2023
General information and occurrence
Quartz (SiO2) is one of the most common mineral and one of the main components of the majority of igneous rocks (e.g. granites). Under conditions favorable for the crystallization (such as voids in rocks), it forms sharp-pointed hexagonal long and slender crystals which are widely used as a popular ornamental stone and also a gemstone in jewellery. Depending on an admixture of coloring oxides, several varieties of these gemstones are differentiated: colorless – rock crystal, purple – amethyst, black – morion.
Quartz also forms veins and lenses in metamorphic and igneous rocks. The vein quartz deposits originate in the result the of the hydrothermal activity as an infill of open fissures and fractures cutting a given rock massif. The quartz infills are characterized by a high content of silica (SiO2) and a low content of coloring oxides (Fe2O3 and TiO2).
In Poland, the vein quartz deposits occur mainly in crystalline rock massifs of the Precambrian and Paleozoic age in the Sudety Mts. (map). The deposits are characterized by a high variability in thickness, a big dip of veins and lenses and a varying quality of a raw material.
The vein quartz is widely used in the industry, starting from the ceramic industry (the production and glazing and decorating bone and fine china, porcelain and porcelite, utility and pottery ware ceramics, technical ceramics) to the production of fire-proof materials, enameller and in the metallurgy. Its purest varieties are used in the manufacturing of high-quality glass and in the chemical and electrotechnical industries.
Resources
The Table 1 presents resources and the current state of the exploration and development of vein quartz deposits.
Table 1. Vein quartz – million tonnesAnticipated economic resources of vein quartz have not changed in comparison with 2022 and amounted to 6.16 million tonnes in 2023. There was a deposit development plan elaborated for the Taczalin 1 deposit and an exploitation concession for the deposit issued. It resulted in the economic resources growth by 0.53 million tonnes (28%) – these resources amounted to 1.88 million tonnes in 2023 accounting for 31% of the total anticipated economic resources of vein quartz in Poland.
In 2023, none of the vein quartz deposits in Poland was exploited. In 2016, the exploitation from the Taczalin deposit ended, whereas the output from the Stanisław deposit was halted in 2005. After the long-lasting lack of exploitation, in spite of the still valid exploitation concession, the Stanisław deposit is still classified as abandoned.
The figure given below shows changes in domestic resources and production of vein quartz in Poland in the years 1989-2023.
The prospects of the new deposits discovery are limited to the already known places of an occurrence. The most favorable conditions for the resources base enlargement occur in the area of the Stanisław deposit extension, in the tectonic zone of the Rozdroże Izerskie ("Izerskie Crossroad"). Prognostic resources of vein quartz are assessed to be equal 2.87 million tonnes and prospective resources 1.33 million tonnes*.
Prepared by: Agnieszka Malon
* Wołkowicz K., Sroga C., 2020 – ‘Kwarc żyłowy (vein quartz)’. In: ‘Bilans perspektywicznych zasobów kopalin Polski wg stanu na 31.12.2018 r.’ (eds. Szamałek K., Szuflicki M., Mizerski W.): 325-328. PIG-PIB, Warszawa [in Polish].
2022
General information and occurrence
Quartz (SiO2) is one of the most common mineral and one of the main components of the majority of igneous rocks (e.g. granites). Under conditions favorable for the crystallization (such as voids in rocks), it forms sharp-pointed hexagonal long and slender crystals which are widely used as a popular ornamental stone and also a gemstone in jewellery. Depending on an admixture of coloring oxides, several varieties of these gemstones are differentiated: colorless – rock crystal, purple – amethyst, black – morion.
Quartz also forms veins and lenses in metamorphic and igneous rocks. The vein quartz deposits originate in the result the of the hydrothermal activity as an infill of open fissures and fractures cutting a given rock massif. The quartz infills are characterized by a high content of silica (SiO2) and a low content of coloring oxides (Fe2O3 and TiO2).
In Poland, the vein quartz deposits occur mainly in crystalline rock massifs of the Precambrian and Paleozoic age in the Sudety Mts. (map). The deposits are characterized by a high variability in thickness, a big dip of veins and lenses and a varying quality of a raw material.
The vein quartz is widely used in the industry, starting from the ceramic industry (the production and glazing and decorating bone and fine china, porcelain and porcelite, utility and pottery ware ceramics, technical ceramics) to the production of fire-proof materials, enameller and in the metallurgy. Its purest varieties are used in the manufacturing of high-quality glass and in the chemical and electrotechnical industries. The quartz vein is also the source of a high-quality quartz powder and fine grade crushed grains (types I and III according to the industry standard No BN-80-6714-19).
Resources
The Table 1 presents resources and the current state of the exploration and development of vein quartz deposits.
Anticipated economic resources of vein quartz decreased by 24.1 thousand tonnes in comparison with 2021 and amounted in 2022 to 6.16 million tonnes. It was the result of the approval of a new geological documentation with recalculated resources (the Supplement No 1) for the Taczalin 1 deposit. The supplement was elaborated to reclassify the resources from the C2 category to C1 category.
In 2022, any of the vein quartz deposits in Poland was exploited. In 2016, the exploitation from the Taczalin deposit ended, whereas the output from the Stanisław deposit was halted in 2005. After the long-lasting lack of exploitation, in spite of the still valid exploitation concession, the Stanisław deposit is still classified as abandoned. The economic resources of this deposit are equal 1.35 million tonnes accounting for 22% of the total anticipated economic resources of vein quartz in Poland.
The figure given below shows changes in domestic resources and production of vein quartz in Poland in the years 1989-2022.
The prospects of the new deposits discovery are limited to the already known places of an occurrence. The most favorable conditions for the resources base enlargement occur in the area of the Stanisław deposit extension, in the tectonic zone of the Rozdroże Izerskie ("Izerskie Crossroad"). Prognostic resources of vein quartz are assessed to be equal 2.87 million tonnes and prospective resources 1.33 million tonnes*.
Prepared by: Agnieszka Malon
* Wołkowicz K., Sroga C., 2020 – ‘Kwarc żyłowy (vein quartz)’. In: ‘Bilans perspektywicznych zasobów kopalin Polski wg stanu na 31.12.2018 r.’ (eds. Szamałek K., Szuflicki M., Mizerski W.): 325-328. PIG-PIB, Warszawa [in Polish].
2021
General information and occurrence
Quartz (SiO2) is one of the most common mineral and one of the main components of the majority of igneous rocks (e.g. granites). Under conditions favorable for the crystallization (such as voids in rocks), it forms sharp-pointed hexagonal long and slender crystals which are widely used as a popular ornamental stone and also a gemstone in jewellery. Depending on an admixture of coloring oxides, several varieties of these gemstones are differentiated: colorless – rock crystal, purple – amethyst, black – morion.
Quartz also forms veins and lenses in metamorphic and igneous rocks. The vein quartz deposits originate in the result the of the hydrothermal activity as an infill of open fissures and fractures cutting a given rock massif. The quartz infills are characterized by a high content of silica (SiO2) and a low content of coloring oxides (Fe2O3 and TiO2).
In Poland, the vein quartz deposits occur mainly in crystalline rock massifs of the Precambrian and Paleozoic age in the Sudety Mts. (map). The deposits are characterized by a high variability in thickness, a big dip of veins and lenses and a varying quality of a raw material.
The vein quartz is widely used in the industry, starting from the ceramic industry (the production and glazing and decorating bone and fine china, porcelain and porcelite, utility and pottery ware ceramics, technical ceramics) to the production of fire-proof materials, enameller and in the metallurgy. Its purest varieties are used in the manufacturing of high-quality glass and in the chemical and electrotechnical industries. The quartz vein is also the source of a high-quality quartz powder and fine grade crushed grains (types I and III according to the industry standard No BN-80-6714-19).
Resources
The Table 1 presents resources and the current state of the exploration and development of vein quartz deposits.
Anticipated economic resources of vein quartz increased by 569.24 thousand tonnes in comparison with 2020 and amounted in 2021 to 6.18 million tonnes. It was the result of a new deposit documentation – Taczalin 1. The deposit was documented partially on an area separated from the Taczalin deposit which resources were settled in a new documentation with recalculated resources (supplement).
In 2021, any of the vein quartz deposits in Poland was exploited. In 2016, the exploitation from the Taczalin deposit ended, whereas the output from the Stanisław deposit was halted in 2005. After the long-lasting lack of exploitation, in spite of the still valid exploitation concession, the Stanisław deposit was classified as abandoned. The economic resources of this deposit are equal 1.35 million tonnes accounting for 22% of the total anticipated economic resources of vein quartz in Poland.
The figure given below shows changes in domestic resources and production of vein quartz in Poland in the years 1989-2021.
The prospects of the new deposits discovery are limited to the already known places of an occurrence. The most favorable conditions for the resources base enlargement occur in the area of the Stanisław deposit extension, in the tectonic zone of the Rozdroże Izerskie ("Izerskie Crossroad"). Prognostic resources of vein quartz are assessed to be equal 2.87 million tonnes and prospective resources 1.33 million tonnes*.
Prepared by: Agnieszka Malon
* Wołkowicz K., Sroga C., 2020 – ‘Kwarc żyłowy (vein quartz)’. In: ‘Bilans perspektywicznych zasobów kopalin Polski wg stanu na 31.12.2018 r.’ (eds. Szamałek K., Szuflicki M., Mizerski W.): 325-328. PIG-PIB, Warszawa [in Polish].
2020
General information and occurrence
Quartz (SiO2) is, next to feldspar, the most common mineral. It is an important rock-forming mineral, being one of the main components of the majority of granites and other igneous rocks. Under conditions favorable for the crystallization, such as voids in rocks, it forms sharp-pointed hexagonal long and slender crystals which are widely used as a popular ornamental stone and also a gemstone in jewellery. Depending on an admixture of coloring oxides, several varieties of these gemstones are differentiated: clear and colorless rock crystal, yellow to orange citrine, pink to rose pink quartz, purple to violet amethyst, brown to gray smoky quartz and black morion.
Quartz also forms veins and lenses in metamorphic and igneous rocks. The vein quartz deposits originate in the result the of the hydrothermal activity as an infill of open fissures and fractures cutting a given rock massif. The quartz infills are characterized by a high content of silica (SiO2) and a low content of coloring oxides (Fe2O3 and TiO2).
In Poland the vein quartz deposits occur mainly in crystalline rock massifs of the Precambrian and Paleozoic age in the Sudety Mts. (map). The deposits are characterized by a high variability in thickness, a big dip of veins and lenses and a varying quality of raw material.
The vein quartz is widely used in the industry, starting from the ceramic industry (the production and glazing and decorating bone and fine china, porcelain and porcelite, utility and pottery ware ceramics, technical ceramics) to the production of fire-proof materials, enameller and in the metallurgy. Its purest varieties are used in the manufacturing high-quality glass and in the chemical and electrotechnical industries. The quartz vein is also the source of a high-quality quartz powder and fine grade crushed grains (qualities I and III according to industry standard No BN-80-6714-19).
Resources
The Table 1 presents resources and the current state of the exploration and development of vein quartz deposits.
Anticipated economic resources of vein quartz have not changed since 2019 and amounted in 2020 to 5.61 million tonnes.
In 2020, any of the vein quartz deposits in Poland was exploited. In 2016, the exploitation from Taczalin deposit ended, whereas the output from Stanisław deposit was halted in 2005. After the long-lasting lack of exploitation, in spite of the still valid exploitation concession, Stanisław deposit was classified as abandoned. The economic resources of this deposit are equal 1.35 million tonnes accounting for 24% of the total anticipated economic resources of vein quartz in Poland.
The figure given below shows changes in domestic resources and production of vein quartz in Poland in the years 1989-2020.
The prospects of the new deposits discovery are limited to the already known places of an occurrence. The most favorable conditions for the resources base magnification occur in the area of Stanisław deposit extension, in the tectonic zone of Rozdroże Izerskie ("Izerskie Crossroad"). Prognostic resources of vein quartz are assessed to be equal 2.87 million tonnes and prospective resources 1.33 million tonnes*.
Prepared by: Agnieszka Malon
* Wołkowicz K., Sroga C., 2020 – ‘Kwarc żyłowy’ (vein quartz). W: ‘Bilans perspektywicznych zasobów kopalin Polski wg stanu na 31.12.2018 r.’ (red. Szamałek K., Szuflicki M., Mizerski W.): 325-328. PIG-PIB, Warszawa [in Polish].
2019
General information and occurrence
Quartz (SiO2) is, next to feldspar, the most common mineral. It is an important rock-forming mineral, being one of the main components of the majority of granites and other igneous rocks. Under conditions favorable for the crystallization, such as voids in rocks, it forms sharp-pointed hexagonal long and slender crystals which are widely used as a popular ornamental stone and also a gemstone in jewellery. Depending on an admixture of coloring oxides, several varieties of these gemstones are differentiated: clear and colorless rock crystal, yellow to orange citrine, pink to rose pink quartz, purple to violet amethyst, brown to gray smoky quartz and black morion.
Quartz also forms veins and lenses in metamorphic and igneous rocks. The vein quartz deposits originate in the result the of the hydrothermal activity as an infill of open fissures and fractures cutting a given rock massif. The quartz infills are characterized by a high content of silica (SiO2) and a low content of coloring oxides (Fe2O3 and TiO2).
In Poland the vein quartz deposits occur mainly in crystalline rock massifs of the Precambrian and Paleozoic age in the Sudety Mts. (map). The deposits are characterized by a high variability in thickness, a big dip of veins and lenses and a varying quality of raw material.
The vein quartz is widely used in the industry, starting from the ceramic industry (the production and glazing and decorating bone and fine china, porcelain and porcelite, utility and pottery ware ceramics, technical ceramics) to the production of fire-proof materials, enameller and in the metallurgy. Its purest varieties are used in the manufacturing high-quality glass and in the chemical and electrotechnical industries. The quartz vein is also the source of a high-quality quartz powder and fine grade crushed grains (qualities I and III according to industry standard No BN-80-6714-19).
Resources
The Table 1 presents resources and the current state of the exploration and development of vein quartz deposits.
Anticipated economic resources of vein quartz have not changed since 2018 and amounted in 2019 to 5.61 million tonnes.
In 2019, the exploitation concession for Taczalin deposit expired. Currently, there is only 1 deposit with the exploitation concession left – Stanisław deposit with the economic resources equal 1.35 million tonnes which accounts for 24% of the total anticipated economic resources of the vein quartz in Poland.
The exploitation of the vein quartz in Poland was not carried out in 2019 from any of deposits. The output from Taczalin deposit has been on hold since 2016, whereas from Stanisławów deposit it was ended in 2005.
The figure given below shows changes in domestic resources and production of vein quartz in Poland in the years 1989-2019.
The prospects of the new deposits discovery are limited to the already known places of an occurrence. The most favorable conditions for the resources base magnification occur in the area of Stanisław deposit extension, in the tectonic zone of Izerskie Crossroad. Prognostic resources of vein quartz are assessed to be equal 2.87 million tonnes and prospective resources 1.33 million tonnes*.
Prepared by: Agnieszka Malon
* Wołkowicz K., Sroga C., 2020 – ‘Kwarc żyłowy’ (vein quartz). W: ‘Bilans perspektywicznych zasobów kopalin Polski wg stanu na 31.12.2018 r.’ (red. Szamałek K., Szuflicki M., Mizerski W.): 325-328. PIG-PIB, Warszawa.
2018
Quartz (SiO2) is, next to feldspar, the most common mineral. It is an important rock-forming mineral, being one of the main components of the majority of granites and other igneous rocks. Under conditions favorable for the crystallization, such as voids in rocks, it forms sharp-pointed hexagonal long and slender crystals which are widely used as a popular ornamental stone and also a gemstone in jewellery. Depending on an admixture of coloring oxides, several varieties of these gemstones are differentiated: clear and colorless rock crystal, yellow to orange citrine, pink to rose pink quartz, purple to violet amethyst, brown to gray smoky quartz and black morion.
Quartz also forms veins and lenses in metamorphic and igneous rocks. Quartz vein deposits originate in the result the of the hydrothermal activity as an infill of open fissures and fractures cutting a given rock massif. The quartz infills are characterized by a high content of silica (SiO2) and a low content of coloring oxides (Fe2O3 and TiO2).
In Poland quartz veins occur mainly in crystalline rock massifs of the Precambrian and Paleozoic in the Sudety Mts. (map). The deposits are characterized by a high variability in thickness, a big dip of veins and lenses and a varying quality of raw material. The prospects of the new deposits discovery are limited to the already known places of an occurrence. The most favorable conditions for the resources magnification occur in the area of Stanisław deposit extension, in the tectonic zone of Izerskie Crossroad. Prognostic resources of vein quartz are assessed to be equal 2.87 million tonnes and prospective resources 1.33 million tonnes*.
Vein quartz is widely used in the industry, starting from the ceramic industry (the production and glazing and decorating bone and fine china, porcelain and porcelite, utility and pottery ware ceramics, technical ceramics) to the production of fire-proof materials, enameller and in the metallurgy. Its purest varieties are used in the manufacturing high-quality glass and in the chemical and electrotechnical industries. The quartz vein is also the source of a high-quality quartz powder and fine grade crushed grains (qualities I and III according to industry standard No BN-80-6714-19).
The Table 1 presents resources and the current state of the exploration and development of vein quartz deposits.
Anticipated economic resources of vein quartz have not changed since 2017 and amounted to 5.61 million tonnes.
There are two exploited deposits – Stanisław and Taczalin. Economic resources of these deposits are equal 1.72 million tonnes which accounts for 45% of their anticipated economic resources.
The exploitation was not carried out from any of vein quartz deposits in 2018. The output from Taczalin deposit was stopped in 2016 and from Stanisław deposit has been suspended since 2005.
The figure given below shows changes in domestic resources and production of vein quartz in Poland in the years 1989-2018.
Prepared by: Agnieszka Malon
* Wołkowicz K., Sroga C., 2011 – ‘Kwarc żyłowy’. In: ‘Bilans perspektywicznych zasobów kopalin Polski wg stanu na 31 XII 2009 r.’ (ed. S. Wołkowicz, T. Smakowski, S. Speczik): 205-208. PIG-PIB, Warszawa.
2017
Quartz (SiO2) is, next to feldspar, the most common mineral. It is an important rock-forming mineral, being one of the main components of the majority of granites and other igneous rocks. Under conditions favorable for the crystallization, such as voids in rock, it forms sharp-pointed hexagonal long and slender crystals which are widely used as a popular ornamental stone and also a gemstone in jewellery. Depending on an admixture of coloring oxides, several varieties of these gemstones are differentiated: clear and colorless rock crystal, yellow to orange citrine, pink to rose pink quartz, purple to violet amethyst, brown to gray smoky quartz and black morion.
Quartz also forms veins and lenses in metamorphic and igneous rocks. Quartz vein deposits originate in the result of hydrothermal activity as an infill of open fissures and fractures cutting a given rock massif. The quartz infills are characterized by a high content of silica (SiO2) and a low content of coloring oxides (Fe2O3 and TiO2).
In Poland quartz veins occur mainly in crystalline rock massifs of the Precambrian and Paleozoic in the Sudety Mts. (map). The deposits are characterized by a high variability in thickness, big dip of veins and lenses and a varying quality of raw material. The prospects of the new deposits discovery are limited to the already known places of an occurrence. The most favorable conditions for the resources magnification occur in the area of Stanisław deposit extension, in the tectonic zone of Izerskie Crossroad. Prognostic resources of vein quartz are assessed to be equal 2.87 million tonnes and prospective resources 1.33 million tonnes*.
Vein quartz is widely used in the industry, starting from the ceramic industry (the production and glazing and decorating bone and fine china, porcelain and porcelite, utility and pottery ware ceramics, technical ceramics) to the production of fire-proof materials, enameller and in the metallurgy. Its purest varieties are used in manufacturing high-quality glass and in the chemical and electrotechnical industries. The quartz vein is also the source of high-quality quartz powder and fine grade crushed grains (qualities I and III according to industry standard No BN-80-6714-19).
The Table 1 presents resources and the current state of the exploration and development of vein quartz deposits.
Anticipated economic resources of vein quartz have not changed since 2016 and amounted to 5.61 million tonnes.
There are two exploited deposits – Stanisław and Taczalin. Economic resources of these deposits are equal 1.72 million tonnes which accounts for 45% of their anticipated economic resources.
The exploitation was not carried out from any of vein quartz deposits in 2017. The output from Taczalin deposit was stopped in 2016 and from Stanisław deposit has been suspended since 2005.
The figure given below shows changes in domestic resources and production of vein quartz in Poland in the years 1989-2017.
Prepared by: Agnieszka Malon
* Wołkowicz K., Sroga C., 2011 – ‘Kwarc żyłowy’. In: ‘Bilans perspektywicznych zasobów kopalin Polski wg stanu na 31 XII 2009 r.’ (ed. S. Wołkowicz, T. Smakowski, S. Speczik): 205-208. PIG-PIB, Warszawa.
2016
Quartz (SiO2) is, next to feldspar, the most common mineral. It is an important rock-forming mineral, being one of the main components of the majority of granites and other igneous rocks. Under conditions favorable for crystallization, such as voids in rock, it forms sharp-pointed hexagonal long and slender crystals which are widely used as a popular ornamental stone and also a gemstone in jewellery. Depending on admixture of coloring oxides, several varieties of these gemstones are differentiated: clear and colorless rock crystal, yellow to orange citrine, pink to rose pink quartz, purple to violet amethyst, brown to gray smoky quartz and black morion.
Quartz also forms veins and lenses in metamorphic and igneous rocks. Quartz vein deposits originate in the result of hydrothermal activity as an infill of open fissures and fractures cutting a given rock massif. The quartz infills are characterized by a high content of silica (SiO2) and a low content of coloring oxides (Fe2O3 and TiO2).
In Poland quartz veins occur mainly in crystalline rock massifs of the Precambrian and Paleozoic in the Sudety Mts. (map). The deposits are characterized by a high variability in thickness, big dip of veins and lenses and a varying quality of raw material. The most favorable conditions for resources magnification occur in the area of Stanisław deposit extension, in the tectonic zone of Izery Crossroad. Prognostic resources of vein quartz are assessed to be equal 2.87 million tonnes and prospective resources 1.33 million tonnes*.
Vein quartz is widely used in the industry, starting from the ceramic industry (the production and glazing and decorating bone and fine china, porcelain and porcelite, utility and pottery ware ceramics, technical ceramics) to the production of fire-proof materials, enameller and in the metallurgy. Its purest varieties are used in manufacturing high-quality glass and in the chemical and electrotechnical industries. The quartz vein is also the source of high-quality quartz powder and fine grade crushed grains (qualities I and III according to industry standard No BN-80-6714-19).
The table 1 shows resources and the current state of exploration and development of deposits of vein quartz.
Anticipated economic resources of vein quartz have not changed since 2015 and amounted to 5.61 million tonnes. The deposits number declined to six, since there is not Sady (Białe Krowy) deposit included in ‘The balance’ – it was crossed out from the statement in 2015.
There are two exploited deposits – Stanisław and Taczalin. Economic resources of these deposits are equal 1.72 million tonnes which accounts for 45% of their anticipated economic resources.
The exploitation was not carried out from any of vein quartz deposits in 2016. The output from Taczalin deposit was stopped and from Stanisław deposit has been suspended since 2005 (table 2).
The figure given below shows changes in domestic resources and production of tein quartz in Poland in the years 1989-2016.
Prepared by: Agnieszka Malon
* Wołkowicz K., Sroga C., 2011 – ‘Kwarc żyłowy’. In: ‘Bilans perspektywicznych zasobów kopalin Polski wg stanu na 31 XII 2009 r.’ (ed. S. Wołkowicz, T. Smakowski, S. Speczik): 205-208. PIG-PIB, Warszawa.
2015
Quartz (SiO2) is, next to feldspar, the most common mineral. It is an important rock-forming mineral, being one of the main components of the majority of granites and other igneous rocks. Under conditions favorable for crystallization, such as voids in rock, it forms sharp-pointed hexagonal long and slender crystals which are widely used as a popular ornamental stone and also a gemstone in jewellery. Depending on admixture of coloring oxides, several varieties of these gemstones are differentiated: clear and colorless rock crystal, yellow to orange citrine, pink to rose pink quartz, purple to violet amethyst, brown to gray smoky quartz and black morion.
Quartz also forms veins and lenses in metamorphic and igneous rocks. Quartz vein deposits originate in result of hydrothermal activity as an infill of open fissures and fractures cutting a given rock massif. The quartz infills are characterized by high content of silica (SiO2) and low content of coloring oxides (Fe2O3 and TiO2).
In Poland quartz veins occur mainly in crystalline rock massifs of the Precambrian and Paleozoic in the Sudety Mts.(map). The deposits are characterized by a high variability in thickness and quality of raw material as well as in generally high dip of veins and lenses. Prognostic resources of vein quartz are assessed to be equal 2.87 million tonnes and prospective resources 1.33 million tonnes*.
Vein quartz is widely used in the industry, starting from ceramic industry (production and glazing and decorating bone and fine china, porcelain and porcelite, utility and pottery ware ceramics, technical ceramics) to production of fire-proof materials and in metallurgy. Its purest varieties are used in manufacturing high-quality glass and in chemical and electrotechnical industries. Quartz vein is also the source of high-quality quartz powder and fine grade crushed grains.
The table 1 shows resources and the current state of exploration and development of deposits of vein quartz.
Anticipated economic resources of vein quartz amounted to 5.61 million tonnes in 2015 and decreased by 0.95 million tonnes in comparison with 2014, mainly due to the crossing Sady (Białe Krowy) deposit out from ‘The balance…’ (0.94 million tonnes).
There are two exploited deposits – Stanisław and Taczalin. Economic resources of these deposits are equal 1.72 million tonnes which accounts for 45% of their anticipated economic resources.
The exploitation from Taczalin deposit amounted to 4.32 thousand tonnes in 2015 (table 2). Production from Stanisław deposit was suspended in 2005.
Prepared by: Agnieszka Malon
* Wołkowicz K., Sroga C., 2011 – ‘Kwarc żyłowy’. In: ‘Bilans perspektywicznych zasobów kopalin Polski wg stanu na 31 XII 2009 r.’ (ed. S. Wołkowicz, T. Smakowski, S. Speczik): 205-208. PIG-PIB, Warszawa.
2014
Quartz (SiO2) is, next to feldspar, the most common mineral. It is an important rock-forming mineral, being one of the main components of the majority of granites and other igneous rocks. Under conditions favorable for crystallization, such as voids in rock, it forms sharp-pointed hexagonal long and slender crystals which are widely used as a popular ornamental stone and also a gemstone in jewellery. Depending on admixture of coloring oxides, several varieties of these gemstones are differentiated: clear and colorless rock crystal, yellow to orange citrine, pink to rose pink quartz, purple to violet amethyst, brown to gray smoky quartz and black morion.
Quartz also forms veins and lenses in metamorphic and igneous rocks. Quartz vein deposits originate in result of hydrothermal activity as an infill of open fissures and fractures cutting a given rock massif. The quartz infills are characterized by high content of silica (SiO2) and low content of coloring oxides (Fe2O3 and TiO2).
In Poland quartz veins occur mainly in crystalline rock massifs of the Precambrian and Paleozoic in the Sudety Mts.(map). The deposits are characterized by a high variability in thickness and quality of raw material as well as in generally high dip of veins and lenses. Prognostic resources of vein quartz are assessed to be equal 2.87 million tonnes and prospective resources 1.33 million tonnes(1).
Vein quartz is widely used in the industry, starting from ceramic industry (production and glazing and decorating bone and fine china, porcelain and porcelite, utility and pottery ware ceramics, technical ceramics) to production of fire-proof materials and in metallurgy. Its purest varieties are used in manufacturing high-quality glass and in chemical and electrotechnical industries. Quartz vein is also the source of high-quality quartz powder and fine grade crushed grains.
The table 1 given below shows resources and the current state of exploration and development of deposits of vein quartz.
Anticipated economic resources of vein quartz within 7 documented deposits has changed only by 6 thousand tonnes and amounted to 6.56 million tonnes in 2014.
There are two exploited deposits – Stanisław and Taczalin. Economic resources of these deposits are equal 1.72 million tonnes which accounts for 45% of their anticipated economic resources.
The exploitation from Taczalin deposit was started in 2014 and amounted to 5.9 thousand tonnes. Production from Stanisław deposit was suspended in 2005.
Prepared by: Agnieszka Malon
(1) K. Wołkowicz, C. Sroga, 2011 – ‘Kwarc żyłowy’ in ‘Bilans perspektywicznych zasobów kopalin Polski wg stanu na 31 XII 2009 r.’ editors: S. Wołkowicza, T. Smakowskiego, S. Speczika. PIG-PIB Warsaw.
2013
Quartz (SiO2) is, next to feldspar, the most common mineral. It is an important rock-forming mineral, being one of the main components of the majority of granites and other igneous rocks. Under conditions favorable for crystallization, such as voids in rock, it forms sharp-pointed hexagonal long and slender crystals which are widely used as a popular ornamental stone and also a gemstone in jewellery. Depending on admixture of coloring oxides, several varieties of these gemstones are differentiated: clear and colorless rock crystal, yellow to orange citrine, pink to rose pink quartz, purple to violet amethyst, brown to gray smoky quartz and black morion.
Quartz also forms veins and lenses in metamorphic and igneous rocks. Quartz vein deposits originate in result of hydrothermal activity as an infill of open fissures and fractures cutting a given rock massif. The quartz infills are characterized by high content of silica (SiO2) and low content of coloring oxides (Fe2O3 and TiO2).
In Poland quartz veins occur mainly in crystalline rock massifs of the Precambrian and Paleozoic in the Sudety Mts.(map). The deposits are characterized by a high variability in thickness and quality of raw material as well as in generally high dip of veins and lenses. Prognostic resources of vein quartz are assessed to be equal 2.87 million tonnes and prospective resources 1.33 million tonnes(1).
Vein quartz is widely used in the industry, starting from ceramic industry (production and glazing and decorating bone and fine china, porcelain and porcelite, utility and pottery ware ceramics, technical ceramics) to production of fire-proof materials and in metallurgy. Its purest varieties are used in manufacturing high-quality glass and in chemical and electrotechnical industries. Quartz vein is also the source of high-quality quartz powder and fine grade crushed grains.
The table 1 given below shows resources and the current state of exploration and development of deposits of vein quartz.
Anticipated economic resources of vein quartz within 7 documented deposits has not changed and amounted to 6.56 million tonnes in 2013.
There are two exploited deposits – Stanisław and Taczalin. Economic resources of these deposits are equal 1.73 million tonnes which accounts for 32% of their anticipated economic resources.
None of domestic deposits is being currently exploited – production from Stanisław and Taczalin deposits was suspended in 2005.
Prepared by: Agnieszka Malon
(1) K. Wołkowicz, C. Sroga, 2011 – ‘Kwarc żyłowy’ in ‘Bilans perspektywicznych zasobów kopalin Polski wg stanu na 31 XII 2009 r.’ editors: S. Wołkowicza, T. Smakowskiego, S. Speczika. PIG-PIB Warsaw.
2012
Quartz (SiO2) is, next to feldspar, the commonest mineral. It is an important rock-forming mineral, being one of the main components of the majority of granites and other igneous rocks. Under conditions favorable for crystallization, such as voids in rock, it forms sharp-pointed hexagonal long and slender crystals which are widely used as a popular ornamental stone and also a gemstone in jewellery. Depending on admixture of coloring oxides, several varieties of these gemstones are differentiated: clear and colorless rock crystal, yellow to orange citrine, pink to rose red rose and pink quartz, purple to violet amethyst, brown to gray smoky quartz and black morion.
Quartz also forms veins and lenses in metamorphic and igneous rocks. Quartz vein deposits originate in result of hydrothermal activity as an infill of open fissures and fractures cutting a given rock massif. The quartz infills are characterized by high content of silica (SiO2) and low content of coloring oxides (Fe2O3 and TiO2).
In Poland quartz veins occur mainly in crystalline rock massifs of the Precambrian and Paleozoic in the Sudety Mts.(map). The deposits are characterized by a high variability in thickness and quality of raw material as well as in generally high dip of veins and lenses. Prognostic resources of vein quartz are assessed to be equal 2.87 million tonnes and prospective resources 1.33 million tonnes(1).
Vein quartz is widely used in the industry, starting from ceramic industry (production and glazing and decorating bone and fine china, porcelain and porcelite, utility and pottery ware ceramics, technical ceramics) to production of fire-proof materials and in metallurgy. Its purest varieties are used in manufacturing high-quality glass and in chemical and electrotechnical industries. Quartz vein is also the source of high-quality quartz powder and fine grade crushed grains.
The table 1 given below shows resources and the current state of exploration and development of deposits of vein quartz.
Anticipated economic resources of vein quartz within 7 documented deposits has not changed since 2010 and amounted to 6.56 million tonnes in 2012.
There are three exploited deposits – Krasków, Stanisław and Taczalin. Economic resources of these deposits are equal 3.23 million tonnes which accounts for 50% of their anticipated economic resources. None of them is being currently exploited – production from Krasków deposit was suspended in 2007 whereas from Stanisław and Taczalin deposits in 2005.
Prepared by: Agnieszka Malon
(1) K. Wołkowicz, C. Sroga, 2011 – ‘Kwarc żyłowy’ in ‘Bilans perspektywicznych zasobów kopalin Polski wg stanu na 31 XII 2009 r.’ editors: S. Wołkowicza, T. Smakowskiego, S. Speczika. PIG-PIB Warsaw.
2011
Quartz (SiO2) is, next to feldspar, the commonest mineral. It is an important rock-forming mineral, being one of the main components of the majority of granites and other igneous rocks. Under conditions favorable for crystallization, such as voids in rock, it forms sharp-pointed hexagonal long and slender crystals which are widely used as a popular ornamental stone and also a gemstone in jewellery. Depending on admixture of coloring oxides, several varieties of these gemstones are differentiated: clear and colorless rock crystal, yellow to orange citrine, pink to rose red rose and pink quartz, purple to violet amethyst, brown to gray smoky quartz and black morion.
Quartz also forms veins and lenses in metamorphic and igneous rocks. Quartz vein deposits originate in result of hydrothermal activity as an infill of open fissures and fractures cutting a given rock massif. The quartz infills are characterized by high content of silica (SiO2) and low content of coloring oxides (Fe2O3 and TiO2).
In Poland quartz veins occur mainly in crystalline rock massifs of the Precambrian and Paleozoic in the Sudety Mts.(map). The deposits are characterized by a high variability in thickness and quality of raw material as well as in generally high dip of veins and lenses. Prognostic resources of vein quartz are assessed to be equal 2.87 million tonnes and prospective resources 1.33 million tonnes(1).
Vein quartz is widely used in the industry, starting from ceramic industry (production and glazing and decorating bone and fine china, porcelain and porcelite, utility and pottery ware ceramics, technical ceramics) to production of fire-proof materials and in metallurgy. Its purest varieties are used in manufacturing high-quality glass and in chemical and electrotechnical industries. Quartz vein is also the source of high-quality quartz powder and fine grade crushed grains.
The table 1 given below shows resources and the current state of exploration and development of deposits of vein quartz.
The largest anticipated economic resources hitherto discovered are 3.3 million tonnes in the Stanisław deposit situated south-west of Jelenia Góra and 1.5 million tonnes in the Krasków deposit from the vicinities of Świdnica, Sudety Mts. There are chances for discovery of some new deposits as potential resources in that region are estimated at about 4 million tonnes. It should be added that the known minor deposits were found to be characterized by very good quality of quartz raw material.
Three deposits are developed: Krasków, Stanisław and Taczalin. Economic resources of these deposits amounted to 3.23 million tonnes (50% of anticipated economic resources). In the year 2011, any of these deposits has not been exploited.
Prepared by: Agnieszka Malon
(1) K. Wołkowicz, C. Sroga, 2011 – ‘Kwarc żyłowy’ w ‘Bilans perspektywicznych zasobów kopalin Polski wg stanu na 31 XII 2009 r.’ editors: S. Wołkowicza, T. Smakowskiego, S. Speczika. PIG-PIB Warsaw.
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