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Peik Chin Myaung Cave
Peik Chin Myaung (ပိတ်ချင်းမြောင်လိုဏ်ဂူ) is a limestone stalactite cave situated south of Wetwun village, 23 km from Pyin Oo Lwin, Myanmar. The cave is a tourist site on the Lashio road. History The cave was firstly developed by local Burmese Gurkhas and later co-opted by the Myanmar government as a tourist attraction in 1990. The cave covers an area of 45 acres, where local plants named Peik Chin, alike long pepper vine used to grow by the mouth of the cave. It is estimated to be 230 million to 310 million years old from the formation of limestone and hillocks. After the establishment of shrines with many Buddhist stupas inside the cave, it has also been called Maha Nadamu cave. Local interest The local people and many Myanmar pilgrims enjoyed swimming at the entrance of the cave. The water flows and cascades from the deep cave. Many locals from Pyin Oo Lwin have shops with local products such as wine and dried game meat (ဆတ ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Stupas
A stupa ( sa, स्तूप, lit=heap, ) is a mound-like or hemispherical structure containing relics (such as ''śarīra'' – typically the remains of Bhikkhu, Buddhist monks or Bhikkhuni, nuns) that is used as a place of meditation. In Buddhism, circumambulation or ''pradakhshina'' has been an important ritual and devotional practice since the earliest times, and stupas always have a ''pradakhshina'' path around them. The original South Asian form is a large solid dome above a tholobate or drum with vertical sides, which usually sits on a square base. There is no access to the inside of the structure. In large stupas there may be walkways for circumambulation on top of the base as well as on the ground below it. Large stupas have or had ''vedikā'' railings outside the path around the base, often highly decorated with sculpture, especially at the torana gateways, of which there are usually four. At the top of the dome is a thin vertical element, with one of more horizo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Stalactites
A stalactite (, ; from the Greek 'stalaktos' ('dripping') via ''stalassein'' ('to drip') is a mineral formation that hangs from the ceiling of caves, hot springs, or man-made structures such as bridges and mines. Any material that is soluble and that can be deposited as a colloid, or is in suspension, or is capable of being melted, may form a stalactite. Stalactites may be composed of lava, minerals, mud, peat, pitch, sand, sinter, and amberat (crystallized urine of pack rats). A stalactite is not necessarily a speleothem, though speleothems are the most common form of stalactite because of the abundance of limestone caves. The corresponding formation on the floor of the cave is known as a stalagmite. Mnemonics have been developed for which word refers to which type of formation; one is that ''stalactite'' has a C for "ceiling", and ''stalagmite'' has a G for "ground". Another example is that ''stalactites'' "hang on ''T''ight" and ''stalagmites'' "''M''ight grow up" ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pyin Oo Lwin
Pyin Oo Lwin or Pyin U Lwin (, ; Shan: ), formerly and colloquially referred to as Maymyo (), is a scenic hill town in the Mandalay Region, Myanmar, some east of Mandalay, and at an elevation of . The town was estimated to have a population of around 255,000 in 2014. Etymology * *Pyin Oo Lwin (ပြင်ဦးလွင်) *Maymyo (မေမြို့) * *Taung Hlay Khar (တောင်လှေခါး) ('hillside stairs') *Taung Sa Kan (တောင်စခန်း) ('hill station') and the best-known name, Pan Myo Taw ('city of flowers) * Remyo (historically) History The town began as a military outpost established near a small Shan village with two dozen households on the Lashio-Mandalay trail between Nawnghkio and Mandalay. In 1897, a permanent military post was established in the town and later, because of its climate, it became a hill station and the summer capital of British Burma. The establishment in Burma (civil, commercial and military) would move to ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Limestone
Limestone ( calcium carbonate ) is a type of carbonate sedimentary rock which is the main source of the material lime. It is composed mostly of the minerals calcite and aragonite, which are different crystal forms of . Limestone forms when these minerals precipitate out of water containing dissolved calcium. This can take place through both biological and nonbiological processes, though biological processes, such as the accumulation of corals and shells in the sea, have likely been more important for the last 540 million years. Limestone often contains fossils which provide scientists with information on ancient environments and on the evolution of life. About 20% to 25% of sedimentary rock is carbonate rock, and most of this is limestone. The remaining carbonate rock is mostly dolomite, a closely related rock, which contains a high percentage of the mineral dolomite, . ''Magnesian limestone'' is an obsolete and poorly-defined term used variously for dolomite, for limes ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Stalactite
A stalactite (, ; from the Greek 'stalaktos' ('dripping') via ''stalassein'' ('to drip') is a mineral formation that hangs from the ceiling of caves, hot springs, or man-made structures such as bridges and mines. Any material that is soluble and that can be deposited as a colloid, or is in suspension, or is capable of being melted, may form a stalactite. Stalactites may be composed of lava, minerals, mud, peat, pitch, sand, sinter, and amberat (crystallized urine of pack rats). A stalactite is not necessarily a speleothem, though speleothems are the most common form of stalactite because of the abundance of limestone caves. The corresponding formation on the floor of the cave is known as a stalagmite. Mnemonics have been developed for which word refers to which type of formation; one is that ''stalactite'' has a C for "ceiling", and ''stalagmite'' has a G for "ground". Another example is that ''stalactites'' "hang on ''T''ight" and ''stalagmites'' "''M''ight grow up" ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Myanmar
Myanmar, ; UK pronunciations: US pronunciations incl. . Note: Wikipedia's IPA conventions require indicating /r/ even in British English although only some British English speakers pronounce r at the end of syllables. As John C. Wells, John Wells explains, the English spellings of both Myanmar and Burma assume a non-rhotic variety of English, in which the letter r before a consonant or finally serves merely to indicate a long vowel: [ˈmjænmɑː, ˈbɜːmə]. So the pronunciation of the last syllable of Myanmar as [mɑːr] or of Burma as [bɜːrmə] by some speakers in the UK and most speakers in North America is in fact a spelling pronunciation based on a misunderstanding of non-rhotic spelling conventions. The final ''r'' in ''Myanmar'' was not intended for pronunciation and is there to ensure that the final a is pronounced with the broad a, broad ''ah'' () in "father". If the Burmese name my, မြန်မာ, label=none were spelled "Myanma" in English, this would b ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lashio
Lashio ( ; Shan: ) is the largest town in northern Shan State, Myanmar, about north-east of Mandalay. It is situated on a low mountain spur overlooking the valley of the Yaw River. Loi Leng, the highest mountain of the Shan Hills, is located to the south-east of Lashio. Lashio is the administrative center of Lashio Township and Lashio District; before April 2010, it was also the administrative center of Shan State (North). The population grew from approximately 5000 in 1960 to 88,590 in 1983. It was estimated at approximately 131,000 in 2009. The population is made up of mostly Shan, Chinese and Burmans. History The British colonial period in this part of the country began in 1887, and the Myanmar Railways line from Mandalay reached Lashio in 1903. Before British rule Lashio was also the centre of authority for the northern Shan States, but the Burmese post in the valley was close to the Nam Yao, in an old Chinese fortified camp. The Lashio valley was formerly very popul ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Burmese Gurkha
Burmese Gurkhas ( my, ဂေါ်ရခါးလူမျိုးများ; ne, गोरखाली) are a group of Nepali language speaking Burmese people of Khas/Gurkha ethnic group living in Myanmar (formerly Burma). While the Gurkhas have lived in Burma for many centuries, it was during the British rule in Burma that the majority of the Gurkha migrated from Nepal. The estimated population of Gurkha is nearly 1 million.The majority of Gurkha now reside in Yangon (Rangoon), Mandalay, Pyin U Lwin, Mogok, Tamu, Kalaymyo, Taunggyi, and other parts of the country. History and demography Like many other people who reside in Myanmar and who have their origin in Nepal, the majority of Gurkha came along with the British administration. Many Gurkhas served during the Second World War in the Burma Campaign, especially as rear guard units for the British retreat from Burma After Burma's independence in 1948, the Gurkhas joined the infant Burma Army. Many Gurkhas served in t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pindaya Caves
The Pindaya Caves ( my, ပင်းတယရွှေဥမင်, ; officially ), located next to the town of Pindaya, Shan State, Burma (Myanmar) are a Buddhist pilgrimage site and a tourist attraction located on a limestone ridge in the Myelat region. The area is part of the ancestral homeland of the Danu people. There are three caves on the ridge which runs north-south, but only the southern cave can be entered and explored. It is not known whether the other two penetrate for any extended distance into the hillside. Scholars have been pushing for the site's inclusion in the UNESCO World Heritage List. Interior The southernmost Pindaya cave can be entered and extends for about 490 feet along a well-worn path. It is known for its interior which contains over 8,000 images of Buddha. Some of the older statues and images in the cave have inscriptions dating to the late 18th century, or early Konbaung period, and the earliest one dates from 1773. There may be some images withou ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Buddhist Caves In Myanmar
Buddhism ( , ), also known as Buddha Dharma and Dharmavinaya (), is an Indian religion or philosophical tradition based on teachings attributed to the Buddha. It originated in northern India as a -movement in the 5th century BCE, and gradually spread throughout much of Asia via the Silk Road. It is the world's fourth-largest religion, with over 520 million followers (Buddhists) who comprise seven percent of the global population. The Buddha taught the Middle Way, a path of spiritual development that avoids both extreme asceticism and hedonism. It aims at liberation from clinging and craving to things which are impermanent (), incapable of satisfying ('), and without a lasting essence (), ending the cycle of death and rebirth (). A summary of this path is expressed in the Noble Eightfold Path, a training of the mind with observance of Buddhist ethics and meditation. Other widely observed practices include: monasticism; "taking refuge" in the Buddha, the , and the ; and ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Limestone Caves
Limestone ( calcium carbonate ) is a type of carbonate sedimentary rock which is the main source of the material lime. It is composed mostly of the minerals calcite and aragonite, which are different crystal forms of . Limestone forms when these minerals precipitate out of water containing dissolved calcium. This can take place through both biological and nonbiological processes, though biological processes, such as the accumulation of corals and shells in the sea, have likely been more important for the last 540 million years. Limestone often contains fossils which provide scientists with information on ancient environments and on the evolution of life. About 20% to 25% of sedimentary rock is carbonate rock, and most of this is limestone. The remaining carbonate rock is mostly dolomite, a closely related rock, which contains a high percentage of the mineral dolomite, . ''Magnesian limestone'' is an obsolete and poorly-defined term used variously for dolomite, for limestone co ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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