Monday, October 26, 2009

Travel to Switzerland



Switzerland is HEAVEN ON EARTH...once you step on this paradise; you wonder God has unleashed all its splendor and beauty on Switzerland. Millions of visitors from all over the world travel to Switzerland for- honeymoon, traveling, family holidays, sports, and relaxation. Scores of Bollywood songs have been shot in the beautiful locales of Swiss Alps. This place is multilingual and fusion of German, French, Italian forms strong culture.

Switzerland is the tourist friendly country in Europe, the trains, funicular railways, cable cars, and ski lifts offers tourist to visit the scenic places and inaccessible areas on tours.
Still wondering where to go in Switzerland? We give you sneak peak into the most popular destination to travel to Switzerland.




Board on flights to Switzerland and visit its stunningly beautiful and largest city, Zurich. We give you necessary information on cheap flights to Zurich and hotels for trouble-free accommodation. Circles around in the northern end by beautiful Lake Zurich the city robust snow-clad peaks, 19th century mansions, historic buildings. One of the best shopping destinations in the world, it boasts world famous opera, restaurants, museums, and galleries.

Our online site provides you details of flights in Switzerland, to reach your dream destinations in a hassle free way. "Interlaken," the oldest and most popular place adorned with the gorgeous views of Swiss Alps, majestic Jungfrau Mountain, it provides plethora of fun activities for adventure lovers like rock climbing, paragliding, downhill skiing, snowboarding, swimming, and sailing; "Bern" is travelers dream! Cobbled streets, sandstone arcaded buildings, street fountains, and medieval architecture, Zytglogge medieval clock and garden of roses; "Geneva" the seat of several United Nations Organizations famous sites are Jet d'Eau fountain, Flower Clock; Fashionable Zearmatt covered with enchanting beauty of Snowfall; lovely city of "Vevey" on the northern shore of Lake Geneva is famous for its vineyards.



Flightstoswitzerland.com is at your service! Giving you details of all cheap flights to Switzerland ...and unravel the picturesque locations; grandeur to the most beautiful county in this entire world.

Wednesday, August 5, 2009

Mohasthangarh is one of the main attractions in north Bengal

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Mahasthangarh (Bengali: Môhasthangôṛ) is the earliest urban archaeological site so far discovered in Bangladesh. The village Mahasthan in Shibganj thana of Bogra District contains the remains of an ancient city which was called Pundranagara or Paundravardhanapura in the territory of Pundravardhana. A limestone slab bearing six lines in Prakrit in Brahmi script, discovered in 1931, dates Mahasthangarh to at least the 3rd century BC. The fortified area was in use till the 18th century AD.

Together with the ancient and mediaeval ruins, the mazhar (holy tomb) of Shah Sultan Balkhi Mahisawar built at site of a Hindu temple is located at Mahasthangarh. He was a dervish (holy person devoted to Islam) of royal lineage who came to the Mahasthangarh area, with the objective of spreading Islam among non-Muslims. He converted the people of the area to Islam and settled there.



Etymology

Mahasthan means a place that has excellent sanctity and garh means fort. Mahasthan was first mentioned in a Sanskrit text of the 13th century entitled Vallalcharita. It is also mentioned in an anonymous text Karatoya mahatmya,, circumstantially placed in 12th-13th century. The same text also mentions two more names to mean the same place – Pundrakshetra, land of the Pundras, and Pundranagara, city of the Pundras. In 1685, an administrative decree mentioned the place as Mastangarh, a mixture of Sanskrit and Persian meaning fortified place of an auspicious personage. Subsequent discoveries have confirmed that the earlier name was Pundranagara or Paundravardhanapura, and that the present name of Mahasthangarh is of later origin.



Geography

Mahasthangarh, the ancient capital of Pundravardhana is located at 25.50°N 81.50°E, 11 km (7 mi) north of Bogra on the Bogra-Rangpur highway, with a feeder road (running along the eastern side of the ramparts of the citadel for 1.5 km) leading to Jahajghata and site museum. Buses are available for Bogra from Dhaka and take 4½ hours for the journey via Bangabandhu Jamuna Bridge across the Jamuna River. Buses are available from Bogra to Mahasthangarh. Rickshaws are available for local movement. Hired transport is available at Dhaka/ Bogra. Accommodation is available at Bogra.[8] When travelling in a hired car, one can return to Dhaka the same day, unless somebody has a plan to visit Somapura Mahavihara at Paharpur in the district of Naogaon and other places, or engage in a detailed study.

It is believed that the location for the city in the area was decided upon because it is one of the highest areas in Bangladesh. The land in the region is almost 36 m above sea level, whereas Dhaka, the capital of Bangladesh, is around 6 m above sea level. Another reason for choosing this place was the position and size of the Karatoya, which seemed to be as wide as the sea.

Mahasthangarh stands on the red soil of the Barind Tract which is slightly elevated within the largely alluvium area. The elevation of 15 to 25 metres above the surrounding areas makes it a relatively flood free physiographic unit.

Discovery

Several personalities contributed to the discovery and identification of the ruins at Mahasthangarh. F.Buchanan Hamilton was the first to locate and visit Mahasthangarh in 1808, C.J.O’Donnell, E.V.Westmacott, and Baveridge followed. Alexander Cunningham was the first to identify the place as the capital of Pundravardhana. He visited the site in 1889.


Citadel

The citadel (see map alongside), the fortified heart of the ancient city, is rectangular in plan, measuring roughly 1.523 km long from north to south, and 1.371 km from east to west, with high and wide ramparts in all its wings. The Karatoya, once a mighty river but now a small stream, flows on its east.

Till the 1920s, when excavations started, the inside of the citadel was higher than the surrounding areas by over 4 metres and was dotted with several straggling elevated pieces of land. The rampart looked like a jungle clad mud rampart with forced openings at several points. The rampart was 11-13 metres higher than the surrounding area. At its south-east corner stood a mazhar (holy tomb). A later day mosque (built in 1718-19) was also there.

At present there are several mounds and structural vestiges inside the fortifications. Of these a few of note are: Jiat Kunda (well possessing life giving power), Mankalir Dhap (place consecrated to Mankali), Parasuramer Basgriha (palace of a king named Parasuram), Bairagir Bhita (palace of a female anchorite), Khodar Pathar Bhita (place of stone bestowed by God), and Munir Ghon (a bastion). There are some gateways at different points: Kata Duar (in the north), Dorab Shah Toran (in the east), Burir Fatak (in the south), and Tamra Dawaza (in the west) At the north-eastern corner there is a flight of steps (a later addition) that goes by the name of Jahajghata. A little beyond Jahajghata and on the banks of the Karatoya is Govinda Bhita (a temple dedicated to Govinda). In front of it is the site museum, displaying some of the representative findings. Beside it is a rest house.



Suburb of the citadel


Besides the fortified area, there are around a hundred mounds spread over an area with a radius of 9 km. (See map alongside).


Excavated mounds

1. Govinda Bhita, a temple close to the north-eastern corner of the fortified area. 2. Khulnar Dhap, a temple 1 km to the west of the fortified area. 3. Mangalkot, a temple 400 m to the south of Khulnar Dhap. 4. Godaibari Dhap, a temple 1 km to the south of Khulnar Dhap. 5. Totaram Panditer Dhap, a vihara (monstery) 4 km to the north-west of the fortified area. 6. Narapatir Dhap (Vasu Vihara), a group of monasteries 1 km to the north-west of Totaram Panditer Dhap (said to be the place where Po-shipo Vihara mentioned by Xuanzang (Hieun Tsang) was located). 7. Gokul Medh (Lakhindarer Basar Ghar), a temple 3 km to the south of the fortified area (it is a small distance off the road from Bogra to Mahasthangarh). 8. Skander Dhap, a temple 2 km to the south-east of Gokul Medh.


Major unexcavated mounds

1. Siladevir Ghat. 2. Chunaru Dighi Dhap. 3. Kaibilki Dhap. 4. Juraintala. 5. Parasuramer Sabhabati. 6. Balai Dhap. 7. Prachir Dhibi. 8. Kanchir Hari Dhibi. 9. Lahonar Dhap. 10. Khujar Dhap. 11. Dosatina Dhap. 12. Dhaniker Dhap. 13. Madarir Dargah. 14. Bismardana Dhibi. 15. Malinar Dhap. 16. Malpukuria Dhap. 17. Yogir Dhap. 18. Padmavatir Dhap. 19. Kanai Dhap. 20. Dulu Majhir Bhita. 21. Padma Devir Bhita. 22. Rastala Dhap. 23. Sasitala Dhap. 24. Dhanbandhar Dhap. 25. Chander Dhap. 26. Sindinath Dhap. 27. Salibahan Rajar Kacharibari Dhipi. 28. Kancher Angina. 29. Mangalnather Dhap. 30. ChhotoTengra/ Babur Dhap/ Kethar Dhap. 31. Baro Tengra/ Sanyasir Dhap.


Excavated mounds

1. Govinda Bhita, a temple close to the north-eastern corner of the fortified area. 2. Khulnar Dhap, a temple 1 km to the west of the fortified area. 3. Mangalkot, a temple 400 m to the south of Khulnar Dhap. 4. Godaibari Dhap, a temple 1 km to the south of Khulnar Dhap. 5. Totaram Panditer Dhap, a vihara (monstery) 4 km to the north-west of the fortified area. 6. Narapatir Dhap (Vasu Vihara), a group of monasteries 1 km to the north-west of Totaram Panditer Dhap (said to be the place where Po-shipo Vihara mentioned by Xuanzang (Hieun Tsang) was located). 7. Gokul Medh (Lakhindarer Basar Ghar), a temple 3 km to the south of the fortified area (it is a small distance off the road from Bogra to Mahasthangarh). 8. Skander Dhap, a temple 2 km to the south-east of Gokul Medh.


Major unexcavated mounds

1. Siladevir Ghat. 2. Chunaru Dighi Dhap. 3. Kaibilki Dhap. 4. Juraintala. 5. Parasuramer Sabhabati. 6. Balai Dhap. 7. Prachir Dhibi. 8. Kanchir Hari Dhibi. 9. Lahonar Dhap. 10. Khujar Dhap. 11. Dosatina Dhap. 12. Dhaniker Dhap. 13. Madarir Dargah. 14. Bismardana Dhibi. 15. Malinar Dhap. 16. Malpukuria Dhap. 17. Yogir Dhap. 18. Padmavatir Dhap. 19. Kanai Dhap. 20. Dulu Majhir Bhita. 21. Padma Devir Bhita. 22. Rastala Dhap. 23. Sasitala Dhap. 24. Dhanbandhar Dhap. 25. Chander Dhap. 26. Sindinath Dhap. 27. Salibahan Rajar Kacharibari Dhipi. 28. Kancher Angina. 29. Mangalnather Dhap. 30. ChhotoTengra/ Babur Dhap/ Kethar Dhap. 31. Baro Tengra/ Sanyasir Dhap.



Excavations

Systematic archaeological excavation of Mahasthangarh was first started in 1928-29 under the guidance of K.N.Dikshit of the Archaeological Survey of India. The areas around Jahajghata, Munir Ghon and Bairagir Bhita were explored. Excavation was resumed in 1934-36 at Bairagir Bhita and Govinda Bhita. Excavation was carried out in 1960s around the Mazhar, Parasuramer Prasad, Mankalir Dhap, Jiat Kunda and in a part of the northern rampart. In the next phase excavation was carried out sporadically in parts of the east and north ramparts but the final report is yet to be published. In the period 1992-98 excavation was conducted in the area lying between Bairagir Bhita and the gateway exposed in 1991 as a Bangla-Franco joint venture, which is now in its second phase with excavation around the mazhar in the western side of the citadel.


Movable antiquities

The excavations have led to the recovery of a large number of items, a few of which are listed here.

Inscriptions: A 4.4 cm x 5.7 cm lime stone slab bearing six lines in Prakrit in Brahmi script, discovered accidentally by a day labourer in 1931 was an important find. The text appears to be a royal order of Magadh, possibly during the rule of Asoka. It dates the antiquity of Mahasthangarh to 3rd century BC. An Arabic inscriptional slab of 1300-1301 discovered in 1911-12 mentions the erection of a tomb in honour of Numar Khan, who was a Meer-e-Vahar (lieutenant of the naval fleet). A Persian inscriptional slab of 1718-19 records the construction of a mosque during the reign of the Mughal emperor Farrukhshiyar.

Coins: Silver punch marked coins are datable to a period between the 4th century BC and the 1st-2nd century AD. Some uninscribed copper cast coins have been found. Two Gupta period coins have been reported from a nearby village named Vamanpara. A number of coins belonging to the sultans of 14th-15th century and British East India Company have been found.

Ceramics: Mostly represented by a vast number of shards.

Sculpture: A 5th century Buddha stone sculpture recovered from Vasu Vihara, a Lokesvara stone sculpture showing blending of Visnu and Avalokitsvara, salvaged from neighbouring Namuja village, a number sand stone door-frames, pillars and lintels (datable to 5th-12th century), numerous Buddha bronze sculpture datable to 10th-11th century, a terracotta Surya discovered at Mankalir Bhita, and numerous other pieces.

Terracotta Plaques: A number of terracotta plaques have been discovered.

Many of these are on display in the site museum, which is open Sunday to Thursday summer:10 am to 6 pm, winter:9 am to 5 pm. Recess:1-2 pm, Friday recess is from 12.30 to 2.30, opens at 9 am in summer, other timings same. Summer timings 1 April to 30 September, winter timings 1 October to 30 March.[2] Books on Mahasthangarh and other archaeological sites in Bangladesh (in Bengali and English) are available at the ticket counter for the site museum.


Highlights of some excavated sites


Inside the citadel

Bairagir Bhita: Constructed/ reconstructed in four periods: 4th-5th century AD, 6th-7th century, 9th-10th century, and 11th century. Excavations have revealed impoverished base ruins resembling temples. Two sculptured sand stone pillars have been recovered.

Khodarpathar Bhita: Some pieces of stone carved with transcendent Buddha along with devotees in anjali (kneeling with folded hands) recovered.

Parasuramer Prasad: Contains remains of three occupation periods - 8th century AD findings include stone Visnupatta of Pala period, 15th- 16th century findings include some glazed shreds of Muslim origin, and the third period has revealed two coins of the British East India Company issued in 1835 and 1853.

Mankalir Dhap: terracotta plaques, bronze Ganesha, bronze Garuda etc were discovered. Base ruins of a 15-domed mosque (15th-16th century) was revealed.

Bangla-Franco joint venture: Excavations have revealed 18 archaeological layers, ranging from 5th century BC to 12th century AD, till virgin soil at a depth of around 17 m.


Outside the citadel

Govinda Bhita: Situated 185 m north-east of Jahajghata and opposite the site museum. Remains dated from 3rd century BC to 15th century AD. Base remains of two temples have been exposed.

Totaram Panditer Dhap: Situated in the village Vihara, about 6 km north-west of the ciradel. Structural remains of a damaged monastery have been exposed.

Narapatir Dhap: Situated in the village Basu Vihara, 1.5 km north-west of Totaram Panditer Dhap. Base remains of two monasteries and a temple have been exposed. Cunningham identified this place as the one visited by Xuanzang (Hiuen Tsang) in the 7th century AD.

Gokul Medh: Also known as Behular Basar Ghar or Lakshindarer Medh, situated in the village Gokul, 3 km to the south of the citadel, off the Bogra-Rangpur road, connected by a narrow motorable road about 1 km. Excavations in 1934-36 revealed a terraced podium with 172 rectangular blind cells. It is dated 6th-7th century. Local mythology associates it with legendary Lakshmindara-Behula. The village Gokul also has several other mound Kansr Dhap has been excavated.

Skandher Dhap: Situated in village Baghopara on the Bogra-Rangpur road, 3.5 km to the south of the citadel, a sandstone Kartika was found and structural vestiges of a damaged building were revealed. It is believed to be the remains of Skandha Mandira (temple consecrated to Kartika), mentioned in Karatoya mahatmya, as well as Kalhan’s Rajatarangin, written in 1149-50. There also are references to Skandhnagara as a suburb of Pundranagara. Baghopara village has three other mounds.

Khulnar Dhap: Situated in village Chenghispur, 700 m west of the north-west corner of the citadel has revealed remains of a temple. The mound is named after Khullana, wife of Chand Sadagar.

From the present findings it can be deduced that there was a city called Pundravardhana at Mahasthangarh with a vast suburb around it, on all sides except the east, where the once mighty Karatoya used to flow. It is evident that the suburbs of Pundravardhana extended at least to Baghopara on the south-west, Gokul on the south, Vamanpara on the west, and Sekendrabad on the north. However, the plan of the city and much of its history are still to be revealed.

Bhimer Jangal This well-known embankment starts from the north-east corner of Bogra town and proceeds northwards for about 30 miles to a marshy place called Damukdaher bit, under police station Govindaganj (Rangpur District) and it is said, goes oil to Ghoraghat. It is made of the red earth of the locality and retains at places even now a height of 20 feet above the level of the country. There is a break ill it of over three miles from Daulatpur (north west of Mahasthan-garh) to Hazaradighi (south-west, of it). About a mile south of Hazradighi. the stream Subil approaches the jangal and runs alongside it down to Bogra town.

Some people think that the Subil is a moat formed by digging the earth for the jangal but as there is no embankment on the northern reach of the Subil (now called the Ato nala. which merges in the Kalidaha bil; north of Mahasthan-garh O'Donnell was probably right in saying that the Subil represents the western of the two branches into which the Karatoya divided above Mahasthan.

On the Bogra-Hazradighi section of thee jaligal, there are two cross embankments running down to the Karatoya, about 2 miles and 4 miles respectively north of Bogra town and there is a diagonal embankment connecting these cross bonds and then running along the Karatoya until it meets the main embankment near Bogra.

This jangal or embankment appears to have been of a military character, thrown up to protect the country on its east. The break roar Mahasthan may be due to the embankment having been washed away or to the existence of natural protection by the bit.

The Bhima to whom the embankment is ascribed may be the ascribed may be the Kaivarta chief of the eleventh century who according to the Ramcharitam ruled over Varendra in succession to his father Rudraka and uncle Divyoka, who had ousted king Mahipala II of the Pala, dynasty. Bhima in his turn was defeated in battle and billed by Ramapala. Mahipala's son.

Jogir Bhaban South west of Bagtahali (beyond Chak Bariapara) and some 3 miles west of the khetlal road is a settlement of the Natha sect of Saiva sannyasis, known as Yogir-bhavan, forming the eastern section of Arora village. An account of this settlement is given by Beveridge, J.:1.S.T., 1878; p. 94. It occupies about so, bighas of land and forms the headquarters of the sect. of which there are branches at Yogigopha and Gorakh-kui, both in the Dinajpur District, the .former in its south-west part some 5 miles west of Paharpur, J.A.S.B.1875, p. 189, and the latter in its north-west part some 4 miles west of Nekmardan.

The shrines at Yogir-bhavan are situated in the south-west corner of an en¬closure or-math. One of them called Dharmma-dungi, bears a brick inscription, reading scrvva-siddha sana 1148 Sri Suphala ……. (the year =1741 A.D.). 'In front of it is another shrine called `Gadighar,' where a fire is kept burn at all hours. Outside the enclose are four temples, dedicated respectively to Kalabhai¬rava, Sarvamangala Durga and Gorakshanatha. The Kalabhairava temple contains a diva linga and bears a brick inscription reading Sri Ramasiddha sana 1173 sala (=1766 A.D.) ample Sri Jayanatha Nara-Narayana. The Sarva¬mangala temple contains three images of Hara-Gauri, one of Mahishamardini, a fragment of an Ashta-matrika slab, a fragment of a three-faced female figure probably Ushnishavijava (Sadhanamala; II. pl .XIV) and a four-armed female figure playing on a vina (evidently Sarasvati, but worshipped here as Sarva¬ mangala). Over the entrance is a brick inscription reading 1089 Meher Natha sadaka sri Abhirama Mehetara (the year =1681 A.D.). In the Durga temple is a stone image of Chamunda, and in the Gorakshanatha one, a Siva lihga. There are three brick built samadhis near the latter temple.

Arora South-west of the Dadhisugar and standing on the Masandighi, in Arora village; is Salvan Rajar bari referred to under Baghahali. This Silvan may possibly be the same as king Salavahan, son of Sahila-deva of the Chamba inscription who won the title of Kari-ghata-varsha (= hunjara-ghata-varsha ?) (R.C. Majumdar, vange kambojadhikara,' vanga-rani,Chaitara, 1330.B.S.p. 251, ind.Ant,XVII.pp.7–13). Beveridge refers to this mound in JA.S.B., 1878, p 95.

This name of Sahila seems, to occur again in Sahiladitya lakshmam in v. 10 of the Silimpllr inscription (Ep. Ind,XIII, p. 291). If this identification is correct, then the word kaunjanraghatacarshcna in the Bangarh stone inscription (Gauda-raja-mala, p. 35) is really the title or virudha of the Gudapati of the Kumboja family and not the date of the inscription.

Teghar North of Chandnia hat the road skirts the bil and comes to Teghar village Which juts out into the bil 'Near about here are several mounds; such as Naras¬patir dhap. Kacher Angina (or glazed courtyard, a term applied to many ruins in these parts) etc. The biggest of these mounds, Mangal-nather dhap, (Fig. 6) is situated close to the point, from which a road branches off to Bihar. It is said that terra-cotta plaques as well as stone images were found at this site, but were all consigned to the neighbouring dighi.

Rojakpur Proceeding westward along the road from Gokul to Haripur, we pass into the western arm of the latter village, already referred to. and meet the Bogra¬ Khetlal road near the Chandnia hat. West of Haripur and south of the Somrai bil is the village of Rojakpur, into which, as already stated, the elevated ground from Chandnia hat extends. On this ground are two mounds called respectively Chandbhita . (probably refering to the Manasa legend) and Dhanbhandar. A little further west is aher mound called Singhinath Dhap.

Mathura East of Bumanpara and extending up to the garh on the east and the Kalidaha bill on the north, is the village of Mathura, in Which there are several tank and on a ridge overlooking the Gilatala moat, two mounds called two mounds called Parasuramer Sabhabati and Yogir Dhap.


Anecdote

There is a local legend that Shah Sultan Balkhi Mahisawar arrived at Pundravardhana in the garb of a fakir (mystic holy pedlar of Islamic philosophy) riding a fish. (Mahisawar is Sanskrit-Persian word meaning a person who rides a fish). He came from Balkh in Afghanistan with a retinue. The period of his arrival is variably put at 5th century AD, 11th century AD and 17th century AD. At that time there was a king named Parasuram with his seat and palace in Mahasthangarh. Mahisawar requested Parasuram for a piece of land to spread his prayer mat on which he could pray. The request was granted but the prayer mat started expanding as soon as it was laid on the ground. When the prayer mat reached the area around the palace bewildered Parasuram declared war. In the beginning the battle seemed to be favouring Parasuram. A scavenger Harapala informed Mahisawar that it was difficult to defeat the royal troops because of the pool called Jiat Kunda. A dead soldier bathed in the waters of Jiat Kunda came back to life. On knowing this Mahisawar asked a kite to drop a piece of beef in Jiat Kunda. When this was done, the pool lost its powers. The royal troops were on the verge of defeat. The commander of the royal troops, Chilhan, with a large number of his followers, went over to Mahisawar. Thereafter Parasuram and many members of the royal family committed suicide. There are many variations of this anecdote, some of which are sold in Bengali booklets in and around Mahasthangarh/Pundravardhana.


Some antiquity comparisons

Mahasthangarh dates back to at least 3rd century BC and is acknowledged as the earliest city-site so far discovered in Bangladesh. Somapura Mahavihara at Paharpur in Naogaon District was once the biggest Buddhist monastery south of the Himalayas. It dates from the 8th century AD. Mainamati ruins in Comilla District date back to 6th-13th centuries AD. In neighbouring West Bengal, the ruins of Pandu Rajar Dhibi on the banks of the Ajay River in Bardhaman district date back to 2,000 BC. However, this recent archaeological discovery has not yet been properly studied by outside experts and specialists in this field, and as such the historical value of many of the statements must be considered as uncertain. The ruins at Chandraketugarh in 24 Parganas South and Rajbadidanga in Murshidabad district date back to the early years of the Christian era.

Tuesday, July 14, 2009

Niger-Congo languages

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The Niger-Congo languages constitute one of the world's major language families, and Africa's largest in terms of geographical area, number of speakers, and number of distinct languages. They may constitute the world's largest language family in terms of distinct languages, although this question is complicated by ambiguity about what constitutes a distinct language. Most of the most widely spoken indigenous languages of Subsaharan Africa belong to this group. A common property of many Niger-Congo languages is the use of a noun class system.

Classification history


Early classifications

Niger-Congo as it is known today was only gradually recognized as a unity. In early classifications of African languages, one of the principal criteria used to distinguish different groupings was the languages' use of prefixes to classify nouns, or the lack thereof. A major advance came with the work of Koelle, who in his 1854 Polyglotta Africana attempted a careful classification, the groupings of which in quite a number of cases correspond to modern groupings. An early sketch of the extent of Niger-Congo as one language family can be found in Koelle's observation, echoed in Bleek (1856), that the Atlantic languages used prefixes just like many Southern African languages. Subsequent work of Bleek, and some decades later the comparative work of Meinhof, solidly established Bantu as a linguistic unit.

In many cases, wider classifications employed a blend of typological and racial criteria. Thus, Friedrich Müller, in his ambitious classification (1876-88), separated the 'Negro' and Bantu languages. Likewise, the Africanist Lepsius considered Bantu to be of African origin, and many 'Mixed Negro languages' as products of an encounter between Bantu and intruding Asiatic languages.

In this period a relation between Bantu and languages with Bantu-like (but less complete) noun class systems began to emerge. Some authors saw the latter as languages which had not yet completely evolved to full Bantu status, whereas others regarded them as languages which had partly lost original features still found in Bantu. The Bantuist Meinhof made a major distinction between Bantu and a 'Semi-Bantu' group which according to him was originally of the unrelated Sudanic stock.



Westermann, Greenberg and beyond




Westermann's 1911 Die Sudansprachen. Eine sprachvergleichende Studie laid the basis for much of Niger-Congo.

Westermann, a pupil of Meinhof, set out to establish the internal classification of the then Sudanic languages. In a 1911 work he established a basic division between 'East' and 'West'. A historical reconstruction of West Sudanic was published in 1927, and in his 1935 'Charakter und Einteilung der Sudansprachen' he conclusively established the relationship between Bantu and West Sudanic.

Joseph Greenberg took Westermann's work as a starting-point for his own classification. In a series of articles published between 1949 and 1954, he argued that Westermann's 'West Sudanic' and Bantu formed a single genetic family, which he named Niger-Congo; that Bantu constituted a subgroup of the Benue-Congo branch; that Adamawa-Eastern, previously not considered to be related, was another member of this family; and that Fula belonged to the West Atlantic languages. Just before these articles were collected in final book form (The Languages of Africa) in 1963, he amended his classification by adding Kordofanian as a branch co-ordinate with Niger-Congo as a whole; consequently, the family was renamed Niger-Kordofanian. Greenberg's work, though initially greeted with scepticism, became the prevailing view among scholars.

Bennet and Sterk (1977) presented an internal reclassification based on lexicostatistics that laid the foundation for the regrouping in Bendor-Samuel (1989). Kordofanian was thought to be one of several primary branches rather than being coordinate to the phylum as a whole, prompting re-introduction of the term 'Niger-Congo', which is in current use among linguists. Many classifications continue to place Kordofanian as the most distant branch, but mainly due to negative evidence (fewer lexical correspondences), rather than positive evidence that the other languages form a valid genealogical group. Likewise, Mande is often assumed to be the second-most distant branch based on its lack of the noun-class system prototypical of the Niger-Congo family. Other branches lacking any trace of the noun-class system are Dogon and Ijaw, whereas the Talodi branch of Kordofanian does have cognate noun classes, suggesting that Kordofanian is also not a valid group.


Niger-Congo and Nilo-Saharan

Over the years, several linguists have suggested a link between Niger-Congo and Nilo-Saharan, probably starting with Westermann's comparative work on the 'Sudanic' family in which 'Eastern Sudanic' (now classified as Nilo-Saharan) and 'Western Sudanic (now classified as Niger-Congo) were united. Gregersen (1972) proposed that Niger-Congo and Nilo-Saharan be united into a larger phylum which he termed Kongo-Saharan. His evidence was mainly based on the uncertainty in the classification of Songhay, morphological resemblances, and lexical similarities. A more recent proponent is Roger Blench (1995), who puts forward phonological, morphological and lexical evidence for uniting Niger-Congo and Nilo-Saharan in a Niger-Saharan phylum. Within Nilo-Saharan, Blench considers Niger-Congo to be most closely related to Central Sudanic. Most hypotheses uniting the two families have failed to generate much discussion.

Common features


Niger-Congo languages have a clear preference for open syllables of the type CV (Consonant Vowel). The typical word structure of Proto-Niger-Congo is thought to have been CVCV, a structure still attested in, for example, Bantu, Mande and Ijoid — in many other branches this structure has been reduced through phonological change. Verbs are composed of a root followed by one or more extensional suffixes. Nouns consist of a root originally preceded by a noun class prefix of (C)V- shape which is often eroded by phonological chang

Consonant and vowel systems

Reconstructions of the consonant system of several branches of Niger-Congo (Stewart for proto-Volta-Congo, Mukarovsky for his proto-West-Nigritic, roughly corresponding to Atlantic-Congo) have posited independently a regular phonological contrast between two classes of consonants. Pending more clarity as to the precise nature of this contrast it is commonly characterized as a contrast between 'fortis' and 'lenis' consonants. Five places of articulation are postulated for the consonant inventory of proto-Niger-Congo: labial, alveolar, palatal, velar, and labial-velar.

Many Niger-Congo languages show vowel harmony based on the feature [ATR] (advanced tongue root). In this type of vowel harmony, the position of the root of the tongue is the phonetic basis for the distinction between two harmonizing sets of vowels. In its fullest form, this type involves two classes, each of five vowels: [+ATR] /i, e, ə, o, u/ and [-ATR] /ɪ, ɛ, a, ɔ, ʊ/. Vowel inventories of this type are still found in some branches of Niger-Congo, for example in the Ghana Togo Mountain languages.[1] To date, many languages show reductions from this fuller system. The fact that ten vowels have been reconstructed for proto-Atlantic, proto-Ijoid and possibly proto-Volta-Congo leads Williamson (1989:23) to the hypothesis that the original vowel inventory of Niger-Congo was a full ten-vowel system. On the other hand, Stewart in recent comparative work reconstructs a seven vowel system for his proto-Potou-Akanic-Bantu.

Monday, July 13, 2009

The Copper Canyon

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Mexico's Copper Canyon (also known as Barranca del Cobre or Sierra Tarahumara) offers some of North America's most dramatic landscapes. Although often referred to as the Copper Canyon, it is actually a series of six massive gorges that cover some 25,000 square miles of northwestern Mexico. It is rugged territory where most roads remain unpaved and elevations range from 7,500 to 9,500 (with a few peaks reaching 12,000 feet).

In addition to the splendors of the landscape, a visit to the Copper Canyon offers a chance to see the Tarahumara Indians, who (more than many of Mexico's indigenous cultures) have been very successful in maintaining their centuries-old way of life. Many still live in caves deep in impassable canyons. The Tarahumara, who call themselves Ramámuri ("people who run"), retreated deep into the canyons several centuries ago to escape the Spanish onslaught of disease, slavery and violence. Because the territory was so rugged, and they were able to adapt to it so well, the Tarahumara have largely escaped assimilation into modern Mexico.

What was once ruggedly impassable territory, however, has become somewhat more accessible since 1961 with the completion of the Chihuahua-Pacifico railway that links Los Mochis (on the Pacific Coast in the Mexican state of Sinaloa) with the state and city of Chihuahua (in the central interior of Mexico's north). The railway is a remarkable feat of engineering. From sea level in Los Mochis, the train crosses 39 bridges and passes through 87 tunnels as it climbs to a maximum altitude of 8,056 feet (just east of Creel, near the Continental Divide), then descends into Chihuahua at 4,700 feet. For much of the 415 mile journey, especially between El Fuerte and Creel, the scenery is simply overwhelming. Deep canyons, rushing rivers, meadows of wildflowers and towering peaks greet the traveler around almost every curve in the tracks. From El Fuerte to Creel is the most spectacular segment of the trip and visitors should make sure they pass through this area during daylight hours (which when the days are short means starting the journey in Los Mochis (or El Fuerte) and traveling east toward Chihuahua).

The first-class train is truly world-class, with air conditioned cars, comfortable reclining seats, large picture windows and an excellent dining car. Plus, since its Mexico where insurance regulations do not control every aspect of life, travelers can stand in the space between the cars and have views (and photo opportunities) unobstructed by glass. (But please, if you decide to ride between cars, don't fall out and ruin it for future travelers.)

Those who simply ride the train through the Copper Canyon will miss much of the area's allure. While the landscapes visible from the train and the 20 minute stopover in El Divisadero are certainly magnificent, there is so much more. One could easily spend a week here, visiting local villages, hiking, horseback riding and more. Our schedule was not so leisurely, but we did manage a stopover of two nights in Creel (the approximate midpoint of the journey), plus an overnight trip deep into the canyon to visit the old mining town of Batopilas on the canyon floor. Creel itself is a gritty logging town and the main commercial center for nearby villages. Brightly dressed Tarahumara women share the main street with local men wearing cowboy hats, tourist agencies, small hotels and all sorts of shops. But the real reason to stop over in Creel is its easy access to the splendors of the surrounding countryside.

If time permits, an overnight trip to Batopilas is highly recommended. The small town on the canyon floor was once a booming mining town, beginning in the 1740s. Legend has it that the cobblestone streets were once paved with silver. Eventually the mines played out and Batopilas began to decline. Today the streets are hardly paved at all, but the town retains a rundown charm that reminds the visitor just how far away the modern world can be. Several miles outside of Batopilas, in an area where one would expect to find only more of the same rugged wilderness, stands the Jesuit mission church of San Miguel de Satevo, built around 1760, and sometimes referred today as the "lost cathedral." Along the way, we also met a group of young Tarahumara children.

After our stopover in Creel and Batopilas, we re-boarded the train and continued east toward the city of Chihuahua. After crossing the Continental Divide, the Chihuahua-Pacifico ("Chepe") train travels through flat open plains and farmland. During our visit in late October, the days were growing shorter and much of this part of the journey was in darkness. Late in the evening, we arrived in Chihuahua. We flew back to Mexico City early the next morning and thus had only a quick view of Chihuahua itself.







GEOGRAPHY

You'll find a variety of climates. It can snow in the mountains while tropical temperatures reign in the valleys.

The average altitude here is 2,275 meters above sea level, while the highest point, Cerro del Mohinora, is 3,306 meters and the lowest point, at the confluence of the Septentrion and Chinipas Rivers, is around 220 meters. Note that the average rainfall in Copper Canyon is close to 15 inches per year. Most of the rainfall takes place during the months of July, August and September.

To journey into this rugged and isolated terrain with knowledge of its spectacular biodiversity and history is one of Mexico's best adventures. Carl Lumholtz explored the Sierra Madre and the Barranca de Sinforosa in 1892, and his well-documented adventures have inspired generations of canyon enthusiasts.

A trip into the canyons and the Sierra requires a good base of operations, such as the town of Creel, most travelers' hub of choice. Multiple-day treks are arranged by many of the hotels in Creel, though you can find independent guide services in any of the towns by asking hotel owners or visitors. There are numerous towns along the railroad and in the valley including Batopilas, Cusárare, Divisadero, Bauchivo and Cerocahui.



CANYON HISTORY

The barrancas are one of Mexico's youngest geological formations and the largest in North America. They were formed about 30-40 million years ago, during a period of intense volcanic activity in what is present day Northwestern Mexico. Thousands of volcanoes erupted, throwing lava and ash onto the surrounding plateau and creating the Sierra Madre Occidental.

The tectonic activity also created deep fractures in the earth's crust. Because the rocks are relatively soft, the rivers originating in the high Sierra cut deep canyons on their descent to the Gulf of Mexico. The canyons bear the names of these powerful rivers: Chinipas, Candameña, Urique, Tararecua, Batopilas and Verdes.

FLORA AND FAUNA

The Sierra is one of the most biologically rich areas in Mexico. One reason is that there are two distinct environmental climates - one in the mountains and on the plateaus, and a different one at the bottom of the canyons. This terrain includes snow-covered mountain peaks and subtropical forests in the canyons.

The canyons are home to 290 recorded bird species, 24 endemic and ten in danger of extinction, including the military macaw (Ara milittaris), the thick-billed parrot (Rhynchopsitta pachyrhyncha), and the eared trogon (Euptilotis noxenus).

Almost a third of Mexico's land mammals are found in the region, including the black bear (Ursus americanus), the puma (Felis concolor), and the Mexican wolf (Canis Lutus baileyi), which is in danger of extinction. Hunting has claimed many species. The grizzly bear is extinct and the wild turkey and deer are now rarely seen.

More than 3,500 vascular plants are found in the region. Among them are tropical and temperate species as well as hundreds of endemic species, including at least 60 wild relatives of major crops and more than 400 wild medicinal plants, an irreplaceable genetic legacy.

Most of these endemic plant species may be endangered by logging and overgrazing. Ironically, ethnobotanists now estimate that the forests are more valuable as extractive reserves for medicinal plants than for timber. The chuchupate plant, used as a blood thinner in both traditional and modern medicine, is worth thousands of dollars per acre in virgin pine forest, but it is sparse in most of the Sierra due to overharvesting and deforestation.

Mixed forests of Ponderosa pine and Douglas fir are found above 2,000 meters (6,500 feet), while juniper, piñon, and live oak are found at lower elevations from 500 to 1,500 meters (1,640 to 4,900 feet). Biologists have counted 15 species of pine and 25 of oak.

Unfortunately, the forests within the Sierra Tarahumara have been commercially logged for 100 years. The logging has been selective, and in many cases, the worst trees have been left in areas to regenerate new forest.
URIQUE CANYON

Urique Canyon is the deepest canyon in North America, and home to a Tarahumara settlement. Founded in 1690 along the banks of the meandering river, Urique was totally isolated until connected by a switchback mountain road in 1975.

SIERRA MADRE ALLIANCE

Copper Canyon does not have federal status as a national park or as a biosphere reserve, but plans and studies are underway. In February 1996, Mexico's Environmental Secretariat (SEMARNAP) announced its intention to form a 2.2 million-acre biosphere reserve in the Sierra. The Chihuahua City–based Sierra Madre Alliance will be responsible for planning approximately 750,000 acres of this reserve in the upper Río Fuerte watershed in the Sierra Tarahumara.

Randall Gingrich, Edwin Bustillos, and indigenous leaders from the Sierra formed the Sierra Madre Alliance in 1992. The mission of the Sierra Madre program is to return control of the forests to traditional indigenous communities and to facilitate sustainable ecosystem management.

The program supports indigenous communities suffering loss of land, destruction of forests, and human rights abuses in a region acknowledged to host the greatest biological diversity in North America. Tropical and temperate species intermix in a spectacular labyrinth of pine-forested highlands and tropical canyons. The native Tarahumara and Tepehuan are among the poorest and most traditional subsistence farmers in North America. Conservation, sustainable agriculture, and defense of basic human rights are inseparable for cultural survival.

We first featured the alliance in a 1999 Profile. For up-to-date info, consult their website.

VISITING?

LOCATION - The Copper Canyon is located in the state of Chihuahua.




TRANSPORTATION - The canyon is accessible from the Chihuahua al Pacífico Railroad, the end points being Los Mochis, Sinaloa and Chihuahua City, Chihuahua. From Chihuahua, you can take the train or bus to the town of Creel, which is the easiest hub for exploration of Copper Canyon country. Other towns on the railroad are developing tourism as well, particularly Divisidero, Bauchivo and Cerocahui.

Saturday, July 11, 2009

Glaciers, Fjords, and Mountains: Hiking New Zealand's South Island

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This may be the only place in the world where you can stand in a rainforest and gaze out through a mantle of giant ferns and hanging moss at a 200-foot thick, five-mile long river of ice directly below you. (If you were pitching a screenplay about the place, you'd call it "Hawaii meets Switzerland.") The South Island has eight national parks that encompass world-class glaciers, a chain of rugged snow-capped mountains where Sir Edmund Hillary trained for Everest, fjords that rate right up there with Norway and Patagonia, semi-tropical rainforest beaches, mirror-smooth lakes, tumbling whitewater rivers, as well as dozens of lesser but still spectacular mountain ranges that will keep a "tramper" (local argot for hiker) busy for a lifetime. All this in a place the size of Florida—with one-tenth of the population.

Hiking in New Zealand has a European flavor, with a broad network of well-maintained trails and huts. Some areas have an American flavor as well, with trails that meander through huge cattle and sheep stations (i.e. ranches) reminiscent of Montana. The famous five-day Milford Track is promoted as "The Most Beautiful Walk in the World," and it may well be, but there are a number of other less-known routes worthy of the name.

Practically Speaking
Tramping is a long tradition in New Zealand. Because of its well-established system of trails, substantial huts, and "bivvies" (small, rudimentary shelters), the South Island is ideal for independent tramping. Maps and guidebooks (in English, of course) are widely available, the trails are well maintained, and huts are spaced at one-day intervals along most major trails. Moreover, there are plenty of campgrounds along major roads for between-hike stays. It's quite possible to hike New Zealand on $20 a day in food, bus fare, and camping/hut fees.

More upscale accommodations are available, of course. Simple "motor camps"—modest motels with cooking facilities—run $30-$50 per night for two people. More elaborate lodges and B&Bs typically go for $50-$100 a night. A number of U.S. outfitters offer all-inclusive multi-day hiking tours of the South Island. Most run 10-16 days and cost from $160 to $250 per person per day. Local New Zealand outfitters run group walking/hiking trips as well, at about the same prices.

Be sure to take good rain gear. Except along the northern coast, rain is a normal part of any New Zealand hiking trip, although you will have beautiful sunny days as well. The prime hiking season is November through March, the Down Under summer. Be wary of January, the traditional Kiwi holiday month, when trails and huts can be