Thortveitite
A valid IMA mineral species - grandfathered
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About Thortveitite
Formula:
Sc2Si2O7
Often contains Y (and minor HREE) replacing Sc.
Colour:
Greyish-green, black, grey, blue, yellow, brown
Lustre:
Vitreous, Dull
Hardness:
6 - 7
Specific Gravity:
3.27 - 3.58
Crystal System:
Monoclinic
Member of:
Name:
Named in 1911 by Jakob Grubbe Cock Schetelig in honour of Gunder Olaus Olsen Thortveit (1 October 1872, Thortveit, Iveland, Aust-Agder, Norway - 15 June 1917, Rossås, Iveland, Aust-Agder, Norway), feldspar and mineral exporter from Iveland, Norway.
The mineral was first found in 1903 by the Norwegian geologist Per (Peder) Elisæus Schei (1875–1905) in Beryllbruddet (The Beryl Quarry)", Landsverk, Evje, Norway, but the sample was labelled by him as "epidote". Later, in 1910, Olaus Thortveit sent some samples of the mineral from another locality, from a quarry at Ljosland, Iveland, Norway to Professor Schetelig who recognized it as a new mineral.
The mineral was first found in 1903 by the Norwegian geologist Per (Peder) Elisæus Schei (1875–1905) in Beryllbruddet (The Beryl Quarry)", Landsverk, Evje, Norway, but the sample was labelled by him as "epidote". Later, in 1910, Olaus Thortveit sent some samples of the mineral from another locality, from a quarry at Ljosland, Iveland, Norway to Professor Schetelig who recognized it as a new mineral.
This page provides mineralogical data about Thortveitite.
Unique Identifiers
Mindat ID:
3950
Long-form identifier:
mindat:1:1:3950:1
IMA Classification of Thortveitite
Approved, 'Grandfathered' (first described prior to 1959)
First published:
1911
Classification of Thortveitite
9.BC.05
9 : SILICATES (Germanates)
B : Sorosilicates
C : Si2O7 groups, without non-tetrahedral anions; cations in octahedral [6] and greater coordination
9 : SILICATES (Germanates)
B : Sorosilicates
C : Si2O7 groups, without non-tetrahedral anions; cations in octahedral [6] and greater coordination
55.2.1a.4
55 : SOROSILICATES Si2O7 Groups,Generally with no Additional Anions
2 : Si2O7 Groups, Generally with no Additional Anions with cations in [6] coordination
55 : SOROSILICATES Si2O7 Groups,Generally with no Additional Anions
2 : Si2O7 Groups, Generally with no Additional Anions with cations in [6] coordination
14.8.5
14 : Silicates not Containing Aluminum
8 : Silicates of Group III metals other than Al
14 : Silicates not Containing Aluminum
8 : Silicates of Group III metals other than Al
Mineral Symbols
As of 2021 there are now IMA–CNMNC approved mineral symbols (abbreviations) for each mineral species, useful for tables and diagrams.
| Symbol | Source | Reference for Standard |
|---|---|---|
| Tvt | IMA–CNMNC | Warr, L.N. (2021). IMA–CNMNC approved mineral symbols. Mineralogical Magazine, 85(3), 291-320. doi:10.1180/mgm.2021.43 |
Physical Properties of Thortveitite
Vitreous, Dull
Transparency:
Translucent, Opaque
Colour:
Greyish-green, black, grey, blue, yellow, brown
Streak:
White
Hardness:
6 - 7 on Mohs scale
Tenacity:
Brittle
Fracture:
Irregular/Uneven, Conchoidal
Density:
3.27 - 3.58 g/cm3 (Measured) 3.32 g/cm3 (Calculated)
Optical Data of Thortveitite
Type:
Biaxial (-)
RI values:
nα = 1.756 nβ = 1.793 nγ = 1.809
2V:
Measured: 65° , Calculated: 64°
Max. Birefringence:
δ = 0.053
Based on recorded range of RI values above.
Based on recorded range of RI values above.
Interference Colours:
The colours simulate birefringence patterns seen in thin section under crossed polars. They do not take into account mineral colouration or opacity.
Michel-Levy Bar The default colours simulate the birefringence range for a 30 µm thin-section thickness. Adjust the slider to simulate a different thickness.
Grain Simulation You can rotate the grain simulation to show how this range might look as you rotated a sample under crossed polars. Each grain retains its interference colour (retardation) while its brightness falls to black at extinction and reaches a maximum between extinction positions.
The colours simulate birefringence patterns seen in thin section under crossed polars. They do not take into account mineral colouration or opacity.
Michel-Levy Bar The default colours simulate the birefringence range for a 30 µm thin-section thickness. Adjust the slider to simulate a different thickness.
Grain Simulation You can rotate the grain simulation to show how this range might look as you rotated a sample under crossed polars. Each grain retains its interference colour (retardation) while its brightness falls to black at extinction and reaches a maximum between extinction positions.
Surface Relief:
Very High (positive)
Relative to Canada balsam mounting medium (n ≈ 1.537).
Relative to Canada balsam mounting medium (n ≈ 1.537).
This shows the grain boundary and Becke line effect under plane-polarised
light, based on the contrast between this mineral's average refractive
index and the mounting medium. It does not take into account mineral
colouration.
In focus
Interference Figure:
This shows the idealized biaxial acute bisectrix (Bxa) interference figure
- the conoscopic view for a grain cut perpendicular to the acute bisectrix, using
this mineral's 2V. The two small white dots mark the melatopes - the points
where the two optic axes emerge - and are shown only when they fall within the
field of view. The coloured bands are isochromatics, and the dark bands are
isogyres.
Rotate the stage: at 0°/90° the isogyres form a cross through the melatopes; at 45° they pull apart into curved hyperbolas. That splitting on rotation - absent in a uniaxial figure - is the standard diagnostic test for telling biaxial minerals from uniaxial ones. If 2V is large, the melatopes may fall outside the field of view, as they often do at the microscope too.
Rotate the stage: at 0°/90° the isogyres form a cross through the melatopes; at 45° they pull apart into curved hyperbolas. That splitting on rotation - absent in a uniaxial figure - is the standard diagnostic test for telling biaxial minerals from uniaxial ones. If 2V is large, the melatopes may fall outside the field of view, as they often do at the microscope too.
Dispersion:
distinct to strong
Optical Extinction:
X ∧ c = 5°.
Pleochroism:
Visible
Comments:
X = deep green; Y = Z = brownish yellow in thick grains.
Comments:
Absorption: X >= Y = Z.
Chemistry of Thortveitite
Mindat Formula:
Sc2Si2O7
Often contains Y (and minor HREE) replacing Sc.
Often contains Y (and minor HREE) replacing Sc.
Element Weights:
Elements listed:
Common Impurities:
Zr,Hf,Al,Fe,Mn,Mg,Ca,Ce,TR
Chemical Analysis
Oxide wt%:
| 1 | 2 | 3 | 4 | 5 | 6 | |
|---|---|---|---|---|---|---|
| SiO2 | 44.13 % | 45.79 % | 44.36 % | 37.59 % | 46.21 % | 44.60 % |
| Sc2O3 | 41.76 % | 34.32 % | 46.76 % | 25.01 % | 48.94 % | 47.66 % |
| ZrO2 | 9.96 % | 2.28 % | ||||
| Fe2O3 | 2.20 % | 2.95 % | 0.99 % | 2.06 % | 1.57 % | |
| Al2O3 | 2.62 % | 4.95 % | 0.04 % | 0.61 % | 0.81 % | |
| MgO | 0.17 % | 0.26 % | 0.06 % | |||
| MnO | 0.53 % | 1.74 % | 0.67 % | 0.03 % | ||
| ThO2 | 0.09 % | |||||
| La2O3 etc. | 1.48 % | |||||
| Y2O3 etc | 9.52 % | |||||
| TiO2 | 0.01 % | 0.30 % | ||||
| U2O3 | 0.00 % | |||||
| CaO | 0.24 % | 0.11 % | 0.19 % | 0.10 % | ||
| H2O | 0.07 % | |||||
| Y2O3 | 1.78 % | 17.73 % | 1.94 % | |||
| SnO2 | 3.64 % | |||||
| Dy2O3 | 1.38 % | 0.35 % | ||||
| Er2O3 | 1.65 % | 0.33 % | ||||
| Tm2O3 | 0.54 % | 0.07 % | ||||
| Yb2O3 | 7.01 % | 0.74 % | ||||
| Lu2O3 | 1.68 % | 0.23 % | ||||
| HfO2 | 0.55 % | |||||
| Ce2O3 | 0.26 % | |||||
| Gd2O3 | 0.05 % | |||||
| FeO | 1.48 % | |||||
| Na2O | 0.03 % | |||||
| K2O | 0.18 % | |||||
| P2O5 | 0.03 % | |||||
| Total: | 100.67 % | 100.12 % | 99.42 % | 99.21 % | 100.69 % | 95.28 % |
Sample references:
| ID | Locality | Reference | Notes |
|---|---|---|---|
| 1 | Befanamo pegmatite, Beronono Commune, Anjozorobe District, Analamanga, Madagascar | Sample found by Rasamoel in 1918 and examined and described by Lacroix (1922) | |
| 2 | Eptevatnet 02 Thortveitite Quarry, Iveland, Agder, Norway | ||
| 3 | Heftetjern pegmatite, Tørdal, Drangedal, Telemark, Norway | Electron-microprobe | |
| 4 | Iveland, Agder, Norway | ||
| 5 | Kola Peninsula, Murmansk Oblast, Russia | ||
| 6 | Crystal Mountain Fluorspar Mine, Sapphire Mountains Area, Ravalli County, Montana, USA |
Crystallography of Thortveitite
Crystal System:
Monoclinic
Class (H-M):
2/m - Prismatic
Space Group:
B2/m
Setting:
C2/m
Cell Parameters:
a = 6.65 Å, b = 8.61 Å, c = 4.68 Å
β = 102.2°
β = 102.2°
Ratio:
a:b:c = 0.772 : 1 : 0.544
Unit Cell V:
261.91 ų (Calculated from Unit Cell)
Twinning:
Common: twinning axis normal to (110), twinning plane (110).
Crystal Structure
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Data courtesy of the American Mineralogist Crystal Structure Database. Click on an AMCSD ID to view structure
| ID | Species | Reference | Link | Year | Locality | Pressure (GPa) | Temp (K) |
|---|---|---|---|---|---|---|---|
| 0001163 | Thortveitite | Bianchi R, Pilati T, Diella V, Gamaccioli C M, Mannucci G (1988) A re-examination of thortveitite Sample 4 from Malagasy Republic American Mineralogist 73 601-607 | ![]() | 1988 | 0 | 293 | |
| 0001162 | Thortveitite | Bianchi R, Pilati T, Diella V, Gamaccioli C M, Mannucci G (1988) A re-examination of thortveitite Sample 3 from Flat, Evje American Mineralogist 73 601-607 | ![]() | 1988 | 0 | 293 | |
| 0001161 | Thortveitite | Bianchi R, Pilati T, Diella V, Gamaccioli C M, Mannucci G (1988) A re-examination of thortveitite Sample 2 from Setesdalen American Mineralogist 73 601-607 | ![]() | 1988 | 0 | 293 | |
| 0001160 | Thortveitite | Bianchi R, Pilati T, Diella V, Gamaccioli C M, Mannucci G (1988) A re-examination of thortveitite Sample 1 from Iveland American Mineralogist 73 601-607 | ![]() | 1988 | 0 | 293 | |
| 0018032 | Thortveitite | Zachariasen W (1930) The structure of thortveitite, Sc2 Si O7 _cod_database_code 1011147 Zeitschrift fur Kristallographie 73 1-6 | 1930 | 0 | 293 |
CIF Raw Data - click here to close
X-Ray Powder Diffraction
Powder Diffraction Data:
| d-spacing | Intensity |
|---|---|
| 3.14 Å | (100) |
| 2.965 Å | (65) |
| 5.18 Å | (60) |
| 2.596 Å | (50) |
| 3.18 Å | (45) |
| 2.627 Å | (30) |
| 2.200 Å | (25) |
Comments:
Tuftane, Norway.
Geological Environment
Paragenetic Mode(s):
| Paragenetic Mode | Earliest Age (Ga) |
|---|---|
| Stage 1: Primary nebular phases | 4.567-4.561 |
| 3 : Solar nebular condensates (CAIs, AOAs, URIs) | >4.565 |
| Stage 4b: Highly evolved igneous rocks | >3.0 |
| 34 : Complex granite pegmatites |
Type Occurrence of Thortveitite
General Appearance of Type Material:
Crystals to >25 cm long and 4 cm thick. In radial rosettes.
Place of Conservation of Type Material:
Mineralogical-Geological Museum, University of Oslo, Oslo, Norway, number 22340 and 20 other specimens (cotype).
Geological Setting of Type Material:
Granite pegmatite.
Associated Minerals at Type Locality:
Other Language Names for Thortveitite
Dutch:Thortveitiet
German:Thortveitit
Russian:Тортвейтит
Simplified Chinese:钪钇石
Spanish:Thortveitita
Traditional Chinese:鈧釔石
Varieties of Thortveitite
| Befanamite | A variety of thortveitite with a higher content of scandium and zirconium and a lower content of yttrium. First discovered in 1918, in the eluvials of the Befanamo pegmatite, Madagascar by the prospector J. B. Rasamoel. The sample was a 10 x 3 cm fragmen... |
Relationship of Thortveitite to other Species
Member of:
Other Members of Thortveitite Group:
| Keiviite-(Y) | Y2Si2O7 | Mon. 2/m : B2/m |
| Keiviite-(Yb) | Yb2Si2O7 | Mon. 2/m : B2/m |
| Yttrialite-(Y) | (Y,Th)2Si2O7 | Mon. 2/m : P21/m |
Common Associates
Associations Based on Photo Data:
| 20 photos of Thortveitite associated with Quartz | SiO2 |
| 10 photos of Thortveitite associated with Aeschynite-(Y) | Y(TiNb)O6 |
| 10 photos of Thortveitite associated with Euxenite-(Y) | (Y,Ca,Ce,U,Th)(Nb,Ta,Ti)2O6 |
| 9 photos of Thortveitite associated with Ilmenite | Fe2+TiO3 |
| 9 photos of Thortveitite associated with Xenotime-(Y) | Y(PO4) |
| 7 photos of Thortveitite associated with Microcline | K(AlSi3O8) |
| 5 photos of Thortveitite associated with Albite | Na(AlSi3O8) |
| 5 photos of Thortveitite associated with Allanite-(Ce) | (CaCe)(AlAlFe2+)O[Si2O7][SiO4](OH) |
| 4 photos of Thortveitite associated with Pyrite | FeS2 |
| 4 photos of Thortveitite associated with Fluorite | CaF2 |
Related Minerals - Strunz-mindat Grouping
| 9.BC. | Anorthoyttrialite-(Y) | Y4(SiO4)(Si3O10) |
| 9.BC. | Kozłowskiite | Ca4(Fe2+Sn3)[Si2O7]2[Si2O6OH]2 |
| 9.BC.05 | Yttrialite-(Y) | (Y,Th)2Si2O7 |
| 9.BC.05 | Keiviite-(Y) | Y2Si2O7 |
| 9.BC.05 | Keiviite-(Yb) | Yb2Si2O7 |
| 9.BC.05 | Gittinsite | CaZrSi2O7 |
| 9.BC.10 | Parakeldyshite | Na2ZrSi2O7 |
| 9.BC.10 | Keldyshite | (Na,H)2ZrSi2O7 |
| 9.BC.10 | Khibinskite | K2ZrSi2O7 |
| 9.BC.10 | Brunovskyite | NaZrSi2O6(OH) |
| 9.BC.15 | Rankinite | Ca3Si2O7 |
| 9.BC.20 | Barysilite | Pb8Mn2+[Si2O7]3 |
| 9.BC.25 | Edgarbaileyite | [Hg2]2+3[Si2O7] |
| 9.BC.30 | Kristiansenite | Ca4(Sc2Sn2)[Si2O7]2[Si2O6OH]2 |
| 9.BC.30 | Nybergite | Ca4Sc3Sn(Si2O7)(Si2O6OH)3 |
| 9.BC.30 | Silesiaite | Ca4(Fe3+2Sn2)[Si2O7]2[Si2O6OH]2 |
| 9.BC.35 | Percleveite-(Ce) | Ce2Si2O7 |
| 9.BC.35 | Percleveite-(La) | La2Si2O7 |
| 9.BC.40 | Scottyite | BaCu2Si2O7 |
Other Information
Notes:
Powdered material is partially decomposed by concentrated HCl, without gelatinization.
Health Risks:
No information on health risks for this material has been entered into the database. You should always treat mineral specimens with care.
Internet Links for Thortveitite
mindat.org URL:
https://www.mindat.org/min-3950.html
Please feel free to link to this page.
Please feel free to link to this page.
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References for Thortveitite
Reference List:
Schetelig, Jakob (1911) Über Thortveitit, ein neues Mineral. Vorläufige Mitteilung. Centralblatt für Mineralogie, Geologie und Paläontologie, 1911. 721-726
Schetelig, Jakob (1922) Thortveitite. A silicate of scandium (Sc,Y)2Si207. Norsk Geologisk Tidsskrift [Norwegian Journal of Geology], 6 (3-4) 233-244
Neumann, Henrich (1961) The scandium content of some norwegian minerals and the formation of Thortveitite, a reconnaissance survey. Norsk Geologisk Tidsskrift [Norwegian Journal of Geology], 41 (2-3-4). 197-210
Sakurai, Kin-ichi, Nagashima, Kozo, Kato, Akira (1962) Thortveitite from Kobe, Omiya, Kyoto, Japan. Bulletin of the Chemical Society of Japan, 35 (11). 1776-1779 doi:10.1246/bcsj.35.1776
Ross, S.D. (1971) The vibrational spectrum of thortveitite. Spectrochimica Acta Part A: Molecular Spectroscopy, 27 (9). 1837-1843 doi:10.1016/0584-8539(71)80236-2
Dowty, Eric (1987) Vibrational interactions of tetrahedra in silicate glasses and crystals. III. Calculations on simple sodium and lithium silicates, thortveitite and rankinite. Physics and Chemistry of Minerals, 14 (6). 542-552 doi:10.1007/bf00308290
Bianchi, Riccardo, Pilati, Tullio, Diella, Valeria, Gramacciou, Carlo Maria, Mannucci, Gregorio (1988) A re-examination of thortveitite. American Mineralogist, 73 (5-6) 601-607
Foord, E. E., Birmingham, S. D., Demartin, F., Pilati, T., Gramaccioli, C. M., Lichte, F. E. (1993) Thortveitite and associated Sc-bearing minerals from Ravalli County, Montana. The Canadian Mineralogist, 31 (2) 337-346 doi:10.3749/1499-1276-31.2.337
Langhof, J. (1996) Thortveitite from granitic NYF pegmatites in Sweden. GFF, 118. 54 doi:10.1080/11035899609546336
Kristiansen, Roy (1997) Thortveititt- et historisk tilbakeblikk og dagens status, in Kongsberg Mineralsymposium 1997. STEIN. Nordisk magasin for populær geologi, 24 (3) 111-115
Kristiansen, Roy (1997) Thortveititt Sc2Si2O7- et historisk tilbakeblikk og dagens status [Thortveitite Sc2Si2O7- a historical review and current status]. Norsk Bergverksmuseum Skrift, 12. 22-25
Gramaccioli, C. M., Diella, V., Demartin, F., Orlandi, P., Campostrini, I. (2000) Cesian bazzite and thortveitite from Cuasso al Monte, Varese, Italy: A comparison with the material from Baveno, and inferred origin. The Canadian Mineralogist, 38 (6) 1409-1418 doi:10.2113/gscanmin.38.6.1409
Spandler, Carl, Hermann, Jörg, Rubatto, Daniela (2004) Exsolution of thortveitite, yttrialite, and xenotime during low-temperature recrystallization of zircon from New Caledonia, and their significance for trace element incorporation in zircon. American Mineralogist, 89 (11) 1795-1806 doi:10.2138/am-2004-11-1226
Chapman, R., Mercer, I.F., Rankin, A.H., Spratt, J. (2008) Thortveitite — a new gemstone. The Journal of Gemmology, 31 (1) 1-6 doi:10.15506/jog.2008.31.1.1
Allix, M., Alba, M. D., Florian, P., Fernandez-Carrion, A. J., Suchomel, M. R., Escudero, A., Suard, E., Becerro, A. I. (2011) Structural elucidation of β-(Y,Sc)2Si2O7: combined use of 89Y MAS NMR and powder diffraction. Journal of Applied Crystallography, 44 (4). 846-852 doi:10.1107/s0021889811021303
Localities for Thortveitite
Showing 87 localities.
Locality List
- This locality has map coordinates listed.
- This locality has estimated coordinates.
ⓘ - Click for references and further information on this occurrence.
? - Indicates mineral may be doubtful at this locality.
- Good crystals or important locality for species.
- World class for species or very significant.
(TL) - Type Locality for a valid mineral species.
(FRL) - First Recorded Locality for everything else (eg varieties).
All localities listed without proper references should be considered as questionable.
Austria | |
| Putz (2007) |
Brazil | |
| Kristiansen (1997) | |
Bulgaria | |
| Georgieva et al. (2023) |
Canada | |
| Potter et al. (2005) |
Chile | |
| Alarcón Novoa (2019) |
China | |
| Liu et al. (2023) +2 other references |
| Sun et al. (2021) |
| Lee (1970) |
| Liu et al. (2025) |
Czech Republic | |
| Výravský et al. (2017) |
DR Congo | |
| Aganze (2018) |
Finland | |
| Ilkka Mikkola collection +1 other reference |
France | |
| Journet et al. (2016) +1 other reference |
| Spandler +1 other reference |
| Gatel et al. (2002) |
Germany | |
| Witzke et al. (2003) |
Italy | |
| Barresi et al. (2005) +1 other reference |
| Bracco et al. (2006) |
| Guastoni A. +1 other reference |
| Gramaccioli et al. (2000) +3 other references |
| Marello et al. (2020) |
| Marello et al. (2020) | |
| Piccoli et al. (2007) |
| Grill (1935) |
| Cuchet et al. (2023) +2 other references |
| Cuchet et al. (2023) +1 other reference | |
| Orlandi et al. (2013) +1 other reference |
| Tanca et al. (2007) |
Japan | |
| Sakurai et al. (1962) |
| Masutomi Museum specimens | |
| Yamada et al. (1980) |
Kazakhstan | |
| geo.web.ru (2007) |
| A.V. Stepanov data |
Madagascar | |
| [var: Befanamite] Lacroix (1922) +1 other reference |
| Guigues (1955) +1 other reference |
| Guigues (1955) | |
| Ferraris et al. (2020) |
| [var: Befanamite] Behier (1960) |
| [var: Befanamite] Behier (1960) |
Norway | |
| Neumann (1961) +1 other reference |
| Bjørlykke (1935) |
| Schetelig (1922) +1 other reference | |
| Frigstad (1968) | |
| Schetelig (1922) | |
| Levinson et al. (1960) +2 other references | |
| Pedersen (2007) |
| Schetelig (1922) +1 other reference | |
| Neumann et al. (1960) |
| Nordrum (2004) +1 other reference | |
| Bjørlykke (1935) |
| Bjørlykke (1935) |
| Nordrum (2005) | |
| [Ronald Werner] +1 other reference | |
| Schetelig (1922) |
| Bjørlykke (1935) | |
| Rudy Bolona photo and specimen | |
| Corneliussen (2012) | |
| Bjørlykke (1935) | |
| Husdal (2021) |
| Knut Edvard Larsen collection & Roy ... +2 other references |
| Steffenssen (2018) |
| Amli (1977) |
| Mathiesen (1970) |
| Svein (1988) +1 other reference | |
Poland | |
| Evans et al. (2018) +1 other reference |
| Chabros E. |
Russia | |
| Egorov et al (1993) |
| Kainov (1973) |
| Kozlov et al. (n.d.) |
| Voloshin et al. (1991) |
| Kompanchenko et al. (2018) +1 other reference |
Saudi Arabia | |
| Gahlan et al. (2021) |
Sweden | |
| Langhof (1996) |
| Langhof (1996) |
| Langhof (1996) |
| Kjellman (analyst) +1 other reference |
Switzerland | |
| Cuchet et al. (2014) |
USA | |
| Parker & Havens (1963) +1 other reference |
| Foord et al. (1993) +1 other reference |
| Dunn (1995) |
| Dunn et al. (1990) +1 other reference |
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The
Knipan, Ljosland, Iveland, Agder, Norway