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Ampegama quarry, Galle District, Southern Province, Sri Lankai
| Regional Level Types | |
|---|---|
| Ampegama quarry | Quarry |
| Galle District | District |
| Southern Province | Province |
| Sri Lanka | Country |
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Latitude & Longitude (WGS84):
6° 11' 41'' North , 80° 8' 54'' East
Latitude & Longitude (decimal):
Type:
KĂśppen climate type:
Nearest Settlements:
| Place | Population | Distance |
|---|---|---|
| Hikkaduwa | 1,300 (2012) | 8.0km |
| Ambalangoda | 20,133 (2012) | 11.4km |
| Galle | 93,118 (2012) | 19.1km |
| Unawatuna | 2,000 (2013) | 22.3km |
| Talpe | 3,000 (2013) | 26.0km |
In the Ampegama area, charnockitic gneiss, calc-silicate and garnet-bearing quartzofeldspathic rocks crop out.
"In the Ampegama quarry, a large charnockitic gneiss is mined. There are calc-silicate rocks that occur mainly as dyke-like bands cross-cutting the major foliation of the rock with reaction zones in close proximity to the surrounding
charnockitic gneiss." (Sameera et al., 2026).
Green, euhedral to subhedral grains of ekanite were observed in only some of the calc-silicate dykes.
"In the Ampegama quarry, a large charnockitic gneiss is mined. There are calc-silicate rocks that occur mainly as dyke-like bands cross-cutting the major foliation of the rock with reaction zones in close proximity to the surrounding
charnockitic gneiss." (Sameera et al., 2026).
Green, euhedral to subhedral grains of ekanite were observed in only some of the calc-silicate dykes.
Select Mineral List Type
Standard Detailed Gallery Strunz Chemical ElementsMineral List
8 valid minerals.
Rock Types Recorded
Select Rock List Type
Alphabetical List Tree DiagramDetailed Mineral List:
Gallery:
List of minerals arranged by Strunz 10th Edition classification
| Group 1 - Elements | |||
|---|---|---|---|
| â | Graphite | 1.CB.05a | C |
| Group 3 - Halides | |||
| â | Fluorite | 3.AB.25 | CaF2 |
| Group 4 - Oxides and Hydroxides | |||
| â | Quartz | 4.00.05 | SiO2 |
| â | Ilmenite | 4.CB.05 | Fe2+TiO3 |
| Group 5 - Nitrates and Carbonates | |||
| â | Calcite | 5.AB.05 | CaCO3 |
| Group 9 - Silicates | |||
| â | Titanite | 9.AG.15 | CaTiO(SiO4) |
| â | Wollastonite | 9.DG.05 | Ca3(Si3O9) |
| â | Ekanite | 9.EA.10 | Ca2ThSi8O20 |
| Unclassified | |||
| â | 'Biotite' | - | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| â | 'Feldspar Group' | - | |
| â | 'Calcium Amphibole Subgroup var. Hornblende' | - | AnCa2(Z2+5-mZ3+m)(Si8-(n+m)Al(n+m))(OH,F,Cl)2 |
| â | 'Clinopyroxene Subgroup' | - | |
| â | 'Scapolite' | - | |
| â | 'Plagioclase' | - | (Na,Ca)[(Si,Al)AlSi2]O8 |
| â | 'K Feldspar' | - | |
| â | 'Orthopyroxene Subgroup' | - | |
| â | 'Apatite' | - | Ca5(PO4)3A |
| â | 'Calcium Amphibole Subgroup' | - | AnCa2(C2+5-mC3+m)(Si8-(n+m)Al(n+m))W2 |
| â | 'Mafic minerals' | - | |
List of minerals for each chemical element
| H | Hydrogen | |
|---|---|---|
| H | â Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| H | â Calcium Amphibole Subgroup var. Hornblende | AnCa2(Z2+5-mZm3+)(Si8-(n+m)Al(n+m))(OH,F,Cl)2 |
| C | Carbon | |
| C | â Calcite | CaCO3 |
| C | â Graphite | C |
| O | Oxygen | |
| O | â Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| O | â Calcite | CaCO3 |
| O | â Ekanite | Ca2ThSi8O20 |
| O | â Calcium Amphibole Subgroup var. Hornblende | AnCa2(Z2+5-mZm3+)(Si8-(n+m)Al(n+m))(OH,F,Cl)2 |
| O | â Ilmenite | Fe2+TiO3 |
| O | â Quartz | SiO2 |
| O | â Titanite | CaTiO(SiO4) |
| O | â Wollastonite | Ca3(Si3O9) |
| O | â Plagioclase | (Na,Ca)[(Si,Al)AlSi2]O8 |
| O | â Apatite | Ca5(PO4)3A |
| F | Fluorine | |
| F | â Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| F | â Fluorite | CaF2 |
| F | â Calcium Amphibole Subgroup var. Hornblende | AnCa2(Z2+5-mZm3+)(Si8-(n+m)Al(n+m))(OH,F,Cl)2 |
| Na | Sodium | |
| Na | â Plagioclase | (Na,Ca)[(Si,Al)AlSi2]O8 |
| Mg | Magnesium | |
| Mg | â Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| Al | Aluminium | |
| Al | â Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| Al | â Calcium Amphibole Subgroup var. Hornblende | AnCa2(Z2+5-mZm3+)(Si8-(n+m)Al(n+m))(OH,F,Cl)2 |
| Al | â Plagioclase | (Na,Ca)[(Si,Al)AlSi2]O8 |
| Al | â Calcium Amphibole Subgroup | AnCa2(C2+5-mCm3+)(Si8-(n+m)Al(n+m))W2 |
| Si | Silicon | |
| Si | â Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| Si | â Ekanite | Ca2ThSi8O20 |
| Si | â Calcium Amphibole Subgroup var. Hornblende | AnCa2(Z2+5-mZm3+)(Si8-(n+m)Al(n+m))(OH,F,Cl)2 |
| Si | â Quartz | SiO2 |
| Si | â Titanite | CaTiO(SiO4) |
| Si | â Wollastonite | Ca3(Si3O9) |
| Si | â Plagioclase | (Na,Ca)[(Si,Al)AlSi2]O8 |
| Si | â Calcium Amphibole Subgroup | AnCa2(C2+5-mCm3+)(Si8-(n+m)Al(n+m))W2 |
| P | Phosphorus | |
| P | â Apatite | Ca5(PO4)3A |
| Cl | Chlorine | |
| Cl | â Calcium Amphibole Subgroup var. Hornblende | AnCa2(Z2+5-mZm3+)(Si8-(n+m)Al(n+m))(OH,F,Cl)2 |
| K | Potassium | |
| K | â Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| Ca | Calcium | |
| Ca | â Calcite | CaCO3 |
| Ca | â Ekanite | Ca2ThSi8O20 |
| Ca | â Fluorite | CaF2 |
| Ca | â Calcium Amphibole Subgroup var. Hornblende | AnCa2(Z2+5-mZm3+)(Si8-(n+m)Al(n+m))(OH,F,Cl)2 |
| Ca | â Titanite | CaTiO(SiO4) |
| Ca | â Wollastonite | Ca3(Si3O9) |
| Ca | â Plagioclase | (Na,Ca)[(Si,Al)AlSi2]O8 |
| Ca | â Apatite | Ca5(PO4)3A |
| Ca | â Calcium Amphibole Subgroup | AnCa2(C2+5-mCm3+)(Si8-(n+m)Al(n+m))W2 |
| Ti | Titanium | |
| Ti | â Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| Ti | â Ilmenite | Fe2+TiO3 |
| Ti | â Titanite | CaTiO(SiO4) |
| Fe | Iron | |
| Fe | â Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| Fe | â Ilmenite | Fe2+TiO3 |
| Th | Thorium | |
| Th | â Ekanite | Ca2ThSi8O20 |
Other Regions, Features and Areas containing this locality
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References
Sameera, K. A. Geeth; Hauzenberger, Christoph A.; Fernando, G. W. A. Rohan; Ĺ koda, Radek; Dharmapriya, Prasanna L.; Chanmuang N., Chutimun; Nasdala, Lutz (2026) Formation of ekanite in âantiskarnâ by carbonatitic melt infiltration into charnockitic gneiss, Ampegama, southwestern Highland Complex, Sri Lanka. Contributions to Mineralogy and Petrology, 181 (7). p.52. doi:10.1007/s00410-026-02330-z