Norsk versjon | |||||
THE NATURAL STONE DATABASE | |||||
Deposit Area 1129 - 601 | |||||
(Last updated 12.jan.2024) |
Name of Deposit Area : Eiane |
(Object Id : 1129,601,00,00) |
Location |
County : | Rogaland (11) | Municipality : | Forsand (1129) |
Map 1:50000: | Høle (1212-1) | Map 1:250000: | Haugesund |
Marking point: | Longitude: | 6.1734370 | Latitude: | 58.9585040 |
EU89-UTM Zone 32 | (Coordinates IS confirmed) |
X-coord: | 337442 m. | Y-coord: | 6538867 m. |
|
Commodity |
Main Type: | Granite and other igneous rocks | Sub Type: | Granite | |
Brickstone(Y/N): | N |
Production |
Activity: | Stone quarrying | Reserves: | ||
Prod. method: | Open pit mining | Production: | ||
Prod. status: | Disused, closed | Volume of dump: |
Importance |
Public: | Not Assessed (reg. 21.03.2017) |
Economical: | Could be significant , (Confirmed 03.jan.2006 by Bjørn Lund) |
Products |
Commercial Name | Product description |
Granitt | Classification :Massive blocks | Colour :Grayish | |
Play of colours : | Uniformity :Good | ||
Lithology :Granite | Grain size :Coarse grained (> 3 mm) |
Mineralogy: |
Feldspar | Major mineral (>10%) | ||
Quartz | Major mineral (>10%) | ||
Mica | Major mineral (>10%) |
|
Operations |
From - To | Activity | Comments | |
1899 - 1955 | Regular production | Company/Institution :Haabeth fra Stavanger |
Deposit rock |
Lithology: | Granite | Weathering colour: | Gray | |
Era: | Period: | |||
Dating: | Method: | |||
Genesis: | Magmatic | Form: | Massive | |
Main texture: | Structureless |
Main grain size: | Coarse grained (> 3 mm) | Main alteration: |
Strike/Dip: | Direction: | |||
Plunge: |
Stratigraphic classification of host rock |
Era: | Period: |
Province: | ||
Geotec.unit: | ||
Tectonic complex: | ||
Igneous complex: |
Group: | Formation: |
Structures |
Location: | Type: | Orientation(360 gr.): | Relation to min.: | |
Not defined | Exfoliation |
Information(s) in free text format |
Examples |
Referanser: Gate- og kantstein i Stavanger Rådhuset i Haugesund Stavanger sykehus Teatret i Stavanger |
Location |
Den gamle forekomsten ligger nede ved sjøen på sørøstsiden av Lysefjorden ca 1 mil fra Forsand sentrum. |
Photo(s) from the Deposit area: |
Bibliography: |
From NGU's Reference Archive: |
Oxaal, John , 1916 |
Norsk granit |
;Norges geologiske undersøkelse;TIDSSKRIFTARTIKKEL;NGU; No.76;1-220 pages |
Abstract: | |
This work is a report of granite and the granite industry in Norway. It contains a description of the various fields of granite and similar rocks from a scientific as well as from a technical and economical standpoint. The geological occurrence of the various rocks, their chemical and mineralogical composition, are thoruoughlyoughly treated, also the questions of practical interest, as the quality and other technical properties, further the problems of location and conditions for transport, conditions for quarrying and otherquestions of interest in the utilization of the various occurrences of granite. Granite: This chapter consideres first the mineralogical and chemical composition of the granite, and the various types of granite resulting from the varying composition; thereafter the most important structural types and how these are dependent on the geological appearance of the rock. Lakkolites and other froms assumed by granite masses when injected into the crust of the earth, are mentioned; some examples of beautifully formed lakkolites are also mentioned. The question of sheet structure and rift in the granite are of great importance in its utilization, and are of interest both practically and theoretically. |
References not to be found in NGU's Reference Archive.: |
Engen, S. (1981). Forsandboka: gards- og ættesoge. Forsand kommune. |
The fact sheet was created on 20.01.2025 |
Questions or comments regarding the fact sheet can be emailed to: ressursdatabaser@ngu.no |
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