Rsi Stone World Private Limited Arera Colony, Bhopal, Madhya Pradesh

We are offering mint sandstone. sand stone is a classic sedimentary rock composed mainly of sand-sized minerals, bonded or cemented grains that might be either fragments of existing rock, or minerals. Typically, these grains are calcite, clays and silica. sandstone is usually formed by sedimentation that occurs as a result of a fluid, such as a river or a lake, in environments where sand accumulates such as sandy beaches, floodplains and deltas. Geologists gather information from sandstone samples to determine the geologic history of a particular region. Fossils are commonly found in sandstone, making it useful for paleontologists as well. sandstone has been popular and used for domestic construction and house wares since prehistoric times and continues to be used. it is relatively soft, making it easy to carve. It has been widely used around the world in constructing temples, cathedrals, homes, and other buildings. It has also been used for artistic purposes to create ornamental fountains and statues. sandstone is composed of different chemicals and rock fragments, and it is typically categorized as three main types. arkosic sandstone that contains more than 25 percent feldspar grains is called arkosic sandstone. The composition of this type of sandstone is similar to granite. Arkosic sandstone's high feldspar composition indicates that it has spent a short time in its depositional basin (place where sediments accumulate) because feldspar typically weathers rapidly, turning to clay if it sits long enough. quartzose quartzose sandstones typically have a quartz content of greater than 90 percent. This type of sandstone is also called beach sand or quartzite, and its high quartz composition suggests that the rock has spent a long period of time in its depositional basin. Typically, this type of sandstone is white, but it may be a variety of colors such as red, depending on the conditions in which it forms. Quartzose sandstone is marked with ripples, and is commonly found in central north america and australia. argillaceous argillaceous sandstone, also called wacke or greywacke, has a considerable amount of clay or silt content. It has a smoother texture in comparison to quartzose or arkosic sandstone. Almost all of this type of sandstone is formed in the sea and is dark in color with a mixture of rock fragments, feldspar and quartz along with large amounts of mud (15 to 40 percent). This type of sandstone is typically found in areas where rapid erosion occurs and where the climate is temperate or arid.

Brand Name : RSIWS

We are offering yellow limestone. limestone is a sedimentary rock, made up mostly of the mineral calcite, a form of calcium carbonate, caco3. The calcium carbonate is originally produced by living animals (such as shellfish). Later, much of it goes into solution in sea water, and then is deposited as limestone. Calcium carbonate gets precipitated when the physical condition of the water changes. For example, if the concentration of caco3 is high, then a temperature drop, or a ph (acidity) change, can cause precipitation. limestone refers to sedimentary rocks that contain a minimum of 50 percent of calcium carbonate in their composition. Minor components include clay, iron, feldspar, and quartz. Limestone is formed by the deposition of calcium carbonate suspended in the water or by the accumulation of shells and other fossilized materials. Limestone rock types include chalk, coquina, travertine, tufa, as well as oolitic and lithographic limestone. chalk and coquina chalk and coquina are two fossiliferous limestones, which can contain fossils. Chalk is soft, white to light gray in color and has a extremely fine texture. The remains of the calcareous shells of prehistorical and microscopic marine organisms formed this type of limestone rock. The white cliffs of dover, in england, are an example of chalk. On the other hand, coquina has a rough texture, because it is the results of the cementing of debris of broken shells and corals. The anastasia geologic formation, in florida, is an example of coquina that was formed more 10,000 years ago. oolitic limestone this type of limestone rock consists of small spheres. When primitive oceans were saturated with calcium carbonate, the mineral's small particles started to aggregate around grains of sand, forming the oolitic limestone. Florida's lower keys contain oolitic limestone. In britain, the cotswold area is famous for its old houses built with yellow oolitic limestone, which was formed 150 million years ago. travertine and tufa travertine is a white to yellow limestone often found in caves or near water sources. It is formed when the calcium carbonate dissolved in the water accumulates over time on rock surfaces, producing cave formations such as stalactites. In the u.s., travertine formations are found in several locations, including the mitchell caverns, at the mojave national preserve, california. Plitvice lakes national park, in croatia, is an example of travertine formation associated to waterfalls. Similar to travertine, tufa is a type of limestone often linked to hot water springs. lithographic limestone lithographic limestone was formed about 150 million of years ago, during the jurassic period. It is a dense and fine-grain type of rock, which became important in the late 1700s with the advent of a printing process called lithography. Artists drew images on the stone using a special oily ink, and pressed onto sheets of paper. One single drawing could generate many paper copies. The first lithographic limestone was found in southern germany.

Brand Name : RSIT

We are offering rsit brown sandstone. sand stone is a classic sedimentary rock composed mainly of sand-sized minerals, bonded or cemented grains that might be either fragments of existing rock, or minerals. Typically, these grains are calcite, clays and silica. sandstone is usually formed by sedimentation that occurs as a result of a fluid, such as a river or a lake, in environments where sand accumulates such as sandy beaches, floodplains and deltas. Geologists gather information from sandstone samples to determine the geologic history of a particular region. Fossils are commonly found in sandstone, making it useful for paleontologists as well. sandstone has been popular and used for domestic construction and house wares since prehistoric times and continues to be used. it is relatively soft, making it easy to carve. It has been widely used around the world in constructing temples, cathedrals, homes, and other buildings. It has also been used for artistic purposes to create ornamental fountains and statues. sandstone is composed of different chemicals and rock fragments, and it is typically categorized as three main types. arkosic sandstone that contains more than 25 percent feldspar grains is called arkosic sandstone. The composition of this type of sandstone is similar to granite. Arkosic sandstone's high feldspar composition indicates that it has spent a short time in its depositional basin (place where sediments accumulate) because feldspar typically weathers rapidly, turning to clay if it sits long enough. quartzose quartzose sandstones typically have a quartz content of greater than 90 percent. This type of sandstone is also called beach sand or quartzite, and its high quartz composition suggests that the rock has spent a long period of time in its depositional basin. Typically, this type of sandstone is white, but it may be a variety of colors such as red, depending on the conditions in which it forms. Quartzose sandstone is marked with ripples, and is commonly found in central north america and australia. argillaceous argillaceous sandstone, also called wacke or greywacke, has a considerable amount of clay or silt content. It has a smoother texture in comparison to quartzose or arkosic sandstone. Almost all of this type of sandstone is formed in the sea and is dark in color with a mixture of rock fragments, feldspar and quartz along with large amounts of mud (15 to 40 percent). This type of sandstone is typically found in areas where rapid erosion occurs and where the climate is temperate or arid.

We are offering black sandstone. sand stone is a classic sedimentary rock composed mainly of sand-sized minerals, bonded or cemented grains that might be either fragments of existing rock, or minerals. Typically, these grains are calcite, clays and silica. sandstone is usually formed by sedimentation that occurs as a result of a fluid, such as a river or a lake, in environments where sand accumulates such as sandy beaches, floodplains and deltas. Geologists gather information from sandstone samples to determine the geologic history of a particular region. Fossils are commonly found in sandstone, making it useful for paleontologists as well. sandstone has been popular and used for domestic construction and house wares since prehistoric times and continues to be used. it is relatively soft, making it easy to carve. It has been widely used around the world in constructing temples, cathedrals, homes, and other buildings. It has also been used for artistic purposes to create ornamental fountains and statues. sandstone is composed of different chemicals and rock fragments, and it is typically categorized as three main types. arkosic sandstone that contains more than 25 percent feldspar grains is called arkosic sandstone. The composition of this type of sandstone is similar to granite. Arkosic sandstone's high feldspar composition indicates that it has spent a short time in its depositional basin (place where sediments accumulate) because feldspar typically weathers rapidly, turning to clay if it sits long enough. quartzose quartzose sandstones typically have a quartz content of greater than 90 percent. This type of sandstone is also called beach sand or quartzite, and its high quartz composition suggests that the rock has spent a long period of time in its depositional basin. Typically, this type of sandstone is white, but it may be a variety of colors such as red, depending on the conditions in which it forms. Quartzose sandstone is marked with ripples, and is commonly found in central north america and australia. argillaceous argillaceous sandstone, also called wacke or greywacke, has a considerable amount of clay or silt content. It has a smoother texture in comparison to quartzose or arkosic sandstone. Almost all of this type of sandstone is formed in the sea and is dark in color with a mixture of rock fragments, feldspar and quartz along with large amounts of mud (15 to 40 percent). This type of sandstone is typically found in areas where rapid erosion occurs and where the climate is temperate or arid.

We are offering dark green sandstone. sand stone is a classic sedimentary rock composed mainly of sand-sized minerals, bonded or cemented grains that might be either fragments of existing rock, or minerals. Typically, these grains are calcite, clays and silica. sandstone is usually formed by sedimentation that occurs as a result of a fluid, such as a river or a lake, in environments where sand accumulates such as sandy beaches, floodplains and deltas. Geologists gather information from sandstone samples to determine the geologic history of a particular region. Fossils are commonly found in sandstone, making it useful for paleontologists as well. sandstone has been popular and used for domestic construction and house wares since prehistoric times and continues to be used. it is relatively soft, making it easy to carve. It has been widely used around the world in constructing temples, cathedrals, homes, and other buildings. It has also been used for artistic purposes to create ornamental fountains and statues. sandstone is composed of different chemicals and rock fragments, and it is typically categorized as three main types. arkosic sandstone that contains more than 25 percent feldspar grains is called arkosic sandstone. The composition of this type of sandstone is similar to granite. Arkosic sandstone's high feldspar composition indicates that it has spent a short time in its depositional basin (place where sediments accumulate) because feldspar typically weathers rapidly, turning to clay if it sits long enough. quartzose quartzose sandstones typically have a quartz content of greater than 90 percent. This type of sandstone is also called beach sand or quartzite, and its high quartz composition suggests that the rock has spent a long period of time in its depositional basin. Typically, this type of sandstone is white, but it may be a variety of colors such as red, depending on the conditions in which it forms. Quartzose sandstone is marked with ripples, and is commonly found in central north america and australia. argillaceous argillaceous sandstone, also called wacke or greywacke, has a considerable amount of clay or silt content. It has a smoother texture in comparison to quartzose or arkosic sandstone. Almost all of this type of sandstone is formed in the sea and is dark in color with a mixture of rock fragments, feldspar and quartz along with large amounts of mud (15 to 40 percent). This type of sandstone is typically found in areas where rapid erosion occurs and where the climate is temperate or arid.

We are offering mint sandstone. sand stone is a classic sedimentary rock composed mainly of sand-sized minerals, bonded or cemented grains that might be either fragments of existing rock, or minerals. Typically, these grains are calcite, clays and silica. sandstone is usually formed by sedimentation that occurs as a result of a fluid, such as a river or a lake, in environments where sand accumulates such as sandy beaches, floodplains and deltas. Geologists gather information from sandstone samples to determine the geologic history of a particular region. Fossils are commonly found in sandstone, making it useful for paleontologists as well. sandstone has been popular and used for domestic construction and house wares since prehistoric times and continues to be used. it is relatively soft, making it easy to carve. It has been widely used around the world in constructing temples, cathedrals, homes, and other buildings. It has also been used for artistic purposes to create ornamental fountains and statues. sandstone is composed of different chemicals and rock fragments, and it is typically categorized as three main types. arkosic sandstone that contains more than 25 percent feldspar grains is called arkosic sandstone. The composition of this type of sandstone is similar to granite. Arkosic sandstone's high feldspar composition indicates that it has spent a short time in its depositional basin (place where sediments accumulate) because feldspar typically weathers rapidly, turning to clay if it sits long enough. quartzose quartzose sandstones typically have a quartz content of greater than 90 percent. This type of sandstone is also called beach sand or quartzite, and its high quartz composition suggests that the rock has spent a long period of time in its depositional basin. Typically, this type of sandstone is white, but it may be a variety of colors such as red, depending on the conditions in which it forms. Quartzose sandstone is marked with ripples, and is commonly found in central north america and australia. argillaceous argillaceous sandstone, also called wacke or greywacke, has a considerable amount of clay or silt content. It has a smoother texture in comparison to quartzose or arkosic sandstone. Almost all of this type of sandstone is formed in the sea and is dark in color with a mixture of rock fragments, feldspar and quartz along with large amounts of mud (15 to 40 percent). This type of sandstone is typically found in areas where rapid erosion occurs and where the climate is temperate or arid.

Brand Name : RSIPS

We are offering mint sandstone. sand stone is a classic sedimentary rock composed mainly of sand-sized minerals, bonded or cemented grains that might be either fragments of existing rock, or minerals. Typically, these grains are calcite, clays and silica. sandstone is usually formed by sedimentation that occurs as a result of a fluid, such as a river or a lake, in environments where sand accumulates such as sandy beaches, floodplains and deltas. Geologists gather information from sandstone samples to determine the geologic history of a particular region. Fossils are commonly found in sandstone, making it useful for paleontologists as well. sandstone has been popular and used for domestic construction and house wares since prehistoric times and continues to be used. it is relatively soft, making it easy to carve. It has been widely used around the world in constructing temples, cathedrals, homes, and other buildings. It has also been used for artistic purposes to create ornamental fountains and statues. sandstone is composed of different chemicals and rock fragments, and it is typically categorized as three main types. arkosic sandstone that contains more than 25 percent feldspar grains is called arkosic sandstone. The composition of this type of sandstone is similar to granite. Arkosic sandstone's high feldspar composition indicates that it has spent a short time in its depositional basin (place where sediments accumulate) because feldspar typically weathers rapidly, turning to clay if it sits long enough. quartzose quartzose sandstones typically have a quartz content of greater than 90 percent. This type of sandstone is also called beach sand or quartzite, and its high quartz composition suggests that the rock has spent a long period of time in its depositional basin. Typically, this type of sandstone is white, but it may be a variety of colors such as red, depending on the conditions in which it forms. Quartzose sandstone is marked with ripples, and is commonly found in central north america and australia. argillaceous argillaceous sandstone, also called wacke or greywacke, has a considerable amount of clay or silt content. It has a smoother texture in comparison to quartzose or arkosic sandstone. Almost all of this type of sandstone is formed in the sea and is dark in color with a mixture of rock fragments, feldspar and quartz along with large amounts of mud (15 to 40 percent). This type of sandstone is typically found in areas where rapid erosion occurs and where the climate is temperate or arid.

Brand Name : RSIMS

We are offering pink sandstone. sand stone is a classic sedimentary rock composed mainly of sand-sized minerals, bonded or cemented grains that might be either fragments of existing rock, or minerals. Typically, these grains are calcite, clays and silica. sandstone is usually formed by sedimentation that occurs as a result of a fluid, such as a river or a lake, in environments where sand accumulates such as sandy beaches, floodplains and deltas. Geologists gather information from sandstone samples to determine the geologic history of a particular region. Fossils are commonly found in sandstone, making it useful for paleontologists as well. sandstone has been popular and used for domestic construction and house wares since prehistoric times and continues to be used. it is relatively soft, making it easy to carve. It has been widely used around the world in constructing temples, cathedrals, homes, and other buildings. It has also been used for artistic purposes to create ornamental fountains and statues. sandstone is composed of different chemicals and rock fragments, and it is typically categorized as three main types. arkosic sandstone that contains more than 25 percent feldspar grains is called arkosic sandstone. The composition of this type of sandstone is similar to granite. Arkosic sandstone's high feldspar composition indicates that it has spent a short time in its depositional basin (place where sediments accumulate) because feldspar typically weathers rapidly, turning to clay if it sits long enough. quartzose quartzose sandstones typically have a quartz content of greater than 90 percent. This type of sandstone is also called beach sand or quartzite, and its high quartz composition suggests that the rock has spent a long period of time in its depositional basin. Typically, this type of sandstone is white, but it may be a variety of colors such as red, depending on the conditions in which it forms. Quartzose sandstone is marked with ripples, and is commonly found in central north america and australia. argillaceous argillaceous sandstone, also called wacke or greywacke, has a considerable amount of clay or silt content. It has a smoother texture in comparison to quartzose or arkosic sandstone. Almost all of this type of sandstone is formed in the sea and is dark in color with a mixture of rock fragments, feldspar and quartz along with large amounts of mud (15 to 40 percent). This type of sandstone is typically found in areas where rapid erosion occurs and where the climate is temperate or arid.

Brand Name : RSIMB

We are offering mint sandstone. sand stone is a classic sedimentary rock composed mainly of sand-sized minerals, bonded or cemented grains that might be either fragments of existing rock, or minerals. Typically, these grains are calcite, clays and silica. sandstone is usually formed by sedimentation that occurs as a result of a fluid, such as a river or a lake, in environments where sand accumulates such as sandy beaches, floodplains and deltas. Geologists gather information from sandstone samples to determine the geologic history of a particular region. Fossils are commonly found in sandstone, making it useful for paleontologists as well. sandstone has been popular and used for domestic construction and house wares since prehistoric times and continues to be used. it is relatively soft, making it easy to carve. It has been widely used around the world in constructing temples, cathedrals, homes, and other buildings. It has also been used for artistic purposes to create ornamental fountains and statues. sandstone is composed of different chemicals and rock fragments, and it is typically categorized as three main types. arkosic sandstone that contains more than 25 percent feldspar grains is called arkosic sandstone. The composition of this type of sandstone is similar to granite. Arkosic sandstone's high feldspar composition indicates that it has spent a short time in its depositional basin (place where sediments accumulate) because feldspar typically weathers rapidly, turning to clay if it sits long enough. quartzose quartzose sandstones typically have a quartz content of greater than 90 percent. This type of sandstone is also called beach sand or quartzite, and its high quartz composition suggests that the rock has spent a long period of time in its depositional basin. Typically, this type of sandstone is white, but it may be a variety of colors such as red, depending on the conditions in which it forms. Quartzose sandstone is marked with ripples, and is commonly found in central north america and australia. argillaceous argillaceous sandstone, also called wacke or greywacke, has a considerable amount of clay or silt content. It has a smoother texture in comparison to quartzose or arkosic sandstone. Almost all of this type of sandstone is formed in the sea and is dark in color with a mixture of rock fragments, feldspar and quartz along with large amounts of mud (15 to 40 percent). This type of sandstone is typically found in areas where rapid erosion occurs and where the climate is temperate or arid.

Brand Name : RSILS

We are offering rsil yellow sandstone. sand stone is a classic sedimentary rock composed mainly of sand-sized minerals, bonded or cemented grains that might be either fragments of existing rock, or minerals. Typically, these grains are calcite, clays and silica. sandstone is usually formed by sedimentation that occurs as a result of a fluid, such as a river or a lake, in environments where sand accumulates such as sandy beaches, floodplains and deltas. Geologists gather information from sandstone samples to determine the geologic history of a particular region. Fossils are commonly found in sandstone, making it useful for paleontologists as well. sandstone has been popular and used for domestic construction and house wares since prehistoric times and continues to be used. it is relatively soft, making it easy to carve. It has been widely used around the world in constructing temples, cathedrals, homes, and other buildings. It has also been used for artistic purposes to create ornamental fountains and statues. sandstone is composed of different chemicals and rock fragments, and it is typically categorized as three main types. arkosic sandstone that contains more than 25 percent feldspar grains is called arkosic sandstone. The composition of this type of sandstone is similar to granite. Arkosic sandstone's high feldspar composition indicates that it has spent a short time in its depositional basin (place where sediments accumulate) because feldspar typically weathers rapidly, turning to clay if it sits long enough. quartzose quartzose sandstones typically have a quartz content of greater than 90 percent. This type of sandstone is also called beach sand or quartzite, and its high quartz composition suggests that the rock has spent a long period of time in its depositional basin. Typically, this type of sandstone is white, but it may be a variety of colors such as red, depending on the conditions in which it forms. Quartzose sandstone is marked with ripples, and is commonly found in central north america and australia. argillaceous argillaceous sandstone, also called wacke or greywacke, has a considerable amount of clay or silt content. It has a smoother texture in comparison to quartzose or arkosic sandstone. Almost all of this type of sandstone is formed in the sea and is dark in color with a mixture of rock fragments, feldspar and quartz along with large amounts of mud (15 to 40 percent). This type of sandstone is typically found in areas where rapid erosion occurs and where the climate is temperate or arid.

We are offering rail black slate stone. slate stones have various levels of porosity, hardness and compressive strength. They are best suited for exterior and interior applications. Slate renders a graceful, natural finish to any building and is more cost effective than other wall and floor coverings. All natural slate stones are fireproof and non-slippery. It is used in architecture, flooring, wall cladding and roofing etc. The usual colors of slate are black, dark grey, greenish grey, copper and purplish grey. a great combination of earth tone colors and the finish makes this stone one of its kinds. The vibrant colors and unique texture makes slates appropriate for interior as well as exterior applications. Slate is formed of compressed layers of sediments formed under ocean. slate is a regionally metamorphosis, argillaceous rock, that has developed but has suffered re-crystallization, and compressed into a dense stone made up of quartz, iolite, mica and calcite. Because it is formed in layers, it can easily be split to expose beautifully textured surfaces. The usual colors of slates are earthy (various shades and mixes of browns, beiges, yellows), black, dark-grays, and greenish-gray but shades of pinks, purples and copper are also found. They usually exhibit lot of variations amongst the pieces quarried from the same pit. Slates, depending on their individual hardness, are used for flooring, cladding and landscaping.

We are offering black limestone. limestone is a sedimentary rock, made up mostly of the mineral calcite, a form of calcium carbonate, caco3. The calcium carbonate is originally produced by living animals (such as shellfish). Later, much of it goes into solution in sea water, and then is deposited as limestone. Calcium carbonate gets precipitated when the physical condition of the water changes. For example, if the concentration of caco3 is high, then a temperature drop, or a ph (acidity) change, can cause precipitation. limestone refers to sedimentary rocks that contain a minimum of 50 percent of calcium carbonate in their composition. Minor components include clay, iron, feldspar, and quartz. Limestone is formed by the deposition of calcium carbonate suspended in the water or by the accumulation of shells and other fossilized materials. Limestone rock types include chalk, coquina, travertine, tufa, as well as oolitic and lithographic limestone. chalk and coquina chalk and coquina are two fossiliferous limestones, which can contain fossils. Chalk is soft, white to light gray in color and has a extremely fine texture. The remains of the calcareous shells of prehistorical and microscopic marine organisms formed this type of limestone rock. The white cliffs of dover, in england, are an example of chalk. On the other hand, coquina has a rough texture, because it is the results of the cementing of debris of broken shells and corals. The anastasia geologic formation, in florida, is an example of coquina that was formed more 10,000 years ago. oolitic limestone this type of limestone rock consists of small spheres. When primitive oceans were saturated with calcium carbonate, the mineral's small particles started to aggregate around grains of sand, forming the oolitic limestone. Florida's lower keys contain oolitic limestone. In britain, the cotswold area is famous for its old houses built with yellow oolitic limestone, which was formed 150 million years ago. travertine and tufa travertine is a white to yellow limestone often found in caves or near water sources. It is formed when the calcium carbonate dissolved in the water accumulates over time on rock surfaces, producing cave formations such as stalactites. In the u.s., travertine formations are found in several locations, including the mitchell caverns, at the mojave national preserve, california. Plitvice lakes national park, in croatia, is an example of travertine formation associated to waterfalls. Similar to travertine, tufa is a type of limestone often linked to hot water springs. lithographic limestone lithographic limestone was formed about 150 million of years ago, during the jurassic period. It is a dense and fine-grain type of rock, which became important in the late 1700s with the advent of a printing process called lithography. Artists drew images on the stone using a special oily ink, and pressed onto sheets of paper. One single drawing could generate many paper copies. The first lithographic limestone was found in southern germany.

Brand Name : RSIKK

We are offering multi color slate stone. slate stones have various levels of porosity, hardness and compressive strength. They are best suited for exterior and interior applications. Slate renders a graceful, natural finish to any building and is more cost effective than other wall and floor coverings. All natural slate stones are fireproof and non-slippery. It is used in architecture, flooring, wall cladding and roofing etc. The usual colors of slate are black, dark grey, greenish grey, copper and purplish grey. a great combination of earth tone colors and the finish makes this stone one of its kinds. The vibrant colors and unique texture makes slates appropriate for interior as well as exterior applications. Slate is formed of compressed layers of sediments formed under ocean. slate is a regionally metamorphosis, argillaceous rock, that has developed but has suffered re-crystallization, and compressed into a dense stone made up of quartz, iolite, mica and calcite. Because it is formed in layers, it can easily be split to expose beautifully textured surfaces. The usual colors of slates are earthy (various shades and mixes of browns, beiges, yellows), black, dark-grays, and greenish-gray but shades of pinks, purples and copper are also found. They usually exhibit lot of variations amongst the pieces quarried from the same pit. Slates, depending on their individual hardness, are used for flooring, cladding and landscaping.

We are offering grey sandstone. Sand stone is a classic sedimentary rock composed mainly of sand-sized minerals, bonded or cemented grains that might be either fragments of existing rock, or minerals. Typically, these grains are calcite, clays and silica. Sandstone is usually formed by sedimentation that occurs as a result of a fluid, such as a river or a lake, in environments where sand accumulates such as sandy beaches, floodplains and deltas. Geologists gather information from sandstone samples to determine the geologic history of a particular region. Fossils are commonly found in sandstone, making it useful for paleontologists as well. Sandstone has been popular and used for domestic construction and house wares since prehistoric times and continues to be used. It is relatively soft, making it easy to carve. It has been widely used around the world in constructing temples, cathedrals, homes, and other buildings. It has also been used for artistic purposes to create ornamental fountains and statues. Sandstone is composed of different chemicals and rock fragments, and it is typically categorized as three main types. arkosic sandstone that contains more than 25 percent feldspar grains is called arkosic sandstone. The composition of this type of sandstone is similar to granite. Arkosic sandstone's high feldspar composition indicates that it has spent a short time in its depositional basin (place where sediments accumulate) because feldspar typically weathers rapidly, turning to clay if it sits long enough. Quartzose quartzose sandstones typically have a quartz content of greater than 90 percent. This type of sandstone is also called beach sand or quartzite, and its high quartz composition suggests that the rock has spent a long period of time in its depositional basin. Typically, this type of sandstone is white, but it may be a variety of colors such as red, depending on the conditions in which it forms. Quartzose sandstone is marked with ripples, and is commonly found in central north america and australia. Argillaceous argillaceous sandstone, also called wacke or greywacke, has a considerable amount of clay or silt content. It has a smoother texture in comparison to quartzose or arkosic sandstone. Almost all of this type of sandstone is formed in the sea and is dark in color with a mixture of rock fragments, feldspar and quartz along with large amounts of mud (15 to 40 percent). This type of sandstone is typically found in areas where rapid erosion occurs and where the climate is temperate or arid.

We are offering brown limestone. limestone is a sedimentary rock, made up mostly of the mineral calcite, a form of calcium carbonate, caco3. The calcium carbonate is originally produced by living animals (such as shellfish). Later, much of it goes into solution in sea water, and then is deposited as limestone. Calcium carbonate gets precipitated when the physical condition of the water changes. For example, if the concentration of caco3 is high, then a temperature drop, or a ph (acidity) change, can cause precipitation. limestone refers to sedimentary rocks that contain a minimum of 50 percent of calcium carbonate in their composition. Minor components include clay, iron, feldspar, and quartz. Limestone is formed by the deposition of calcium carbonate suspended in the water or by the accumulation of shells and other fossilized materials. Limestone rock types include chalk, coquina, travertine, tufa, as well as oolitic and lithographic limestone. chalk and coquina chalk and coquina are two fossiliferous limestones, which can contain fossils. Chalk is soft, white to light gray in color and has a extremely fine texture. The remains of the calcareous shells of prehistorical and microscopic marine organisms formed this type of limestone rock. The white cliffs of dover, in england, are an example of chalk. On the other hand, coquina has a rough texture, because it is the results of the cementing of debris of broken shells and corals. The anastasia geologic formation, in florida, is an example of coquina that was formed more 10,000 years ago. oolitic limestone this type of limestone rock consists of small spheres. When primitive oceans were saturated with calcium carbonate, the mineral's small particles started to aggregate around grains of sand, forming the oolitic limestone. Florida's lower keys contain oolitic limestone. In britain, the cotswold area is famous for its old houses built with yellow oolitic limestone, which was formed 150 million years ago. travertine and tufa travertine is a white to yellow limestone often found in caves or near water sources. It is formed when the calcium carbonate dissolved in the water accumulates over time on rock surfaces, producing cave formations such as stalactites. In the u.s., travertine formations are found in several locations, including the mitchell caverns, at the mojave national preserve, california. Plitvice lakes national park, in croatia, is an example of travertine formation associated to waterfalls. Similar to travertine, tufa is a type of limestone often linked to hot water springs. lithographic limestone lithographic limestone was formed about 150 million of years ago, during the jurassic period. It is a dense and fine-grain type of rock, which became important in the late 1700s with the advent of a printing process called lithography. Artists drew images on the stone using a special oily ink, and pressed onto sheets of paper. One single drawing could generate many paper copies. The first lithographic limestone was found in southern germany.

We are offering blue limestone limestone is a sedimentary rock, made up mostly of the mineral calcite, a form of calcium carbonate, caco3. The calcium carbonate is originally produced by living animals (such as shellfish). Later, much of it goes into solution in sea water, and then is deposited as limestone. Calcium carbonate gets precipitated when the physical condition of the water changes. For example, if the concentration of caco3 is high, then a temperature drop, or a ph (acidity) change, can cause precipitation. limestone refers to sedimentary rocks that contain a minimum of 50 percent of calcium carbonate in their composition. Minor components include clay, iron, feldspar, and quartz. Limestone is formed by the deposition of calcium carbonate suspended in the water or by the accumulation of shells and other fossilized materials. Limestone rock types include chalk, coquina, travertine, tufa, as well as oolitic and lithographic limestone. chalk and coquina chalk and coquina are two fossiliferous limestones, which can contain fossils. Chalk is soft, white to light gray in color and has a extremely fine texture. The remains of the calcareous shells of prehistorical and microscopic marine organisms formed this type of limestone rock. The white cliffs of dover, in england, are an example of chalk. On the other hand, coquina has a rough texture, because it is the results of the cementing of debris of broken shells and corals. The anastasia geologic formation, in florida, is an example of coquina that was formed more 10,000 years ago. oolitic limestone this type of limestone rock consists of small spheres. When primitive oceans were saturated with calcium carbonate, the mineral's small particles started to aggregate around grains of sand, forming the oolitic limestone. Florida's lower keys contain oolitic limestone. In britain, the cotswold area is famous for its old houses built with yellow oolitic limestone, which was formed 150 million years ago. travertine and tufa travertine is a white to yellow limestone often found in caves or near water sources. It is formed when the calcium carbonate dissolved in the water accumulates over time on rock surfaces, producing cave formations such as stalactites. In the u.s., travertine formations are found in several locations, including the mitchell caverns, at the mojave national preserve, california. Plitvice lakes national park, in croatia, is an example of travertine formation associated to waterfalls. Similar to travertine, tufa is a type of limestone often linked to hot water springs. lithographic limestone lithographic limestone was formed about 150 million of years ago, during the jurassic period. It is a dense and fine-grain type of rock, which became important in the late 1700s with the advent of a printing process called lithography. Artists drew images on the stone using a special oily ink, and pressed onto sheets of paper. One single drawing could generate many paper copies. The first lithographic limestone was found in southern germany.

We are offering yellow sandstone. sand stone is a classic sedimentary rock composed mainly of sand-sized minerals, bonded or cemented grains that might be either fragments of existing rock, or minerals. Typically, these grains are calcite, clays and silica. sandstone is usually formed by sedimentation that occurs as a result of a fluid, such as a river or a lake, in environments where sand accumulates such as sandy beaches, floodplains and deltas. Geologists gather information from sandstone samples to determine the geologic history of a particular region. Fossils are commonly found in sandstone, making it useful for paleontologists as well. sandstone has been popular and used for domestic construction and house wares since prehistoric times and continues to be used. it is relatively soft, making it easy to carve. It has been widely used around the world in constructing temples, cathedrals, homes, and other buildings. It has also been used for artistic purposes to create ornamental fountains and statues. sandstone is composed of different chemicals and rock fragments, and it is typically categorized as three main types. arkosic sandstone that contains more than 25 percent feldspar grains is called arkosic sandstone. The composition of this type of sandstone is similar to granite. Arkosic sandstone's high feldspar composition indicates that it has spent a short time in its depositional basin (place where sediments accumulate) because feldspar typically weathers rapidly, turning to clay if it sits long enough. quartzose quartzose sandstones typically have a quartz content of greater than 90 percent. This type of sandstone is also called beach sand or quartzite, and its high quartz composition suggests that the rock has spent a long period of time in its depositional basin. Typically, this type of sandstone is white, but it may be a variety of colors such as red, depending on the conditions in which it forms. Quartzose sandstone is marked with ripples, and is commonly found in central north america and australia. argillaceous argillaceous sandstone, also called wacke or greywacke, has a considerable amount of clay or silt content. It has a smoother texture in comparison to quartzose or arkosic sandstone. Almost all of this type of sandstone is formed in the sea and is dark in color with a mixture of rock fragments, feldspar and quartz along with large amounts of mud (15 to 40 percent). This type of sandstone is typically found in areas where rapid erosion occurs and where the climate is temperate or arid.

We are offering black slate stone. slate stones have various levels of porosity, hardness and compressive strength. They are best suited for exterior and interior applications. Slate renders a graceful, natural finish to any building and is more cost effective than other wall and floor coverings. All natural slate stones are fireproof and non-slippery. It is used in architecture, flooring, wall cladding and roofing etc. The usual colors of slate are black, dark grey, greenish grey, copper and purplish grey. a great combination of earth tone colors and the finish makes this stone one of its kinds. The vibrant colors and unique texture makes slates appropriate for interior as well as exterior applications. Slate is formed of compressed layers of sediments formed under ocean. slate is a regionally metamorphosis, argillaceous rock, that has developed but has suffered re-crystallization, and compressed into a dense stone made up of quartz, iolite, mica and calcite. Because it is formed in layers, it can easily be split to expose beautifully textured surfaces. The usual colors of slates are earthy (various shades and mixes of browns, beiges, yellows), black, dark-grays, and greenish-gray but shades of pinks, purples and copper are also found. They usually exhibit lot of variations amongst the pieces quarried from the same pit. Slates, depending on their individual hardness, are used for flooring, cladding and landscaping.

Brand Name : RSIJ

We are offering rsig yellow sandstone. sand stone is a classic sedimentary rock composed mainly of sand-sized minerals, bonded or cemented grains that might be either fragments of existing rock, or minerals. Typically, these grains are calcite, clays and silica. sandstone is usually formed by sedimentation that occurs as a result of a fluid, such as a river or a lake, in environments where sand accumulates such as sandy beaches, floodplains and deltas. Geologists gather information from sandstone samples to determine the geologic history of a particular region. Fossils are commonly found in sandstone, making it useful for paleontologists as well. sandstone has been popular and used for domestic construction and house wares since prehistoric times and continues to be used. it is relatively soft, making it easy to carve. It has been widely used around the world in constructing temples, cathedrals, homes, and other buildings. It has also been used for artistic purposes to create ornamental fountains and statues. sandstone is composed of different chemicals and rock fragments, and it is typically categorized as three main types. arkosic sandstone that contains more than 25 percent feldspar grains is called arkosic sandstone. The composition of this type of sandstone is similar to granite. Arkosic sandstone's high feldspar composition indicates that it has spent a short time in its depositional basin (place where sediments accumulate) because feldspar typically weathers rapidly, turning to clay if it sits long enough. quartzose quartzose sandstones typically have a quartz content of greater than 90 percent. This type of sandstone is also called beach sand or quartzite, and its high quartz composition suggests that the rock has spent a long period of time in its depositional basin. Typically, this type of sandstone is white, but it may be a variety of colors such as red, depending on the conditions in which it forms. Quartzose sandstone is marked with ripples, and is commonly found in central north america and australia. argillaceous argillaceous sandstone, also called wacke or greywacke, has a considerable amount of clay or silt content. It has a smoother texture in comparison to quartzose or arkosic sandstone. Almost all of this type of sandstone is formed in the sea and is dark in color with a mixture of rock fragments, feldspar and quartz along with large amounts of mud (15 to 40 percent). This type of sandstone is typically found in areas where rapid erosion occurs and where the climate is temperate or arid.

We are offering mint sandstone. sand stone is a classic sedimentary rock composed mainly of sand-sized minerals, bonded or cemented grains that might be either fragments of existing rock, or minerals. Typically, these grains are calcite, clays and silica. sandstone is usually formed by sedimentation that occurs as a result of a fluid, such as a river or a lake, in environments where sand accumulates such as sandy beaches, floodplains and deltas. Geologists gather information from sandstone samples to determine the geologic history of a particular region. Fossils are commonly found in sandstone, making it useful for paleontologists as well. sandstone has been popular and used for domestic construction and house wares since prehistoric times and continues to be used. it is relatively soft, making it easy to carve. It has been widely used around the world in constructing temples, cathedrals, homes, and other buildings. It has also been used for artistic purposes to create ornamental fountains and statues. sandstone is composed of different chemicals and rock fragments, and it is typically categorized as three main types. arkosic sandstone that contains more than 25 percent feldspar grains is called arkosic sandstone. The composition of this type of sandstone is similar to granite. Arkosic sandstone's high feldspar composition indicates that it has spent a short time in its depositional basin (place where sediments accumulate) because feldspar typically weathers rapidly, turning to clay if it sits long enough. quartzose quartzose sandstones typically have a quartz content of greater than 90 percent. This type of sandstone is also called beach sand or quartzite, and its high quartz composition suggests that the rock has spent a long period of time in its depositional basin. Typically, this type of sandstone is white, but it may be a variety of colors such as red, depending on the conditions in which it forms. Quartzose sandstone is marked with ripples, and is commonly found in central north america and australia. argillaceous argillaceous sandstone, also called wacke or greywacke, has a considerable amount of clay or silt content. It has a smoother texture in comparison to quartzose or arkosic sandstone. Almost all of this type of sandstone is formed in the sea and is dark in color with a mixture of rock fragments, feldspar and quartz along with large amounts of mud (15 to 40 percent). This type of sandstone is typically found in areas where rapid erosion occurs and where the climate is temperate or arid.

We are offering mint sandstone. sand stone is a classic sedimentary rock composed mainly of sand-sized minerals, bonded or cemented grains that might be either fragments of existing rock, or minerals. Typically, these grains are calcite, clays and silica. sandstone is usually formed by sedimentation that occurs as a result of a fluid, such as a river or a lake, in environments where sand accumulates such as sandy beaches, floodplains and deltas. Geologists gather information from sandstone samples to determine the geologic history of a particular region. Fossils are commonly found in sandstone, making it useful for paleontologists as well. sandstone has been popular and used for domestic construction and house wares since prehistoric times and continues to be used. it is relatively soft, making it easy to carve. It has been widely used around the world in constructing temples, cathedrals, homes, and other buildings. It has also been used for artistic purposes to create ornamental fountains and statues. sandstone is composed of different chemicals and rock fragments, and it is typically categorized as three main types. arkosic sandstone that contains more than 25 percent feldspar grains is called arkosic sandstone. The composition of this type of sandstone is similar to granite. Arkosic sandstone's high feldspar composition indicates that it has spent a short time in its depositional basin (place where sediments accumulate) because feldspar typically weathers rapidly, turning to clay if it sits long enough. quartzose quartzose sandstones typically have a quartz content of greater than 90 percent. This type of sandstone is also called beach sand or quartzite, and its high quartz composition suggests that the rock has spent a long period of time in its depositional basin. Typically, this type of sandstone is white, but it may be a variety of colors such as red, depending on the conditions in which it forms. Quartzose sandstone is marked with ripples, and is commonly found in central north america and australia. argillaceous argillaceous sandstone, also called wacke or greywacke, has a considerable amount of clay or silt content. It has a smoother texture in comparison to quartzose or arkosic sandstone. Almost all of this type of sandstone is formed in the sea and is dark in color with a mixture of rock fragments, feldspar and quartz along with large amounts of mud (15 to 40 percent). This type of sandstone is typically found in areas where rapid erosion occurs and where the climate is temperate or arid.

We are offering rose beige sandstone. sand stone is a classic sedimentary rock composed mainly of sand-sized minerals, bonded or cemented grains that might be either fragments of existing rock, or minerals. Typically, these grains are calcite, clays and silica. sandstone is usually formed by sedimentation that occurs as a result of a fluid, such as a river or a lake, in environments where sand accumulates such as sandy beaches, floodplains and deltas. Geologists gather information from sandstone samples to determine the geologic history of a particular region. Fossils are commonly found in sandstone, making it useful for paleontologists as well. sandstone has been popular and used for domestic construction and house wares since prehistoric times and continues to be used. it is relatively soft, making it easy to carve. It has been widely used around the world in constructing temples, cathedrals, homes, and other buildings. It has also been used for artistic purposes to create ornamental fountains and statues. sandstone is composed of different chemicals and rock fragments, and it is typically categorized as three main types. arkosic sandstone that contains more than 25 percent feldspar grains is called arkosic sandstone. The composition of this type of sandstone is similar to granite. Arkosic sandstone's high feldspar composition indicates that it has spent a short time in its depositional basin (place where sediments accumulate) because feldspar typically weathers rapidly, turning to clay if it sits long enough. quartzose quartzose sandstones typically have a quartz content of greater than 90 percent. This type of sandstone is also called beach sand or quartzite, and its high quartz composition suggests that the rock has spent a long period of time in its depositional basin. Typically, this type of sandstone is white, but it may be a variety of colors such as red, depending on the conditions in which it forms. Quartzose sandstone is marked with ripples, and is commonly found in central north america and australia. argillaceous argillaceous sandstone, also called wacke or greywacke, has a considerable amount of clay or silt content. It has a smoother texture in comparison to quartzose or arkosic sandstone. Almost all of this type of sandstone is formed in the sea and is dark in color with a mixture of rock fragments, feldspar and quartz along with large amounts of mud (15 to 40 percent). This type of sandstone is typically found in areas where rapid erosion occurs and where the climate is temperate or arid.