Stone Carving In Odisha
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Stone Carving In Odisha
Stone carving in Odisha is the ancient practice of sculpting stone into art and utilitarian objects. It is an ancient practice in the Indian state of Odisha. Stone carving is practiced by artisans mainly in Puri, Bhubaneswar and Lalitgiri in the Cuttack district, though some carvings can be found in Khiching in the Mayurbhanj District. Stone carving is one of the major handcrafts of Odisha. The art form primarily consists of custom carved works, with the Sun Temple of Konark and its intricate sculpture and delicate carvings on the red vivid sandstone exemplifying the practice. Other noteworthy monuments include the Stupas of Udayagiri and Ratnagiri and the temples at Jagannath, Lingaraj, Mukteshwar and as well as other temples in the region. Stones Sandstone, soapstone, serpentinite, Makrana marble, and granite were used in Konark stone carving. Skillful artists may use the soft, white soapstone, , or the slightly harder greenish chlorite The chlorite ion, or c ...
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Handcraft
A handicraft, sometimes more precisely expressed as artisanal handicraft or handmade, is any of a wide variety of types of work where useful and decorative objects are made completely by one’s hand or by using only simple, non-automated related tools like scissors, carving implements, or hooks. It is a traditional main sector of craft making and applies to a wide range of creative and design activities that are related to making things with one's hands and skill, including work with textiles, moldable and rigid materials, paper, plant fibers,clay etc. One of the oldest handicraft is Dhokra; this is a sort of metal casting that has been used in India for over 4,000 years and is still used. In Iranian Baluchistan, women still make red ware hand-made pottery with dotted ornaments, much similar to the 5000-year-old pottery tradition of Kalpurgan, an archaeological site near the village. Usually, the term is applied to traditional techniques of creating items (whether for perso ...
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Ratnagiri, Odisha
Ratnagiri (Odia: ରତ୍ନଗିରି, meaning "hill of jewels") is the site of a ruined mahavihara, once the major Buddhist monastery in modern Odisha, India. It is located on a hill in between the Brahmani and Birupa rivers in Jajpur district. It is close to other Buddhist sites in the area, including Lalitagiri and Udayagiri, and from the state capital Bhubaneswar and 70km from the former state capital Cuttack. The Buddhist monuments were constructed from the 5th century CE onwards, with the last work in the 13th century, and the peak period of work done between about the 7th to 10th centuries. After perhaps the 16th century the site ceased to be used and fell into ruins. These were little known until the 1960s when major campaigns of excavations by the Archaeological Survey of India ("ASI") revealed the site, producing large quantities of very fine sculpture. Monastery 1 has been described as "the finest in terms of carved stone decoration to have survived in India". ...
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Puja (Hinduism)
''Puja'' ( sa, पूजा, pūjā, translit-std=IAST) is a worship ritual performed by Hindus, Buddhists and Jains to offer devotional homage and prayer to one or more deities, to host and honor a guest, or to spiritually celebrate an event. It may honor or celebrate the presence of special guests, or their memories after they die. The word ''pūjā'' is Sanskrit, and means reverence, honor, homage, adoration, and worship.पूजा
''Sanskrit Dictionary'', Germany (2009)
Puja, the loving offering of light, flowers, and water or food to the divine, is the essential ritual of Hinduism. For the worshipper, the divine is visible in the image, and the divinity sees the worshipper. The interaction between human and deity, between

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Stoneware
Stoneware is a rather broad term for pottery or other ceramics fired at a relatively high temperature. A modern technical definition is a Vitrification#Ceramics, vitreous or semi-vitreous ceramic made primarily from stoneware clay or non-refractory fire clay. Whether vitrified or not, it is nonporous (does not soak up liquids);Arthur Dodd & David Murfin. ''Dictionary of Ceramics''; 3rd edition. The Institute of Minerals, 1994. it may or may not be glaze (ceramics), glazed. Historically, around the world, it has been developed after earthenware and before porcelain, and has often been used for high-quality as well as utilitarian wares. As a rough guide, modern earthenwares are normally fired in a kiln at temperatures in the range of about 1,000 °Celsius, C (1,830 Fahrenheit, °F) to ; stonewares at between about to ; and porcelains at between about to . Historically, reaching high temperatures was a long-lasting challenge, and temperatures somewhat below these were used for a lo ...
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Chlorite
The chlorite ion, or chlorine dioxide anion, is the halite with the chemical formula of . A chlorite (compound) is a compound that contains this group, with chlorine in the oxidation state of +3. Chlorites are also known as salts of chlorous acid. Compounds The free acid, chlorous acid HClO2, is the least stable oxoacid of chlorine and has only been observed as an aqueous solution at low concentrations. Since it cannot be concentrated, it is not a commercial product. The alkali metal and alkaline earth metal compounds are all colorless or pale yellow, with sodium chlorite (NaClO2) being the only commercially important chlorite. Heavy metal chlorites (Ag+, Hg+, Tl+, Pb2+, and also Cu2+ and ) are unstable and decompose explosively with heat or shock. Sodium chlorite is derived indirectly from sodium chlorate, NaClO3. First, the explosively unstable gas chlorine dioxide, ClO2 is produced by reducing sodium chlorate with a suitable reducing agent such as methanol, hydrogen perox ...
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Granite
Granite () is a coarse-grained (phaneritic) intrusive igneous rock composed mostly of quartz, alkali feldspar, and plagioclase. It forms from magma with a high content of silica and alkali metal oxides that slowly cools and solidifies underground. It is common in the continental crust of Earth, where it is found in igneous intrusions. These range in size from dikes only a few centimeters across to batholiths exposed over hundreds of square kilometers. Granite is typical of a larger family of ''granitic rocks'', or ''granitoids'', that are composed mostly of coarse-grained quartz and feldspars in varying proportions. These rocks are classified by the relative percentages of quartz, alkali feldspar, and plagioclase (the QAPF classification), with true granite representing granitic rocks rich in quartz and alkali feldspar. Most granitic rocks also contain mica or amphibole minerals, though a few (known as leucogranites) contain almost no dark minerals. Granite is nearly alway ...
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Makrana Marble
Makrana marble is a type of white marble, popular for use in sculpture and building decor. It is mined in the town of Makrana in Rajasthan, India, and was used in the construction of several iconic monuments such as the Taj Mahal in Agra and the Victoria Memorial in Kolkata. The Makrana Marble is listed as a Global Heritage Stone Resource by International Union of Geological Sciences Geology In the Makrana area, marble is found as five steeply-dipping bands. They form part of the Ajmer Formation of the Delhi Supergroup, which is a sequence of sedimentary rocks that was deposited in the Delhi Basin during the Proterozoic. About 1450 Ma (million years ago) these rocks were affected by the Delhi Orogeny, causing the metamorphism that transformed the original limestones to marble and the folding that caused the steep dip and the current outcrop pattern. Properties Makrana is regarded as the oldest place in India with a marble quarry. Upon mining, Makrana marble is not subjected t ...
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Serpentinite
Serpentinite is a rock composed predominantly of one or more serpentine group minerals, the name originating from the similarity of the texture of the rock to that of the skin of a snake. Serpentinite has been called ''serpentine'' or ''serpentine rock'', particularly in older geological texts and in wider cultural settings.California Government Code § 425.2; ''see'' Formation and mineralogy Serpentinite is formed by near to complete serpentinization of mafic to ultramafic rocks. Serpentinite can be formed wherever ultramafic rock is infiltrated by water poor in carbon dioxide. This occurs at mid-ocean ridges and in the forearc mantle of subduction zones. The final mineral composition of serpentinite is usually dominated by lizardite, chrysotile, and magnetite. Brucite and antigorite are less commonly present. Lizardite, chrysotile, and antigorite all have approximately the formula or , but differ in minor components and in form. Accessory minerals, present in smal ...
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Soap Stone
Soapstone (also known as steatite or soaprock) is a talc-schist, which is a type of metamorphic rock. It is composed largely of the magnesium rich mineral talc. It is produced by dynamothermal metamorphism and metasomatism, which occur in the zones where tectonic plates are subducted, changing rocks by heat and pressure, with influx of fluids, but without melting. It has been a medium for carving for thousands of years. Terminology The definitions of the terms "steatite" and "soapstone" vary with the field of study. In geology, steatite is a rock that is to a very large extent composed of talc. The mining industry will define steatite as a high-purity talc rock that is suitable for manufacturing of, for example, insulators, the lesser grades of the mineral can be called simply "talc rock". Steatite can be used both in lumps ("block steatite", "lava steatite", "lava grade talc"), and in the ground form. While the geologists logically will use "steatite" to designate both forms, ...
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Sandstone
Sandstone is a clastic sedimentary rock composed mainly of sand-sized (0.0625 to 2 mm) silicate grains. Sandstones comprise about 20–25% of all sedimentary rocks. Most sandstone is composed of quartz or feldspar (both silicates) because they are the most resistant minerals to weathering processes at the Earth's surface. Like uncemented sand, sandstone may be any color due to impurities within the minerals, but the most common colors are tan, brown, yellow, red, grey, pink, white, and black. Since sandstone beds often form highly visible cliffs and other topographic features, certain colors of sandstone have been strongly identified with certain regions. Rock formations that are primarily composed of sandstone usually allow the percolation of water and other fluids and are porous enough to store large quantities, making them valuable aquifers and petroleum reservoirs. Quartz-bearing sandstone can be changed into quartzite through metamorphism, usually related to ...
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Mukteshwar
Mukteshwar is a village and tourist destination in the Nainital district of Uttarakhand, India. It sits high in the Kumaon Hills at an altitude of 2171 meters (7500 feet), 51 km from Nainital, 72 km from Haldwani, and 343 km from Delhi. Places of interest Mukteshwar Shiva temple Mukteshwar gets its name from a 350-year-old temple of Shiva, known as ''Mukteshwar Dham'', situated atop the highest point in the town, on the veterinary institute's campus. Close to it lie the overhanging cliffs, locally known as ''Chauli-ki-Jali'', used for rock climbing and rappelling, with an excellent view of the valleys below. ''Mukteshwar famously know for its breezy waterfalls houses some famous waterfallas such as ''The Bhalu Ghaad, Tarikhet waterfalls, Rudradhari waterfall and The Dhokaney waterfall''. The sunrise point is at the government-run PWD guest house. Another tourist attraction is the small Satoli Village, situated just 21 km from Mukteshwar. One can ...
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Lingaraj
Lingaraja Temple is a Hindu temple dedicated to Shiva and is one of the oldest temples in Bhubaneswar, the capital of the Indian state of Odisha, India. The temple is the most prominent landmark of Bhubaneswar city and one of the major tourist attractions of the state. The Lingaraja temple is the largest temple in Bhubaneswar. The central tower of the temple is tall. The temple represents the quintessence of the Kalinga architecture and culminating the medieval stages of the architectural tradition at Bhubaneswar. The temple is believed to be built by the kings from the Somavamsi dynasty, with later additions from the Ganga rulers. The temple is built in the ''Deula'' style that has four components namely, ''vimana'' (structure containing the sanctum), ''jagamohana'' (assembly hall), ''natamandira'' (festival hall) and ''bhoga-mandapa'' (hall of offerings), each increasing in the height to its predecessor. The temple complex has 50 other shrines and is enclosed by a large co ...
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