Sunday, April 27, 2014

DIAH WULANDARI



Name  : Diah Wulandari
Class   : D4.1
NPM   : 12 23 065

 

Hạ Long Bay

From Wikipedia, the free encyclopedia

Hạ Long Bay (Vietnamese: Vịnh Hạ Long, About this sound listen, literally: "descending dragon bay") is a UNESCO World Heritage Site, and a popular travel destination, in Quảng Ninh Province, Vietnam. Administratively, the bay belongs to Hạ Long City, Cẩm Phả town, and part of Vân Đồn District. The bay features thousands of limestone karsts and isles in various sizes and shapes. Hạ Long Bay is a center of a larger zone which includes Bái Tử Long bay to the northeast, and Cát Bà islands to the southwest. These larger zones share similar geological, geographical, geomorphological, climate, and cultural characters.
Hạ Long Bay has an area of around 1,553 km2, including 1,960–2,000 islets, most of which are limestone. The core of the bay has an area of 334 km2 with a high density of 775 islets.[1] The limestone in this bay has gone through 500 million years of formation in different conditions and environments. The evolution of the karst in this bay has taken 20 million years under the impact of the tropical wet climate.[2] The geo-diversity of the environment in the area has created biodiversity, including a tropical evergreen biosystem, oceanic and sea shore biosystem.[3] Hạ Long Bay is home to 14 endemic floral species[4] and 60 endemic faunal species.[5]
Historical research surveys have shown the presence of prehistorical human beings in this area tens of thousands years ago. The successive ancient cultures are the Soi Nhụ culture around 18,000–7000 BC, the Cái Bèo culture 7000–5000 BC[6] and the Hạ Long culture 5,000–3,500 years ago.[7] Hạ Long Bay also marked important events in the history of Vietnam with many artifacts found in Bài Thơ Mout, Đầu Gỗ Cave, Bãi Cháy.[7]
500 years ago, Nguyễn Trãi praised the beauty of Hạ Long Bay in his verse Lộ nhập Vân Đồn, in which he called it "rock wonder in the sky".[8] In 1962, the Ministry of Culture, Sports and Tourism of North Vietnam listed Hạ Long Bay in the National Relics and Landscapes publication.[9] In 1994, the core zone of Hạ Long Bay was listed by UNESCO as a World Heritage Site according to criterion vii, and listed for a second time according to criterion viii.[10]

Etymology

The name Hạ Long is derived from the Sino-Vietnamese 下 龍, meaning "descending dragon".
According to local legend, when Vietnam had just started to develop into a country, they had to fight against invaders. To assist the Vietnamese in defending their country, the gods sent a family of dragons as protectors. This family of dragons began spitting out jewels and jade. These jewels turned into the islands and islets dotting the bay, linking together to form a great wall against the invaders. Under magics, numerous rock mountains abruptly appeared on the sea, ahead of invaders' ships; the forward ships struck the rocks and each other. After winning the battle, the dragons were interested in peaceful sightseeing of the Earth, and then decided to live in this bay. The place where the mother dragon descended was named Hạ Long, the place where the dragon's children attended upon their mother was called Bái Tử Long island (Bái: attend upon, Tử: children, Long: dragon), and the place where the dragon's children wriggled their tails violently was called Bạch Long Vỹ island (Bạch: white-color of the foam made when Dragon's children wriggled, Long: dragon, Vỹ: tail), present day Trà Cổ peninsula, Móng Cái.[11]

Overview


Thien Cung grotto
Floating fishing village
The bay consists of a dense cluster of some 1,600 [12] limestone monolithic islands each topped with thick jungle vegetation, rising spectacularly from the ocean. Several of the islands are hollow, with enormous caves. Hang Đầu Gỗ (Wooden stakes cave) is the largest grotto in the Hạ Long area. French tourists visited in the late 19th century, and named the cave Grotte des Merveilles. Its three large chambers contain large numerous stalactites and stalagmites (as well as 19th century French graffiti). There are two bigger islands, Tuần Châu and Cát Bà, that have permanent inhabitants, as well as tourist facilities including hotels and beaches. There are a number of beautiful beaches on the smaller islands.
A community of around 1,600 people live on Hạ Long Bay in four fishing villages: Cửa Vạn, Ba Hang, Cống Tàu and Vông Viêng in Hùng Thắng commune, Hạ Long city. They live on floating houses and are sustained through fishing and marine aquaculture (cultivating marine biota), plying the shallow waters for 200 species of fish and 450 different kinds of mollusks. Many of the islands have acquired their names as a result of interpretation of their unusual shapes. Such names include Voi Islet (elephant), Ga Choi Islet (fighting cock), Khi Islet (monkey), and Mai Nha Islet (roof). 989 of the islands have been given names. Birds and animals including bantams, antelopes, monkeys, and lizard also live on some of the islands.
Almost all these islands are as individual towers in a classic fenglin landscape with heights from 50m to 100m, and height/width ratios of up to about six.
Another specific feature of Halong Bay is the abundance of lakes inside the limestone islands. For example, Dau Be island has six enclosed lakes. All these island lakes occupy drowned dolines within fengcong karst.

Location

Hạ Long Bay is located in northeastern Vietnam, from E106°56' to E107°37' and from N20°43' to N21°09'. The bay stretches from Yên Hưng district, past Hạ Long city, Cẩm Phả town to Vân Đồn District, bordered on the south and southeast by the Gulf of Tonkin, on the north by China, and on the west and southwest by Cát Bà Island. The bay has a 120 km long coastline and is approximately 1,553 km² in size with about 2,000 islets. The area designated by UNESCO as the World Natural Heritage Site incorporates 434 km² with 775 islets, of which the core zone is delimited by 69 points: Đầu Gỗ island on the west, Ba Hầm lake on the south and Cống Tây island on the east. The protected area is from the Cái Dăm petrol store to Quang Hanh commune, Cẩm Phả town and the surrounding zone.

Climate

The climate of the bay is tropical, wet, sea islands, with two seasons: hot and moist summer, and dry and cold winter. The average temperature is from 15°C- 25°C, and annual rainfall is between 2 meters and 2.2 meters. Hạ Long Bay has the typical diurnal tide system (tide amplitude ranges from 3.5-4m). The salinity is from 31 to 34.5MT in the dry season and lower in the rainy season.

History

Soi Nhụ culture (16,000–5000 BC)

Located in Hạ Long and Bái Tử Long are archaeological sites such as Mê Cung and Thiên Long. There are remains from mounds of mountain shellfish (Cyclophorus), spring shellfish (Melania), some fresh water mollusc and some rudimentary labour tools. The main way of life of Soi Nhụ's inhabitants included catching fish and shellfish, collecting fruits and digging for bulbs and roots. Their living environment was a coastal area unlike other Vietnamese cultures, for example, like those found in Hòa Bình and Bắc Sơn.

Cái Bèo culture (5000–3000 BC)

Located in Hạ Long and Cát Bà island, its inhabitants developed to the level of sea exploitation.

Feudal period

History shows that Hạ Long Bay was the setting for local naval battles against Vietnam's coastal neighbors. On three occasions, in the labyrinth of channels in Bạch Đằng river near the islands, the Vietnamese army stopped the Chinese from landing. In 1288, General Trần Hưng Đạo stopped Mongol ships from sailing up the nearby Bạch Đằng River by placing steel-tipped wooden stakes at high tide, sinking the Mongol Kublai Khan's fleet.
During the Vietnam War, many of the channels between the islands were heavily mined by the United States navy, some of which pose a threat to shipping to this day.

 

 

Geology and geomorphology

In 2000, the UNESCO’s World Heritage Committee has inscribed the Hạ Long Bay in the World Heritage List according to its outstanding examples representing major stages of the Earth’s history and its original limestone karstic geomorphologic features. The Hạ Long Bay and its adjacent areas consist of a part of the Sino-Vietnamese composite terrane having its development history from pre-Cambrian up to present day. During Phanerozoic, terrigenous, volcanogenic and cherty-carbonate sediments containing in abundance graptolites, brachiopods, fishes, corals, foraminiferas, radiolarias, bivalves and flora, separated one from another by 10 stratigraphic gaps, but the boundary between Devonian and Carboniferous has been considered as continuous. The limestone karstic geomorphology of the bay was developed since Miocene, especially the cone-shaped hills (fengcong), or isolated high limestone karst towers (fenglin) with many remnants of old phreatic caves, old karstic foot caves, marine notch caves form magnificent limestone karst landforms as unique on the world. The Quaternary geology was developed through 5 cycles with the intercalation of marine and continental environments. The present Hạ Long Bay, in fact, appeared after the Middle Holocene maximum transgression, leaving ultimate zone of lateral undercutting in the limestone cliffs bearing many shells of oysters, having the 14C age as 2280 to >40,000 y. BP. Geological resources are abundant: anthracite, lignite, oil shale, petroleum, phosphate, limestone and cement additives, kaolin, silica sand, dolomite, quartzite of exogenous origin, and antimony, mercury of hydrothermal origin. Besides, there still are surface water, groundwater and thermal mineral water on the shore of the Hạ Long - Bái Tử Long Bays and other environmental resources [17, 18],
In terms of marine geology, this area is recorded as an especially coastal sedimentary environment. In the alkaline seawater environment, the chemical denudation process of calcium carbonate proceeds rapidly, creating wide, strangely shaped marine notches.
The bottom surface sediments are various from clay mud to sand, however, silty mud and clay mud are dominated in distribution. Especially, the carbonate materials originated from organisms make up from 60-65% sedimentary content. The surface sediments of coral reefs are mainly sand and pebbles of which the carbonate materials occupy for more than 90%. The intertidal zone sediments are various from clay mud to sand and gravel depending to distinguished sedimentary environments such as mangrove marshes, tidal flats, beaches etc. At the small beaches, but wonderfully beautiful, the sand sediments may be dominated quartz or carbonate materials.
The sediment layers of intertidal zone, the upper sea bed with a plain surface conserving ancient rivers, systems of caves and it's sediments, traces of ancient marine action forming distinctive notches, beaches and marine terraces, mangrove swamps are important evidence of geological events and processes taking place during Quaternary.

History of tectonics

Hạ Long Bay has experienced at least 500 million years in various geological states of orogeny, marine transgression and marine regression. During the Ordovician and Silurian periods (500-410 million years ago), Hạ Long Bay was deep sea. During the Carboniferous and Permian periods (340-250 million years ago), Hạ Long Bay was at shallow sea level.
The dominated uplift movement of neotectonic and recent tectonic influenced deeply on topography of this area, and the present landscape of sea-islands was formed around 7 or 8 thousand years ago by the sea invasion during Holocene transgression begun at about 17-18 thousand years ago. Particularly from the Holocene time, from about 11,000 years ago Cat Ba - Hạ Long area has much archaeological evidence connecting variations in sea levels with the development of ancient cultures such as the Soi Nhu and Ha Long cultures.

Karst geomorphology value

Due to a simultaneous combination of ideal factors such as thick, pale, grey, and strong limestone layers, which are formed by fine-grained materials; hot and moist climate and slow tectonic process as a whole; Hạ Long Bay has had a complete karst evolution for 20 million years. There are many types of karst topography in the bay, such as karst field.
Hạ Long Bay is a mature karst landscape developed during a warm, wet, tropical climate. The sequence of stages in the evolution of a karst landscape over a period of 20 million years requires a combination of several distinct elements including a massive thickness of limestone, a hot wet climate and slow overall tectonic up lift. The process of karst formation is divided into five stage is the formation of the distinctive do line karst. This is followed by the development of fengcong karst can be seen in the groups of hills on Bo Hon and Dau Be Inland. These cones with sloping side average 100m in height with the tallest exceeding 200m. Fenglin karst is characterised by steep separate towers. The hundreds of rocky islands with form the beautiful and famous landscape of the Bay are the individual towers of a classic Fenglin landscape where the intervening plains have been submerged by the sea. Most towers reach a height of between 50 and 100m with a height to width ratio of about 6. The karst dolines were flooded by the sea becoming the abundance of lakes that lie within the limestone islands. For example, Dau Be island at the mouth of the Bay has six enclosed lakes including those of the Ba Ham lakes lying within its fencong karst. The Bay contains examples of the landscape elements of fengcong, fenglin and karst plain. These are not separate evolutionary stages but the result of natural non – uniform processes in the denudation of a large mass of limestone. Marine erosion created the notches which in some places have been enlarged into caves. The marine notch is a feature of limestone coastline but, in Ha Long Bay, it has created the mature landscape.
Within Ha Long Bay, the main accessible caves are the older passages that survive from the time when the karst was evolving though its various stages of fengcong and fenglin. Three main types of caves can be recognized in the limestone islands (Waltham, T. 1998):
  • Remnants of old phreatic caves
  • Old karstic foot caves
  • Marine notch caves
The first group of caves is old phreatic caves which include Sung Sot, Tam Cung, Lau Dai, Thien Cung, Dau Go, Hoang Long, Thien Long. Nowadays, these caves lie at various high levels. Sung Sot cave is on Bo Hon island. From its truncated entrance chambers on allege high on the cliff, a passage of more that 10m high and wide descends to the south. Tam Cung is a large phreatic fissure cave that developed in the bedding planes of the limestone dividing the fissure cave into three chambers. Lau Dai is a cave with a complex of passages extending over 300m opening on the south side of Con Ngua island. Thien Cung and Dau Go are remnants of the same old cave system. They both survive in the northern part of Dau Go island at between 20 and 50m above sea level. Thien Cung has one large chamber more that 100m long, blocked at its ends and almost subdivided into smaller chambers by massive wall of stalactites and stalagmites. Dau Go is a single large tunnel descending along a major set of fractures to a massive choke.
The second group of caves is the old karstic foot caves which include Trinh Lu, Bo Nau, Tien Ong and Trong caves. Foot caves are a ubiquitous feature of karst landscapes which have reached a stage of widespread lateral undercutting at base level. They may extend back into maze caves of stream caves draining from larger cave systems within the limestone. They are distinguished by the main elements of their passages being close to the horizontal and are commonly related to denuded or accumulated terraces at the old base levels. Trinh Nu, which is one of the larger foot caves in Ha Long Bay with its ceiling at about 12m above sea level and about 80m in length, was developed in multiple stages. Bo Nau, a horizontal cave containing old stalactite deposits, cuts across the 25o dip of the bedding plane.
The third group is the marine notch caves that are a special feature of the karst of Ha Long Bay. The dissolution process of sea water acting on the limestone and erosion by wave action crates notches at the base of the cliffs. In advantageous conditions, dissolution of the limestone allows the cliff notches to be steadily deepened and extended into caves. Many of these at sea level extend right though the limestone hills into drowned dolines which are now tidal lakes.
A distinguishing feature of marine notch caves is an absolutely smooth and horizontal ceiling cut through the limestone. Some marine notch caves had been not formed at present sea level, but old sea levels related to sea level changes in Holocene transgression, event to Pleistocene sea levels. Some of them passed preserved the development of old karstic foot cave in mainland environment or preserved the remnants of older phreatic caves. One of the most unusual features of Ha Long Bay is the Bo Ham lake group of hidden lakes and their connecting tunnel – notch caves in Dau Be island. From the island’s perimeter cliff a cave, 10m wide at water level and curving so that it is almost completely dark, extends about 150m to Lake 1. Luon cave is on Bo Hon island and extends 50m though to an enclosed tidal lake. It has a massive stalactite hanging 2m down and truncated at the modern tidal level. It has passed though many stages in its formation.
The karst landscape of Ha Long Bay is of international significance and of fundamental importance to the science of geomorphology. The fenglin tower karst, which is the type present in much of Ha Long Bay, is the most extreme form of limestone landscape development. If these karst landscapes are broadly compared in terms of their height, steepness and number of their limestone towers, Ha Long Bay is probably second in the entire world only to Yangshou, in China. However, Ha Long Bay ha also been invaded by the sea so that the geomorphology of its limestone is lands are, at least in part, the consequence of marine erosion. The marine invasion distinguishes Ha Long Bay and makes it unique in the world. There are other areas of submerged karst towers which were invaded by the sea, but none is as extensive as Ha Long Bay. [14] [15]

Timeline of geologic evolution

Some of the most remarkable geological events in Hạ Long Bay's history have occurred in the last 1,000 years, include the advance of the sea, the raising of the bay area, strong erosion that has formed coral, and, pure blue and heavily salted water. This process of erosion by seawater has deeply engraved the stone, contributing to its fantastic beauty. Present-day Hạ Long Bay is the result of this long process of geological evolution that has been influenced by so many factors.
Due to all these factors, tourists visiting Hạ Long Bay are not only treated to one of the natural wonders of the world, but also to a precious geological museum that has been naturally preserved in the open air for the last 300 million years.
Date
Geologic period
Events
570,000,000-500,000,000 BC
beginning of the Cambrian Period
The area, which now forms Hạ Long Bay, was basically mainland, submitted to a process of rain erosion.

end of the Cambrian Period
The area was flooded, commencing the existence of Hạ Long Bay.
500,000,000-400,000,000 BC
Ordovician and Silurian periods
The area of north-east Vietnam was almost like a deep sea, submitted to the constant activity of tectonic plates.

end of the Silurian Period
It underwent a phase of inverse-motion that created mountains deep under the water.
420,000,000-340,000,000 BC
end of the Silurian Period and throughout the whole Devonian Period
The area was subjected to powerful forces of erosion from the hot and dry climate. At this point, Hạ Long was part of a wide mainland that comprised most of today's South China Sea and Chinese continental shelf.

end of the Devonian Period
Due to tectonic activity, the Hạ Long area and the entire north-east region were raised from the depths
340,000,000-240,000,000 BC
later Carboniferous and Permian periods
The formation of the limestone layer more than 1,000 m thick. A shallow and warm sea reformed, which existed for approximately 100 million years. It created two kinds of limestone: the Cát Bà layer of the early Carboniferous period (450 m thick); and the Quang Hanh layer of the middle Carboniferous and the early Permian period (750 m thick). These two layers constitute the majority of the islands of the Bay.
67,000,000 BC
end of the Cretaceous Period
Hạ Long Bay existed in the environment of a high mountainous mainland due to the influence of strong mountain-forming phases.

middle of the Paleogene Period
These motions remain continuous and stable, while strong processes of erosion began, and after millions of years, a form of semi-highland topography took shape. The continuation of this erosion has progressively cut the highlands into blocks with altitudes similar to today's mountains
26,000,000-10,000,000 BC
Neogene Period
The development of the Hạ Long depression
2,000,000-9000 BC
Pleistocene epoch of the Quaternary period
The process of erosion began dissolving the limestone-rich region of Hạ Long, after that, forming the limestone plain was most active
68,000-9000 BC
middle and late Pleistocene Epoch
Period when the caves and grottoes of the area formed.

early Holocene Epoch
The islands of today's Hạ Long Bay are basically remnants of these mountains, flooded. Rainwater flowed into crevices in the limestone that had formed from tectonic activity. This steady erosion constantly widened the cracks, eventually creating today's formations.
9000-5000 BC
Holocene Epoch
This period is notable for the advance of the sea.
5000-2000 BC
The movement of the sea reached its peak and forming today's Hạ Long Bay.
2000–1000 BC
With the sea in a steady process of recession, Hạ Long culture began to develop.

beginning of the late Holocene Epoch
The level of the water once again increased, forming a marshy floor of canals and streams, and creating the water marks that can be seen on the stone cliffs of today.

Ecology

Halong Bay is host to two ecosystems: a tropical, moist, evergreen rainforest ecosystem; and a marine and coastal ecosystem. The bay is home to seven endemic species: Livistona halongensis, Impatiens halongensis, Chirita halongensis, Chirita hiepii, Chirita modesta, Paraboea halongensis and Alpinia calcicola.
The many islands that dot the bay are home to a great many other species, including (but likely not limited to): 477 magnoliales, 12 pteris, 20 salt marsh flora; and 4 amphibia, 10 reptilia, 40 aves, and 4 mammalia.
Common aquatic species found in the bay include: cuttlefish (mực); oyster (hào); cyclinae (ngán); prawns (penaeidea (tôm he), panulirus (tôm hùm), parapenaeopsis (tôm sắt), etc.); sipunculoideas (sá sùng); nerita (ốc đĩa); charonia tritonis (ốc tù và); and cà sáy.

Environmental damage

With an increasing tourist trade, mangroves and seagrass beds have been cleared and jetties and wharves have been built for tourist boats.
Game fishing, often near coral reefs, is threatening many endangered species of fish.
Local government and businesses are aware of problems and many measures have been taken to minimize tourism affect to the bay environment for sustainable economic growth [16]

Awards and designations

In 1962, the Vietnam Ministry of Culture, Sport and Tourism designated Hạ Long Bay a 'Renowned National Landscape Monument'.
Hạ Long Bay was first listed as a UNESCO World Heritage Site in 1994,[17] in recognition of its outstanding, universal aesthetic value. In 2000 the World Heritage Committee additionally recognised Hạ Long Bay for its outstanding geological and geomorphological value,[12] and its World Heritage Listing was updated.[18]
In October 2011, World Monuments Fund included the bay on the 2012 World Monuments Watch, citing tourism pressures and associated development as threats to the site that must be addressed. The goal of Watch-listing is to promote strategies of responsible heritage-driven development for a sustainable future.
In 2012, New 7 Wonders Foundation officially named Halong Bay as one of New Seven Natural Wonders of the world.
Hạ Long Bay is also a member of the Club of the Most Beautiful Bays of the World.[19]

In literature

In writings about Hạ Long Bay, the following Vietnamese writers said:
  • Nguyễn Trãi: "This wonder is ground raising up into the middle of the high sky".
  • Xuân Diệu: "Here is the unfinished works of the Beings...Here is the stones which the Giant played and threw away".
  • Nguyên Ngọc: "...to form this first- rate wonder, nature only uses: Stone and Water...There are just only two materials themselves chosen from as much as materials, in order to write, to draw, to sculpture, to create everything...It is quite possible that here is the image of the future world".
  • Ho Chi Minh: "It is the wonder that one cannot impart to others".
  • Phạm Văn Đồng: "Is it one scenery or many sceneries? Is it the scenery in the world or somewhere?".
  • Nguyễn Tuân: "Only mountains accept to be old, but Hạ Long sea and wave are young for ever".
  • Huy Cận: "Night breathes, stars wave Hạ Long's water".
  • Chế Lan Viên:
"Hạ Long, Bái Tử Long- Dragons were hidden, only stones still remain
On the moonlight nights, stones meditate as men do..."
Lord Trịnh Cương overflowed with emotion: "Mountains are glistened by water shadow, water spills all over the sky".

Ancient tales

Hạ Long bay's inhabitants have developed numerous tales explaining names given to various isles and caves in the bay.[20]
  • Đầu Gỗ cave (literally: "the end of wooden bars" cave): these wooden bars in this cave are the remnants of sharped wooden columns built under the water level by the order of Trần Hưng Đạo commander in order to sink Mongolian invaders' ships in 13th century.
  • Kim Quy cave (literally: "Golden Turtle" cave): it is told that the Golden Turtle swam toward the Eastern Sea (international name: South China Sea) after returning the holy sword which had assisted King Lê Thái Tổ in the combat against Ming invaders from China. Next, with the approval of the Sea King, Golden Turtle continued to fight against monsters in this marine area. Unfortunately, the turtle became exhausted and passed away in a cave. Consequently, the cave was named after the Golden Turtle.
  • Con Cóc isle (literally: Frog isle): is a frog- like isle. According to ancient tales, in a year of severe drought, a frog directed all animals to the Heaven and protested against the God. They demonstrated in favour of making rain. As a result, the God must accept the frog as his uncle. Since then, whenever frogs grind their teeth, the God has to pour water down the ground.




Name  : Diah Wulandari
Class   : D4.1
NPM   : 12 23 065

 

Taman Mini Indonesia Indah     

From Wikipedia, the free encyclopedia
Taman Mini Indonesia Indah (TMII) or "Beautiful Indonesia Miniature Park" (literally translated) is a culture-based recreational area located in East Jakarta, Indonesia. It has an area of about 250 acres (1.0 km2). The park is a synopsis of Indonesian culture, with virtually all aspects of daily life in Indonesia's 26 (in 1975) provinces encapsulated in separate pavilions with the collections of Indonesian architecture, clothing, dances and traditions are all depicted impeccably. Apart from that, there is a lake with a miniature of the archipelago in the middle of it, cable cars, museums, Keong Emas Imax cinema, a theater called the Theatre of My Homeland (Theater Tanah Airku) and other recreational facilities which make TMII one of the most popular tourist destinations in the city.[1]
Since 2007 Taman Mini Indonesia Indah launched new logo with branding slogan Pesona Indonesia ("Indonesian Charm")

History

The idea of presenting Indonesia in a small scale was conceived by former Indonesian first lady, Siti Hartinah, better known as Tien Suharto. It came about at a convention on 8 Cendana Street at March 13, 1970. Through this recreational site, she hoped to cultivate national pride in more Indonesian people.[1] A project called "Indonesian Miniature Project" was started by Harapan Kita Foundation in 1972. The concept of this culture-based recreational area was inspired by Indonesia's unparalled natural riches and local folk diversity.
The iconic golden snail at Taman Mini Indonesia Indah

Characteristics

TMII was originally located on a public area of 145 ha, as farms and fields. Later, the team was able to convert these fields into a suitable location for the construction. The topography of TMII is rather hilly, consistent with what the builders required. The team claimed the advantage of utilizing this uneven terrain was the ability to create interesting and diverse landscapes and enclosures, as well as reflecting the various characteristics of the Indonesian environment.[1]
Parts of TMII

Venues of Indonesian Provinces

Since each Indonesian province maintains its own unique and distinct cultures, shelters, attire and dialects, TMII built a model of each of the houses from Indonesian provinces. TMII attempted not only to reconstruct the homes of the various provinces, but also to create a realistic model of the environment and shelters of the various people of Indonesia.[2] The venues, which are situated around the main lake in a similar fashion to the different islands of the Indonesian archipelago, are thematically divided into six areas in respect to the main islands of Indonesia; Java, Sumatra, Kalimantan (Borneo), Sulawesi, the Lesser Sunda Islands, Maluku and Papua. Each pavilions featured in typical vernacular Indonesian architecture of each provinces. Examples of Indonesian traditional vernacular houses are: Joglo and Omah Kudus Javanese houses of Central Java and Yogyakarta pavilion; Minang Rumah Gadang of West Sumatra pavilion; Malay houses of Jambi and Riau provinces; Torajan Tongkonan and Bugis house of South Sulawesi pavilion; and Balinese house compound with intricately carved Candi Bentar split gate and Kori Agung gate.
It also displays various traditional costumes, wedding costumes, dance costumes, also ethnography artifacts such as weapons and daily tools, models of traditional architecture are in display to describes the way of life of its people. Each provinces pavilions also equipped with small stage, amphitheatre or auditorium for traditional dance performances, traditional music performances or traditional ceremonies that usually held in Sundays. Some of these pavilions also equipped with cafeterias featuring traditional Indonesian cuisines and also souvenir shops offering various handicrafts, t-shirts and souvenirs.
Since 1975 until 2000s, the original design of TMII consist of a model of the houses from the 27 provinces of Indonesia, including East Timor. But after the secession of East Timor from Indonesia in 2002, the East Timor pavilion changed its status to become the Museum of East Timor. Also since Indonesia now consist of 33 provinces, currently the new province pavilions of Bangka Belitung, Banten, West Sulawesi, North Maluku, Gorontalo, and West Papua is being built in northeast part of the park.
After the recognition of Indonesian Chinese culture as the integral part of Indonesian culture in 2000, the new Indonesian Chinese pavilion and a Confucian temple was built within the park.

Religious Buildings

The religious buildings of several official faiths is meant to showcase the inter-faiths tolerance and religious harmony of Indonesia. The religious buildings are:
West Sumatra pavilion in TMII

Gardens and Parks

There are about ten gardens spread within TMII complex, but most are located primarily on the north and northeast side of the main lake:
  • Orchid Garden
  • Medicinal herbs Garden
  • Cactus Garden
  • Jasmine Garden
  • Keong Emas (Golden Snail) Flower Garden
  • Fresh Water Aquarium
  • Bekisar (a type of rooster) Garden
  • Bird Park
  • Taman Ria Atmaja Park, stage and music performances
  • Taman Budaya Tionghoa Indonesia, an Indonesian Chinese cultural park (under construction)
  • Reptile Park in Komodo Zoological Museum compound. A fully grown Komodo dragon (Varanus komodoensis) nicknamed Bima resides in the reptile park near the eastern gate, which you can pet and take pictures with for Rp.5,000 ($0.60).
Spherical cage Bird Park

Technological Centre

Pusat peragaan Iptek or Science and Technology Display Centre is under coordination of Research and Technology Ministry. At the end of 2011 has 15 sites with about 300 science tools and visited by 341,000 visitor in a year. The sites are Robotic, Electric and Magnet, Mechanics, Mathematics, etc.[4]

Museums

There are fourteen museums at TMII:
  • Indonesia Museum
  • Purna Bhakti Pertiwi Museum
  • Soldier Museum
  • Indonesian stamps Museum
  • Pusaka (Heirloom) Museum
  • Transportation Museum
  • Museum Electricity & New Energy Museum
  • Telecommunication Museum
  • Penerangan Museum
  • Sports Museum
  • Asmat Museum
  • Komodo Zoological Museum and Reptile Park
  • Insects Museum
  • Research & Technology Information Centre
  • Oil & Gas Museum
  • East Timor Museum (former East Timor province pavilion)



The Tumpeng style Purna Bhakti Pertiwi Museum displaying artworks and souvenirs collections of Suharto
The Balinese style Indonesia Museum

Theatres

  • Keong Emas (Golden Snail) Imax Theater
  • Tanah Airku Theater
  • 4D Theater

Monuments, Halls, Buildings and other Exhibits

  • Kala Makara main gates
  • Flower clock
  • Tugu Api Pancasila, the main monument, an obelisk celebrating Pancasila
  • Baluwerti, a twin gate with relief of Indonesian history on its wall
  • Pendopo Agung Sasono Utomo (Grand Hall), the main building in Javanese Joglo style
  • Sasono Utomo, exhibition hall
  • Sasono Langen Budoyo, indoor stage and theater
  • Sasono Manganti
  • Sasana Kriya handicraft center
  • Park Management Office
  • Cokot Sculpture, a display of wooden sculptures by Cokot, a famous Balinese artist
  • The Miniature of Borobudur
  • APEC Memorial Monument and Garden
  • Non Alignment Nations Friendship Monument and Garden
  • The Miniature of Indonesian Archipelago on central lake
  • Indonesian Archipelago Plaza and Stage
  • Jati Taminah, a remnant of a large teak tree
  • Kayu Gede (large wood), the display of large tree trunk

Rides

  • Skylift Indonesia cable car
  • Aeromovel Indonesia, a wind powered people mover
  • Mini train around the park
  • Boat ride on Indonesian archipelago lake
  • Swan paddle boat on Indonesian archipelago lake
  • Bicycle rent ride
  • Car ride around the area
Wind powered Aeromovel people mover ride around the park

Recreation facilities

  • Istana Anak-Anak Indonesia (The Castle of Indonesian Children)
  • Taman Among Putro kiddy rides park
  • Desa Seni dan Kerajinan handicraft center
  • Rare books market
  • Snowbay Waterpark swimmingpool
  • Telaga Mina fishing pond
  • Warna Alam outbound camp
Istana Anak-anak Indonesia

Lodgings

  • Desa Wisata hostel
  • Graha Wisata Remaja youth hostel

Restaurants












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