Nainital

The city of Nainital covers a total area of 11.73 km² (4.53 sq mi), and is located at 29.38°N 79.45°E / 29.38; 79.45,[6] at an average elevation of 2,084 metres (6,837 ft) above sea level. The slopes of the nearby mountains are most populated, with an altitude ranging from 1,940–2,100 m (6,360–6,890 ft). The highest point nearby is the Naina Peak, with an height of 2,619 m (8,593 ft). The city is located in the Kumaon foothills of the outer Himalayas at a distance of 285 km (177 mi) from the state capital Dehradun and 345 km (214 mi) from New Delhi, the capital of India.

Scenic view of the Nainital from Tallital, the lower end of the lake.

The city is set in a valley around the Nainital Lake - an eye-shaped lake, which is located at an altitude of 1,940 m (6,350 ft) from sea level. The lake is 1,433 m (1,567 yd) long and 463 m (506 yd) wide, and is approximately two miles in circumference.[7] The bed of the lake is at a depth of 85 m (93 yd) near Pashandevi, the deepest point of the lake. The lake is deduced to have been formed tectonically. Balia Nala, which is the main stream feeding the lake is along a fault line and the subsequent streams align parallel to major joints and faults. 26 major drains feed the lake including the 3 perennial drains.

Nainital is surrounded by the mountains of Ayarpata (2,344 m (7,689 ft)), Devpata (2,435 m (7,989 ft)), Hanibani (2,180 m (7,153 ft)), China (2,612 m (8,568 ft)), Alma (2,430 m (7,980 ft)), Ladiya Kanta (2,482 m (8,144 ft)) and Sher ka Danda (2,398 m (7,869 ft)).[7]

The Krol group of rocks, comprising slates, marls, sandstones, limestones and dolomites with a few small dykes intrusives, is the dominant geological formation of Nainital's surroundings, although, Nodules, laminae and stringers of phosphatic material, followed upward by the purple-green shales intercalated with muddy fine-grained sandstone and siltstone; recognised as the Tal Formation; are also prevalent. The region has a complex geological framework; the rocks are fragile and newly formed. The city is completely located in the catchment area of the Nainital lake, which has highly folded and faulted rocks due to polyphase deformation.

Landslides are a frequent occurrence in the hill slopes surrounding the lake, which are steep. The slopes are highly vulnerable to landslides and mass movement due to various geological and human factors. The first known landslip occurred in Nainital in 1866 on Alma hill, and in 1879 there was a larger one at the same spot. The greatest landslide in Nainital occurred on 18 September 1880, on the slope which rising from the north of the flats ends at Alma peak, and resulted in 151 people being buried under the debris.[8] Another heavy landslip occurred on 17 August 1898 outside the Nainital valley.[9]

Forest in Nainital after snowfall (2020)

Nainital experiences a subtropical highland climate (Cwb) according to Köppen–Geiger climate classification system as the city's climate is influenced by the elevation. The city is a bit dry during winter and very wet during summer due to South Asian monsoon system. The lowest precipitation total occurs in November with total 7.9 millimetres (0.31 in), while the highest precipitation total occurs in July with total 725 millimetres (28.5 in). Like most places in temperate region, Nainital has relatively cool summer. The hottest month is July with temperature ranging from 16.4 °C (61.5 °F) to 23.5 °C (74.3 °F), while the coldest month is January with temperature ranging from 1.7 °C (35.1 °F) to 10.7 °C (51.3 °F). The highest temperature ever recorded in Nainital was 30 °C (86 °F) recorded on 18 June 1972, while the lowest temperature was −5.6 °C (21.9 °F) recorded on 17 January 1953.[10]

The winter season in Nainital commences by mid-November and lasts till mid-March. The temperature gradually declines from the month of November onwards and January is the coldest month. Frost and mist are common features in the months of December and January. Occasionally widespread rainfall also occurs due to western disturbance, with snow occurring on peaks higher than 2000m. The winter rainfall is sometimes associated with cyclonic activities. The temperature, however, shows an increasing trend by the end of February or the first half of March. By mid-March, there is a progressive rise in temperature, which indicates the onset of the summer season. While days get slightly warmer; the nights continue to be cool. There is a constant increase in temperature during May and early June when the highest temperature is recorded. The months of March and April are also associated with the occurrence of hailstorms, which brings a short spell of cold.

The onset of the summer in the hills is relatively earlier than the plains and is also very lengthy and humid. The mean temperature in July and August goes down and humidity rises abruptly during this season. The monsoon usually begins by mid-May when the rain strikes and continue until mid-October. Nainital, due to its proximity to the outermost high ranges of the Himalaya, receives high annual rainfall. Generally, by mid-September, the monsoon gets weakened and rain occurs generally after long intervals. With the retreat of the monsoon, the winds blow in a reverse direction. The weather during the post-monsoon months is characterized by bright skies. It is in fact a transition between the rains and the winters and with reduced rainfall, the monthly temperature records a progressive decline till mid-January.

A Bear in the Pt. G B Pant High Altitude Zoo.

The areas around Nainital (in the middle Himalayan ranges up to 2,000 m (6,600 ft), a temperate zone), is rich in flora (typical temperate climate plants) and fauna.[12] The trees and bushes grown in the region (lake's basin) with their botanical and common Indian names (in parenthesis) are : Quercus incana Oak (Banj), Aesculus indica (Pangar or Horse chestnuts), Juglans regia (Akhrot or walnut), Populus ciliata (Hill Pipal, a sacred tree), Fraxinus micrantha (Ash tree or Angu), Platanus orientalis (Chinar), Rubus lasiocarpus (Hisalu), Rosa moschata (Kunj or Musk rose), Berberis asiatica (Kilmora), Cupressus torulosa (Surai or Himalayan cypress), Rhododendron arboreum (Buruns), Cedrus deodara (Deodar), Salix acmophylla (Weeping Willow), and Pinus (Pine).[12]

Several species of medicinal flora and horticulture plants have also been found in the lake. The Aquatic Macrophytic vegetation include Potamogeton pectinatus, Potamogeton crispus, Polygonum glabrum, Polygonum amphibium and Polygonum hydropiper (Water pepper).[12] The fishes found in the lake are generally carps Mahseer, and the mirror carp which breed several times during one spawning season during May to September. Two species of Mahaseer fish viz., Tor tor: The red finned mahseer and the Tor putitora: The yellow finned mahseer, a food fish which grows to varying sizes from 20 to 60 cm (7.87 to 23.62 inches) are found. Three species of Hill Trout are found in the lake: the Schizothorax sinuatus, Schizothorax richardsoni and Schizothorax plagiostornus. The imported fish bred in the lake is Mirror carp or Cyprinus carpio.[12] Gambusia affinis also called Mosquitofish has been introduced in the lake as a biocontrol measure to control Mosquito larvae.[12]

The Kumaon Hills came under British rule after the Anglo-Nepalese War (1814–16). The hill station town of Naini Tal was founded only in 1841, with the construction of the first European house (Pilgrim Lodge) by P. Barron, a sugar trader from Shahjahanpur. In his memoir, he wrote: "It is by far the best site I have witnessed in the course of a 1,500 miles (2,400 km) trek in the Himalayas."[16] In 1846, when a Captain Madden of the Bengal Artillery visited Naini Tal, he recorded that "houses were rapidly springing up in most parts of the settlement: some towards the crest of the military ranges were nearly 7,500 ft (2,300 m) above sea level: the rugged and woody Anyarpatta Aashish (Anyar-patt – in Kumaoni means – complete blackout. The reason for this nomenclature by the locals was because there were minimal sun rays due to its location and dense forests) was being gradually planted and that the favourite sites were on the undulating tract of forest land which stretched back from the head of the lake to the base of China and Deopatta (Camel's Hump). The church, St. John(1846) in the Wilderness, was one of the earliest buildings in Nainital, followed by Belvedere, Alma lodge, Ashdale Cottage(1860)..."[17] Soon, the town became a health resort favoured by British soldiers and by colonial officials and their families trying to escape the heat of the plains. Later, the town became the summer residence of the governor of the United Provinces.

1875

1882

A general view of the north end of Naini Tal before and after the landslip of 1882.

On 18 September 1880 a landslide ('the landslip of 1880') occurred at the north end of the town, burying 151 people. The first known landslide had occurred in 1866(old Victoria hotel was destroyed), and in 1869 there was a larger one at the same spot, Alma Hill, but "the great slip" occurred on "Saturday 18 September 1880."[17]

Nainital in 1940's

"During Friday(17th) and Saturday(18th), 33 inches of rain fell, of which 20 inches (510 mm) to 25 in (640 mm) fell during the 40 hours preceding Saturday evening, and the downpour still lasted and continued till the evening of the next day. This heavy fall made the whole hillside one mass of semi-fluid matter, and required little to set in motion. The motive power was a shock of a minor earthquake, which was felt on that day itself by competent observers in the Bhabar below and Nainital itself. On the site of the Slip was the Victoria Hotel and its offices, and below it was the hindu temple of "naina devi" and the Assembly Rooms, both by the side of the lake, and Bell's shop, which was close to the temple. Initial slip started around 10 am of 18 September, taking away western wing of the Victoria Hotel and portion of the hotel's out-houses. Tragically, most of the people were not moved much further away from the spot of the morning slip. At quarter to two the major landslip occurred and within few seconds all the buildings mentioned above were destroyed and made into an unrecognizable heap of rubble and much of it was swept into the lake."[17][18]

The number of dead and missing were 108 Indian and 43 Europeans, along with numerous people who narrowly escaped. (See poem by Hannah Battersby on the page Literary references to Nainital.) The Assembly Rooms and the Naina Devi Temple were destroyed in the disaster. A recreation area known as 'The Flats' was later built on the site and a new temple was erected. To prevent further disasters, storm water drains were constructed and building bylaws were made stricter.

The municipal board of Nainital had its origin in 1845, when the provisions of the Act I of 1842 were sanctioned by the government in the town, which then applied to approximately two thirds of the total population.[19]^:90

Nainital city is represented in the Lok Sabha, the lower house of the Indian Parliament, by a representative elected from the Nainital-Udhamsingh Nagar Constituency. Ajay Bhatt, from BJP, is the current Member of Parliament from Nainital-Udhamsingh Nagar.[20] He won the 2019 Indian general elections by 3,39,096 votes against Harish Rawat from the Congress, who was also the former chief minister of the state.[21] Prior to the delimitation of the Loksabha Constituencies of Uttarakhand in 2008, the city was a part of the Nainital Lok Sabha constituency.[22] Generally considered a Congress Stronghold, the Congress has registered a victory from Nainital eight times since 1951.[23] While the BJP has won this seat three times, several other political parties have also managed three victories.

The Nainital Yacht Club, situated along the lake, is run by the Boat House Club. It is the highest yacht club in India and among the highest clubs in the world. It was founded in 1910 by the British and, till 1970, was only open to members. Today, tourists can pay for a sailing session on the yachts.

The Jama Masjid of Nainital is located in Mallital area of Nainital is a mosque which was built in 1882 during the British Era for Muslims around Nainital. Over the main entrance one can see Arabic inscriptions. The most notable feature is the mihrab where a niche shows the direction towards Mecca.[33]

Temple of Naina Devi is located at the upper end of the beautiful Naini lake. This temple is dedicated to the goddess of the town Naina Devi. Its complex becomes the location of the famous Nanda Devi Mela festival which held every year on Nandashtami during September.[34]

St. John in the Wilderness is one of the oldest and finest churches in Nainital. The Church is dedicated to St. John the Baptist. This Anglican Church was built in 1846 and is one of the earliest buildings erected in Nainital.[35]