width 3 m |
Condition: | damaged |
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Site: | Brandenberg (Tirol, Austria) |
Field name: | Schneidjoch, Wildalm |
Coordinates (approx.): | 47° 34' 11.00" N, 11° 47' 32.00" E |
Find date: | 1957 |
Find circumstances: | by chance |
Current location: | in situ |
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Inscriptions: | |
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Sources: | Schumacher 2004: 191, 219–220 |
Commentary
Further references more related to the inscriptions: Vetter 1957; Prosdocimi 1971. The inscriptions date to the La Tène period.
The find place is located in the Steinberg / Achensee region which is part of the Northern Limestone Alps. This mountain range is made of lighter and more porous rock at which the major component is limestone. Additionally dolomite, marl, sandstone or comparable components appear.
Bibliography
Gleirscher 1991 | Paul Gleirscher, Die Räter, Chur: Rätisches Museum 1991. |
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Kusch 2000 | Heinrich Kusch, "Zur Halbhöhle (Kat.Nr. 1262/6, iBA-704) und einem neuen Felsbildfundplatz am Schneidjoch, Steinberg in Tirol, Austria", in: Manfred Hainzmann (ed.), VOTIS XX SOLVTIS. Jubiläumsschrift der Archäologischen Gesellschaft Steiermark, Graz: Academic Publishers 2000. (= AGST Nachrichtenblatt 1–2 [1999]), 199–208. |
Mandl 2011 | Franz Mandl, Felsbilder. Österreich – Bayern: Nördliche Kalkalpen [= Anisa – Verein für alpine Forschung 4], Haus im Ennstal: 2011. |