Beach cities - Barcelona.

Barcelona  is the capital city of the autonomous community of Catalonia in Spain and the country's second largest city, with a population of 1.6 million within its administrative limits. Its urban area extends beyond the administrative city limits with a population of around 4.5 million people, being the sixth-most populous urban area in the European Union after Paris, London, Madrid, the Ruhr area and Milan. About five million people live in the Barcelona metropolitan area. It is the largest metropolis on the Mediterranean Sea, located on the coast between the mouths of the rivers Llobregat and Besòs, and bounded to the west by the Serra de Collserola mountain range, the tallest peak of which is 512 metres (1,680 ft) high.

Founded as a Roman city, in the Middle Ages Barcelona became the capital of the County of Barcelona. After merging with the Kingdom of Aragon, Barcelona continued to be an important city in the Crown of Aragon. Besieged several times during its history, Barcelona has a rich cultural heritage and is today an important cultural centre and a major tourist destination. Particularly renowned are the architectural works of Antoni Gaudí and Lluís Domènech i Montaner, which have been designated UNESCO World Heritage Sites. The headquarters of the Union for the Mediterranean is located in Barcelona. The city is known for hosting the 1992 Summer Olympics as well as world-class conferences and expositions and also many international sport tournaments.

Barcelona is one of the world's leading tourist, economic, trade fair and cultural centres, and its influence in commerce, education, entertainment, media, fashion, science, and the arts all contribute to its status as one of the world's major global cities. It is a major cultural and economic centre in southwestern Europe, 24th in the world (before Zürich, after Frankfurt) and a financial centre. In 2008 it was the fourth most economically powerful city by GDP in the European Union and 35th in the world with GDP amounting to €177 billion. In 2012 Barcelona had a GDP of $170 billion; it is leading Spain in both employment rate and GDP per capita change. In 2009 the city was ranked Europe's third and one of the world's most successful as a city brand. In the same year the city was ranked Europe's fourth best city for business and fastest improving European city, with growth improved by 17% per year, but it has since been in a full recession with declines in both employment and GDP per capita, with some recent signs of the beginning of an economic recovery. Since 2011 Barcelona is a leading smart city in Europe.Barcelona is a transport hub with the Port of Barcelona being one of Europe's principal seaports and busiest European passenger port, an international airport, Barcelona–El Prat Airport, which handles above 35 million passengers per year,an extensive motorway network and a high-speed rail line with a link to France and the rest of Europe.

The name Barcelona comes from the ancient Iberian Barkeno, attested in an ancient coin inscription in Iberian script as Barkeno in Levantine Iberian script.

During the Middle Ages, the city was variously known as Barchinona, Barçalona, Barchelonaa, and Barchenona.

Some sources say that the city may have been named after the Carthaginian general Hamilcar Barca, who was supposed to have founded the city in the 3rd century BC.

Barcelona's name is usually abbreviated as 'Barna'. Foreigners often erroneously abbreviate Barcelona as 'Barça', the popular name of Barcelona football club. Spaniards also use 'BCN', often written 'Bcn' or 'bcn', which actually corresponds to the IATA airport code of the Barcelona-El Prat Airport. The city is also referred to as the Ciutat Comtal in Catalan, and Ciudad Condal in Spanish, owing to its past as the seat of the Count of Barcelona.

The origin of the earliest settlement at the site of present-day Barcelona is unclear. Around the actual neighborhood of Raval have been found remains of an early settlement, including different tombs and a hut from 5.500 BC. The founding of Barcelona is the subject of two different legends. The first attributes the founding of the city to the mythological Hercules. The second legend attributes the foundation of the city directly to the historical Carthaginian Hamilcar Barca, father of Hannibal, who named the city Barcino after his family in the 3rd century BC.


In about 15 BC, the Romans redrew the town as a castrum (Roman military camp) centred on the "Mons Taber", a little hill near the contemporary city hall (Plaça de Sant Jaume). Under the Romans, it was a colony with the surname of Faventia, or, in full, Colonia Faventia Julia Augusta Pia Barcino or Colonia Julia Augusta Faventia Paterna Barcino. Pomponius Mela mentions it among the small towns of the district, probably as it was eclipsed by its neighbour Tarraco (modern Tarragona), but it may be gathered from later writers that it gradually grew in wealth and consequence, favoured as it was with a beautiful situation and an excellent harbour. It enjoyed immunity from imperial burdens. The city minted its own coins; some from the era of Galba survive.


mportant Roman vestiges are displayed in Plaça del Rei underground, as a part of the Barcelona City History Museum MUHBA; the typically Roman grid plan is still visible today in the layout of the historical centre, the Barri Gòtic (Gothic Quarter). Some remaining fragments of the Roman walls have been incorporated into the cathedral. The cathedral, also known as the Basilica La Seu, is said to have been founded in 343. The city was conquered by the Visigoths in the early 5th century, becoming for a few years the capital of all Hispania. After being conquered by the Arabs in the early 8th century, it was conquered in 801 by Charlemagne's son Louis, who made Barcelona the seat of the Carolingian "Hispanic March" (Marca Hispanica), a buffer zone ruled by the Count of Barcelona.

The Counts of Barcelona became increasingly independent and expanded their territory to include all of Catalonia, although on 6 July 985, Barcelona was sacked by the army of Almanzor. The sack was so traumatic that most of Barcelona's population was either killed or enslaved. In 1137, Aragon and the County of Barcelona merged in dynastic union by the marriage of Ramon Berenguer IV and Petronilla of Aragon, their titles finally borne by only one person when their son Alfonso II of Aragon ascended to the throne in 1162. His territories were later to be known as the Crown of Aragon, which conquered many overseas possessions and ruled the western Mediterranean Sea with outlying territories in Naples and Sicily and as far as Athens in the 13th century. The forging of a dynastic link between the Crowns of Aragon and Castile marked the beginning of Barcelona's decline. The Bank of Barcelona, probably the oldest public bank in Europe, was established by the city magistrates in 1401. It originated from necessities of the state, as did the Bank of Venice (1402) and the Bank of Genoa (1407).



The marriage of Ferdinand II of Aragon and Isabella I of Castile in 1469, united the two royal lines. Madrid became the centre of political power whilst the colonisation of the Americas reduced the financial importance (at least in relative terms) of Mediterranean trade. Barcelona was a center of Catalan separatism, including the Catalan Revolt (1640–52) against Philip IV of Spain. The great plague of 1650–1654 halved the city's population.

In the 18th century, a fortress was built at Montjuïc that overlooked the harbour. In 1794, this fortress was used by the French astronomer Pierre François André Méchain for observations relating to a survey stretching to Dunkirk that provided the official basis of the measurement of a metre. The definitive metre bar, manufactured from platinum, was presented to the French legislative assembly on 22 June 1799. Much of Barcelona was negatively affected by the Napoleonic wars, but the start of industrialization saw the fortunes of the province improve.

During the Spanish Civil War, the city, and Catalonia in general, were resolutely Republican. Many enterprises and public services were "collectivised" by the CNT and UGT unions. As the power of the Republican government and the Generalitat diminished, much of the city was under the effective control of anarchist groups. The anarchists lost control of the city to their own allies, the Communists and official government troops, after the street fighting of the Barcelona May Days. The fall of the city on 26 January 1939, caused a mass exodus of civilians who fled to the French border. The resistance of Barcelona to Franco's coup d'état was to have lasting effects after the defeat of the Republican government. The autonomous institutions of Catalonia were abolished, and the use of the Catalan language in public life was suppressed. Barcelona remained the second largest city in Spain, at the heart of a region which was relatively industrialised and prosperous, despite the devastation of the civil war. The result was a large-scale immigration from poorer regions of Spain (particularly Andalusia, Murcia and Galicia), which in turn led to rapid urbanisation. The city gained vitality in 1992 when it hosted the Olympic games.

Barcelona is located on the northeast coast of the Iberian Peninsula, facing the Mediterranean Sea, on a plain approximately 5 km (3 mi) wide limited by the mountain range of Collserola, the Llobregat river to the southwest and the Besòs river to the north.This plain covers an area of 170 km2 (66 sq mi), of which 101 km2 (39.0 sq mi) are occupied by the city itself. It is 120 kilometres (75 miles) south of the Pyrenees and the Catalan border with France.

Tibidabo, 512 m (1,680 ft) high, offers striking views over the city and is topped by the 288.4 m (946.2 ft) Torre de Collserola, a telecommunications tower that is visible from most of the city. Barcelona is peppered with small hills, most of them urbanised, that gave their name to the neighbourhoods built upon them, such as Carmel (267 m), Putget (181 m) and Rovira (261 m). The escarpment of Montjuïc (173 m), situated to the southeast, overlooks the harbour and is topped by Montjuïc castle, a fortress built in the 17–18th centuries to control the city as a replacement for the Ciutadella. Today, the fortress is a museum and Montjuïc is home to several sporting and cultural venues, as well as Barcelona's biggest park and gardens.

The city borders on the municipalities of Santa Coloma de Gramenet and Sant Adrià de Besòs to the north; the Mediterranean Sea to the east; El Prat de Llobregat and L'Hospitalet de Llobregat to the south; and Sant Feliu de Llobregat, Sant Just Desvern, Esplugues de Llobregat, Sant Cugat del Vallès, and Montcada i Reixac to the west. The municipality includes two small sparsely-inhabited exclaves to the north-west.


Barcelona has a Mediterranean climate (Köppen climate classification: Csa),with mild, humid winters and warm, dry summers.

Its average annual temperature is 20 °C (68 °F) during the day and 11 °C (52 °F) at night. The average annual temperature of the sea is about 18 °C (64 °F). In the coldest month – January, the temperature typically ranges from 7 to 17 °C (45 to 63 °F) during the day, 2 to 10 °C (36 to 50 °F) at night and the average sea temperature is 13 °C (55 °F).In the warmest month – August, the typical temperature ranges from 25 to 31 °C (77 to 88 °F) during the day, about 20 °C (68 °F) at night and the average sea temperature is 25 °C (77 °F). Generally – the summer / "holiday" season lasts about six months, from May to October. Two months – April and November – are transitional; sometimes the temperature exceeds 20 °C (68 °F), with an average temperature of 17–18 °C (63–64 °F) during the day and 8–9 °C (46–48 °F) at night. December, January and February are the coldest months, with average temperatures around 14 °C (57 °F) during the day and 5 °C (41 °F) at night. Large fluctuations in temperature are rare, particularly in the summer months.

Barcelona averages several rainy days per month (= 1 mm), and annual average relative humidity is 72%, ranging from 69% in July to 75% in October. Sunshine duration is 2,524 hours per year, from 138 (average 4.5 hours of sunshine a day) in December to 310 (average 10 hours of sunshine a day) in July.


he Barri Gòtic (Catalan for "Gothic Quarter") is the centre of the old city of Barcelona. Many of the buildings date from medieval times, some from as far back as the Roman settlement of Barcelona. Catalan modernista architecture (related to the movement known as Art Nouveau in the rest of Europe), developed between 1885 and 1950 and left an important legacy in Barcelona. Several of these buildings are World Heritage Sites. Especially remarkable is the work of architect Antoni Gaudí, which can be seen throughout the city. His best-known work is the immense but still unfinished church of the Sagrada Família, which has been under construction since 1882, and is still financed by private donations. As of 2007, completion is planned for 2026.

Barcelona was also home to Mies van der Rohe's Barcelona Pavilion. Designed in 1929 for the International Exposition for Germany, it is an iconic building that came to symbolize modern architecture as the embodiment of van der Rohe's aphorisms "less is more" and "God is in the details." The Barcelona pavilion was intended as a temporary structure, and was torn down in 1930 less than a year after it was constructed. A modern re-creation by Spanish architects now stands in Barcelona, however, constructed in 1986.

Barcelona won the 1999 RIBA Royal Gold Medal for its architecture, the first (and as of 2012, only) time that the winner has been a city, and not an individual architect.

Historic buildings and monuments
    Minor basilica of Sagrada Família, the international symbol of Barcelona
    Palau de la Música Catalana and Hospital de Sant Pau, designed by Lluís Domènech i Montaner, included in the UNESCO Heritage List in 1997.
    Works by Antoni Gaudí, including Park Güell, Palau Güell, Casa Milà (La Pedrera), Casa Vicens, Sagrada Família (Nativity façade and crypt), Casa Batlló, Crypt in Colonia Güell. The first three works were inscribed as a World Heritage Site in 1984. The other four were added as extensions to the site in 2005.
    The Cathedral of the Holy Cross and St. Eulalia (Gothic)
    Gothic basilica of Santa Maria del Mar
    Gothic basilica of Santa Maria del Pi
    Romanesque church of Sant Pau del Camp
    Palau Reial Major, medieval residence of the sovereign Counts of Barcelona, later Kings of Aragon
    The Royal Shipyard (gothic)
    Monastery of Pedralbes (gothic)
    The Columbus Monument
    The Arc de Triomf, a triumphal arch built for entrance to 1888 Barcelona Universal Exposition.
    Expiatory church of the Sacred Heart of Jesus on the summit of Tibidabo.
Museums,Parks, beaches.

Barcelona beach was listed as number one in a list of the top ten city beaches in the world according to National Geographic and Discovery Channel.Barcelona contains seven beaches, totalling 4.5 kilometres (3 miles) (2.8 mi) of coastline. Sant Sebastià, Barceloneta and Somorrostro beaches, both 1,100 m (3,610 ft) in length, are the largest, oldest and the most-frequented beaches in Barcelona. The Olympic Harbour separates them from the other city beaches: Nova Icària, Bogatell, Mar Bella, Nova Mar Bella and Llevant. These beaches (ranging from 400 to 640 m/1,300 to 2,100 ft) were opened as a result of the city restructuring to host the 1992 Summer Olympics, when a great number of industrial buildings were demolished. At present, the beach sand is artificially replenished given that storms regularly remove large quantities of material. The 2004 Universal Forum of Cultures left the city a large concrete bathing zone on the eastmost part of the city's coastline.

Batu Caves - Malaysia

Batu Caves is a limestone hill that has a series of caves and cave temples in the Gombak district, 13 kilometres (8 mi) north of Kuala Lumpur, Malaysia. It takes its name from the Sungai Batu or Batu River, which flows past the hill. Batu Caves is also the name of the nearby village.

The cave is one of the most popular Hindu shrines outside India, and is dedicated to Lord Murugan. It is the focal point of Hindu festival of Thaipusam in Malaysia.

The limestone forming Batu Caves is said to be around 400 million years old. Some of the cave entrances were used as shelters by the indigenous Temuan people (a tribe of Orang Asli).

As early as 1860, Chinese settlers began excavating guano for fertilising their vegetable patches. However, they became famous only after the limestone hills were recorded by colonial authorities including Daly and Syers as well as American Naturalist, William Hornaday in 1878.

Batu Caves was promoted as a place of worship by K. Thamboosamy Pillai, an Indian trader. He was inspired by the 'vel'-shaped entrance of the main cave and was inspired to dedicate a temple to Lord Murugan within the caves. In 1890, Pillai, who also founded the Sri Mahamariamman Temple, Kuala Lumpur, installed the murti (consecrated statue) of Sri Murugan Swami in what is today known as the Temple Cave. Since 1892, the Thaipusam festival in the Tamil month of Thai (which falls in late January/early February) has been celebrated there.

Wooden steps up to the Temple Cave were built in 1920 and have since been replaced by 272 concrete steps. Of the various cave temples that comprise the site, the largest and best known is the Temple Cave, so named because it houses several Hindu shrines beneath its high vaulted ceiling.

Rising almost 100 m above the ground, the Batu Caves temple complex consists of three main caves and a few smaller ones. The biggest, referred to as Cathedral Cave or Temple Cave, has a very high ceiling and features ornate Hindu shrines. To reach it, visitors must climb a steep flight of 272 steps.

At the base of the hill are two more cave temples, Art Gallery Cave and Museum Cave, both of which are full of Hindu statues and paintings. This complex was renovated and opened as the Cave Villa in 2008. Many of the shrines relate the story of Lord Murugan's victory over the demon Soorapadam. An audio tour is available to visitors.

The Ramayana Cave is situated to the extreme left as one faces the sheer wall of the hill. On the way to the Ramayana Cave, there is a 50-foot (15 m) tall statue of Hanuman and a temple dedicated to Lord Hanuman, devotee and aide of Lord Rama. The consecration ceremony of the temple was held in November 2001.

The Ramayana Cave depicts the story of Rama in a chronicle manner along the irregular walls of the cave.

A 42.7-metre (140 ft) high statue of Lord Murugan was unveiled in January 2006, having taken 3 years to construct. It is the tallest Lord Murugan statue in the world.

Batu Malai Sri Murugan Temple is managed by the Board of Management of Sri Maha Mariamman Temple Devasthanam, which also manages the Sri Mahamariamman Temple, Kuala Lumpur and the Kortumalai Pillaiyar Temple. It also performs the role of Hindu Religious Consultant to the Government of Malaysia in determining the Hindu yearly calendar.


There are various undeveloped caves which contain a diverse range of cave fauna, including some unique species, such as Liphistiidae spiders and Eonycteris and fruit bats. The site is also well known for its numerous macaques, which visitors feed — sometimes involuntarily. These monkeys may also pose a biting hazard to tourists (especially small children) as they can be quite territorial.

Below the Temple Cave is the Dark Cave, with rock formations and a number of animals found nowhere else. It is a two-kilometer network of relatively untouched caverns. Stalactites jutting from the cave's ceiling and stalagmites rising from the floor form intricate formations such as cave curtains, flow stones, cave pearls and scallops which took thousands of years to form.

In order to maintain the cave's ecology, access is restricted. The Malaysian Nature Society organises regular educational and adventure trips to the Dark Caves.


Batu Caves is also the centre of rock climbing development in Malaysia for the past 10 years. Batu Caves offers more than 160 climbing routes. The routes are scattered all around the side of Batu Caves, which is made up of limestone hills rising to 150 m. These climbing routes are easily accessed, as most crags start from ground level. These climbing routes often start from the North Eastern side of the cave complex whereas the staircase and temple entrance faces South. This North eastern area is known as the Damai caves. Abseiling and spelunking trips can be organised with some local adventure companies.


The Batu Caves serve as the focus of the Hindu community's yearly Thaipusam (Tamil: தைபூசம்) festival. They have become a pilgrimage site not only for Malaysian Hindus, but Hindus worldwide, from countries such as India, Australia and Singapore.

A procession begins in the wee hours of the morning on Thaipusam from the Sri Mahamariamman Temple, Kuala Lumpur leading up to Batu Caves as a religious undertaking to Lord Muruga lasting eight hours. Devotees carry containers containing milk as offering to Lord Murugan either by hand or in huge decorated carriers on their shoulders called 'kavadi'.

The kavadi may be simple wooden arched semi-circular supports holding a carrier foisted with brass or clay pots of milk or huge, heavy ones which may rise up to two metres, built of bowed metal frames which hold long skewers, the sharpened end of which pierce the skin of the bearers torso. The kavadi is decorated with flowers and peacock feathers imported from India. Some kavadi may weigh as much as a hundred kilograms.

After bathing in the nearby Sungai Batu (Rocky River), the devotees make their way to the Temple Cave and climb the flights of stairs to the temple in the cave. Devotees use the wider centre staircase while worshippers and onlookers throng up and down those balustrades on either side.

When the kavadi bearer arrives at the foot of the 272-step stairway leading up to the Temple Cave, the devotee has to make the arduous climb.

Priests attend to the kavadi bearers. Consecrated ash is sprinkled over the hooks and skewers piercing the devotees' flesh before they are removed. No blood is shed during the piercing and removal.

Housing development began since 1970 with housing estates such as Taman Batu Caves, Taman Selayang, Taman Amaniah, Taman Sri Selayang, and Taman Medan Batu Caves.

In the last decade, the surrounding area has changed from a small village to industrial estates and new housing and shops. There is also an elevated flyover over the highway. A new 515-million-ringgit KTM Komuter rail extension from Sentul to Batu Caves began operations in July 2010, serving the rebuilt Batu Caves Komuter station.

On 1 January 2011, during the Thaipusam festival, it was announced that a cable car would be built for the following year's festival. It would cost around 10 million ringgit

Batu Caves is easily reached by Komuter train using the Batu Caves-Port Klang Route, costing RM 2 for a one-way journey from KL Sentral. Batu Caves may also be reached by bus 11/11d from Bangkok Bank Terminus (Near to Puduraya Terminus) or bus U6 from Titiwangsa.

Waitomo Glowworm Caves - New Zealand.

The Waitomo Glowworm Caves attraction is a cave at Waitomo on the North Island of New Zealand, known for its population of glowworms, Arachnocampa luminosa. This species is found exclusively in New Zealand. They are around the size of an average mosquito. This cave is part of the Waitomo Caves system that includes the Ruakuri Cave and the Aranui Cave.

The attraction has a modern visitor centre at the entrance, largely designed in wood. There are organized tours that include a boat ride under the glowworms.

The name "Waitomo" comes from the Maori words wai, water and tomo, hole or shaft. The local Maori people had known about the caves for quite some time before the local Maori Chief Tane Tinorau and an English surveyor, Fred Mace, did an extensive exploration in 1887. Their exploration was conducted with candlelight on a raft going into the cave where the stream goes underground. This is now the exit for the cave. As they began their journey, they came across the Glowworm Grotto and were amazed by the twinkling glow coming from the ceiling. As they travelled further into the cave by poling themselves towards an embankment, they were also astounded by the limestone formations. These formations surrounded them in all shapes and sizes.

They returned many times after and Chief Tane independently discovered the upper level entrance to the cave, which is now the current entrance. Tane Tinorau and his wife Huti, by 1889, had opened the cave to visitors and were leading groups for a small fee. The administration of the cave was taken over by the government in 1906 after there was an escalation in vandalism. In 1910, the Waitomo Caves Hotel was built to house the many visitors.

In 1989, the land and cave were returned to the descendants of Chief Tane Tinorau and Huti. They now receive a percentage of the cave’s revenue and are involved in the management and development of the cave. These descendants encompass many of the employees of the caves today.

Geological and volcanic activity has created around 300 known limestone caves in the Waitomo region over the last 30 million years.

The limestone formations in the Waitomo Glowworm Caves were formed when the region was still under the ocean about 30 million years ago. The limestone is composed of fossilized corals, seashells, fish skeletons, and many small marine organisms on the sea beds. Over millions of years, these fossilized rocks have been layered upon each other and compressed to create limestone and within the Waitomo region the limestone can be over 200 m thick.

The caves began to form when earth movement caused the hard limestone to bend and buckle under the ocean and rise above the sea floor. As the rock was exposed to air, it separated and created cracks and weaknesses that allowed for water to flow through them dissolving the limestone and over millions of years large caves were formed.

The stalactites, stalagmites, and other cave formations grew from water dripping from the ceiling or flowing over the walls and leaving behind limestone deposits. The stalagmites form upward from the floor while the stalactites form from the ceiling. When these formations connect they are called pillars or columns and if they twist around each other they are called helicti. These cave decorations take millions of years to form given that the average stalactite grows one cubic centimetre every 100 years.

The most renowned animal in the cave is the glowworm Arachnocampa luminosa. There are several small underwater lakes that were created by freshwater creeks or brooks.

The walls of the caves are covered with a variety of fungi including the cave flower (a distant relation to the genus Pleurotus) that is actually a mushroom-like fungus. The most common animals in the caves are insects. This includes albino cave ants, giant crickets, and of course the glowworms.


The glowworms of the Waitomo Glowworm Caves are closely guarded by a Scientific Advisory Group. This group has automated equipment that continually monitors the air quality especially the carbon dioxide levels, rock and air temperature, and humidity. Data from this equipment is carefully analyzed by specialist staff. The advisory group uses the information to establish how the cave should be managed. They determine if and when air flow patterns should be changed and how many people are allowed to visit the caves each day.


The guided tour through the Waitomo Glowworm Caves brings the visitor through three different levels and begins at the top level of the cave and the Catacombs. The levels are linked by the Tomo, which is a 16 m vertical shaft made of limestone. The second level is called the Banquet Chamber. This level is where early visitors stopped to eat and there is evidence of this in the smoke on the ceiling of the chamber. From here it may be possible to link back to the upper level to see the largest formation called the Pipe Organ but on busy days this area is closed to the public because the build-up of carbon monoxide may be hazardous.

The third and final level goes down into the Cathedral, demonstration platform, and the jetty. The Cathedral is an enclosed area with rough surfaces, now paved, and is about 18 m high, giving it good acoustics. A number of famous singers and choirs have performed here including Dame Kiri Te Kanawa.

The tour concludes with a boat ride through the Glowworm Grotto. The boat takes the visitor onto the underground Waitomo River where the only light comes from the tiny glowworms creating a sky of living lights.

The Waitomo Glowworm Caves are located in the southern Waikato region of the North Island of New Zealand, 12 km northwest of Te Kuiti. This cave is about 2 hours south of Auckland, 1 hour south of Hamilton, and 2 hours west of Rotorua by car. The directions to the Caves are to exit State Highway 3 onto Waitomo Caves Road and to continue on the road for about 8 km.

Pandavleni Caves

Pandavleni Caves

Pandu Leni (also known as Trirashmi Caves and other variations) (Leni is Marathi word for caves), are a group of 24 caves carved between the 3rd century BC and the 2nd century AD, representing the Hinayana Buddhist caves and has nothing to do with the characters of Mahabharata (the Pandavas). Most of the caves are Viharas except for the 18th cave which is a Chaitya. The location of the caves is a holy Buddhist site and is located about 8 km south of Nashik, Maharashtra, India.

Caves

The caves were carved out from the 4th century BC till the 12th century AD as abodes for the idols of the local kings. The caves lodge idols of Buddha and Bodhisattva. Some caves are intricately connected by stone-cut ladders that join them to the other caves. Steps lead to the caves from the bottom of the hill. The peak of the Pandavleni is also accessible by trekking of about 20 mins but the path is well built with steps.

Some of the caves are large and contain numerous chambers - these rock-cut caves served as a viharas or monasteries for the disciples to meet and hear sermons. They contain interesting sculptures. One of the vihara caves is older and finer in sculptural detail and is thought to be nearly as old as the Karla Cave near Lonavala. Another cave (cave No. 18) is a Chaitya and is similar in age to the Karla Cave and has a particularly elaborate facade.

The site has an excellent ancient water management system and skillfully chiseled out of solid rock are several attractive water tanks.


The caves can be traced back up to 3rd century BC. Out of the twenty-four caves, two caves are a major attraction - the main cave which is the Chaitya (prayer hall) has a beautiful Stupa; the second one is cave no. 10 which is complete in all structural as well inscriptions. Both the caves have carvings and inscriptions also. The caves are facing eastwards. So it is recommended to visit the caves early morning as in sunlight the beauty of carvings is enhanced.

The caves were called Pundru which in Pali language means "yellow ochre color". This is because the caves were the residence of Buddhist monks who wore "the chivara or the yellow robes". Later on, the word Pundru changed to Pandu Caves (as per Ancient Monuments Act 26 May 1909). Decades later people started calling it Pandav Caves - a misnomer which is used for every cave in India.

The various inscriptions confirm that Nashik in that period was ruled by 3 kings – The Kshatrapas, The Satavahanas and The Abhirs. It seems there was always a conflict between Satavahanas and the Kshatrapas over supremacy. However, all the 3 kings fully supported Buddhism though they were not Buddhist in real sense. The inscriptions also confirm that apart from the kings, local merchants, landlords too supported and donated huge sums for the development of these caves.

The inscriptions of cave no.10 reveal that in 105-106 BC, Ksatrapas defeated the Satavahanas after which Kshatrap Nahapana’s son-in-law and Dinika’s son- Usabhdatta donated 3000 gold coins for this cave as well as for the food and clothing of the monks. Usabhdatta’s wife (Nahapana’s daughter), Dakshmitra also donated one cave for the Buddhist monks.
Attractions

Inscriptions in caves 3, 11, 12, 13, 14, 15, 19 and 20 are legible. Cave 15 - 'Sri Yajna Vihar' inscription mentions Sri Yajna Satkarni, the last Satvahana King who ruled over the western Maharashtra. Similar inscription in cave 3 at Kanheri. This means probably the cave was carved during the beginning of the 3rd century AD. Other inscriptions note the names Bhattapalika, Gautamiputra Satkarni, Vashishthiputra Pulumavi of the Satvahanas and two of the Kshatrapas, Dakshamitra and Ushavadant. Cave 10 - 'Nahapan Vihar' is spacious with 16 rooms.

Since the caves were inhibited by the Mahayana as well as the Hinayana sects of Buddhism, one can see a nice confluence of structural and carvings.


Routes

The caves are located high in the mountains of Trirashmi. Some caves are intricately connected by stone-cut ladders that join them to the other caves. Steps lead to the caves from the bottom of the hill. The peak of the Trirashmi Caves is also accessible by trekking of about 20 mins but the path is treacherous and dangerous. Its good destination where the person feel relax.

Mullu caves

Gunung Mulu National Park near Miri, Sarawak, Malaysian Borneo, is a UNESCO World Heritage Site that encompasses caves and karst formations in a mountainous equatorial rainforest setting. The park is famous for its caves and the expeditions that have been mounted to explore them and their surrounding rainforest, most notably the Royal Geographical Society Expedition of 1977–1978, which saw over 100 scientists in the field for 15 months. This initiated a series of over 20 expeditions now drawn together as the Mulu Caves Project

The national park is named after Mount Mulu, the second highest mountain in Sarawak.


Geology and landforms

Gunung Mulu National Park is famous for its limestone karst formations. Features include enormous caves, vast cave networks, rock pinnacles, cliffs and gorges. Mount Mulu is a sandstone mountain rising to 2,376 m (7,795 ft).

Gunung Mulu National Park has the largest known natural chamber or room – Sarawak Chamber, found in Gua Nasib Bagus. It is 700 m (2,300 ft)) long, 396 m (1,299 ft) wide and at least 70 m (230 ft) high. It has been said that the chamber is so big that it could accommodate about 40 Boeing 747s, without overlapping their wings. The nearby Deer Cave is one of the largest single cave passages in the world.

Other notable caves in this area are Benarat Cavern, Cave of the Winds, and Clearwater Cave, the 8th longest cave in the world (May 2014) and believed to be the largest cave in the world by volume at 30,347,540 m3 (1.071713×109 cu ft).

Mulu's limestones belong to the Melinau Formation and their age is between 17 and 40 million years (Late Eocene to Early Miocene).

Stratigraphically below the limestones, and forming the highest peaks in the south east sector of the Park including Gunung Mulu, lies the Mulu Formation (shales and sandstones). The age of these rocks is between 40 and 90 million years (Late Cretaceous to Late Eocene).

Fauna
Eight species of hornbill have been spotted in Mulu including the rhinoceros hornbill (Buceros rhinoceros) which is featured on Sarawak's state emblem, the white-crowned hornbill (Berenicornis/Aceros comatus) and the helmeted hornbill (Buceros vigil) with its large solid casque (an enlargement on the bill).

Twenty seven species of bat have been recorded in Mulu. Deer Cave in the southern limestone hills of the park is home to an enormous colony of Wrinkle-lipped bats (Tadarida plicata). The bats exit the cave almost every evening in search of food in a spectacular exodus. A huge mound of guano in the cave is evidence of the size of the bat colony that roosts in the cave's high ceilings.

Mulu's mammals also include the bearded pig Sus barbatus, the moonrat Echinosorex gymnurus, shrews, the Bornean tarsier Tarsius bancanus, the long-tailed macaque Macaca fascicularis, gibbons, squirrels, and three types of deer including the small barking deer and mouse deer. The small Malaysian sun bear Helarctos malayanus, which is the only bear known in South-East Asia, has also been identified in Gunung Mulu National Park.

A number of amphibians are only known from the Gunung Mulu National Park, including squat frog Calluella flava and stream toad Ansonia torrentis.


Flora

Gunung Mulu National Park contains a large number of plant species, including flowering plants, trees, and fungi. Geology, soil types and topography have given rise to a rich tapestry of plant zones and types. On Gunung Mulu itself these include lowland mixed dipterocarp forest, lower montane forest, mossy or upper montane forest and summit zone vegetation on the highest peaks. On the limestones there is lowland limestone forest as well as lower and upper montane limestone forest. Other plant communities dominate the alluvial plains, including kerangas (tropical heath forest) and peatswamp forest.

Access

Mulu National Park is a very remote access area; the only practical way of getting to and from it is by air, through Mulu Airport. There are flights between Mulu Airport and Miri (daily), Kuching (Tuesdays, Thursdays and Saturdays) and Kota Kinabalu (Tuesdays, Thursdays and Saturdays) on MASwings. Alternatively, it is possible to travel by river from Miri, which is about 100 km away, using a riverboat, then a chartered long boat, which in total takes around 12 hours. Before the opening of the airport and the opening of a helipad in 1991, this was the only way to reach the national park.

Excursions to Mulu continues to retain the sense of adventure associated with its original exploration through the provision of adventure caving and other adventure activities. The primary focus, however, has shifted to the promotion of an awareness of the significance of the park and its environment through the provision of ecotourism activities that foster understanding and appreciation of the parks values. Accommodation is available onsite at Gunung Mulu National Park headquarters, as well as at the Royal Mulu Resort and across the Melinau River at Benarat Inn also known as Benarat Lodge. Homestays offered by locals, and other typically cheaper lodging are available across the river.