Thalisain
Thalisain is a town and tehsil of Pauri Garhwal district in the North Indian state of Uttarakhand. At an altitude of 1690 metres from sea level, it is situated on a gentle slope above the right bank of Nayaar river. It is in the southwestern foothills of Dudhatoli Range and at a distance of 83 kilometers from Pauri town and 95 kilometers from Gairsain, the future capital of Uttarakhand.
Etymology
Originally, the name of the place was Thali, but since the town is settled on a long and gentle hill it later came to be known as Thalisain. Just like in Gairsain, “Gair” means a deep place or a valley and “Sain” means a flattish hill.History
Garhwal got its name during the 9th century AD when Kanakpal, the chieftain of Chaandpurgarhi, conquered all the little kingdoms from Uttarkashi to Garhwal-Kumaon border and unified them to form the kingdom of Garhwal with Garhwali as the official state language. Garhwal literally translates to “Land of Forts”. There were 52 of those fortresses scattered all over the land, Chaandpur being one of them. Thalisain was a part of Patti Choprakot in the historic Chaandpur kingdom, with its headquarters at Chaandpurgarhi in Chamoli Garhwal. Chaandpur kingdom administered five Pattis of Garhwal viz Choprakot, Chauthan, Dhaijyuli, Lohbha and Chaandpur.Ruins of ancient temples of that era can still be found and a few temples are in a very good condition. From these ancient monuments, it can be ascertained that the place has been inhabited since ancient times. Although Thalisain town doesn't have any ancient monuments, but ancient temples can be found scattered around the surrounding hill-tops. Most of these stone temples have been built in traditional Ashlar style, some even showing Katyuri characteristics dating from 12th to 16th century AD. All the temples except Rahu temple in Paithani have been built in remote areas or in wilderness. Besides temples, there are a good number of old houses that can be seen in some villages. These traditional houses, known as Tibaari in Garhwali were quite popular at the time, when Garhwal dynasty was at its peak. Later on, Pauri and Chamoli became a part of British Garhwal and the kingdom of Garhwal shrank in size, almost the entire Uttarakhand was under the British. Thus began a decline of those houses and their construction flourished only in the valley of Bhagirathi, which was the last stronghold of the royal family. Today, those temples and houses tell of the glorious past of the Garhwal kingdom when there were no roads and warriors roamed the forests and bridle paths on their horses.
While British administration undertook the construction of several roads, schools and medical facilities in the region, they also formulated policies to take control of the natural resources, specifically the forests, as the region had one of the densest forest covers in Garhwal hills and was conveniently close to the plains of North India. Trees were felled recklessly for timber, fuel and railway sleepers. It was during that era, when railway line was extended from Moradabad to Ramnagar in 1907. Ramnagar became the nearest railhead for the region and facilitated harvesting of forest produce.
Geography
Thalisain tehsil comprises two blocks, Bironkhal block and Thalisain block. Thalisain development block extends from latitudes 29.54 N to 30.10 N and longitudes 78.54 E to 79.13 E, measuring 35 km in length and 49 km in width. Most of the Himalayan ranges extend from north-west to south-east direction. The south-eastern face is most favorable site for the location of settlements. Because of the sunny aspect, compact settlements are located on the spurs and river terraces. The south- eastern faces are denser than northern and western aspects. North western aspects are not favorable for human habitation and agricultural occupations because it receives less solar energy.Climate
The climate is influenced by the altitude and relative position of the land. The overall climate of the region is temperate. The valley area experiences pleasantly warm climate, hence dense population is found in the valleys. Mid slope and mountain ranges have a temperate climate hence semi-compact and scattered settlements are found here. Above 2000m, there are temporary seasonal settlements which are generally distributed on the forest land. Aspects play a significant role in the selection of settlement sites in the Himalayan Mountain. Temperature ranges between 15 and 30 degrees Celsius in summer and -5 to 15 degrees Celsius in winter. The region receives a significant amount of rain in monsoon season as well as snow from December to March.Natural resources
* Soil: Thalisain tehsil has a variety of soils depending of the altitude and terrain. As the Nayaar valley broadens in the south, it forms vast beds of fertile alluvial soil which is suitable for rice and other water-intensive crops. As one gains altitude while heading north towards Dudhatoli mountains, the soil gets sandy-loamy with good aeration and drainage. Such soil is suitable for fruits, vegetables and other horticultural produce. North-eastern faces of hills often have humus rich soil as they have stands of dense oak forest.* Forests: There are chiefly 4 types of forests found in the region.
- Chir pine forests: The primary species is Pinus roxburghii. Occurring from 1100 to 2200 metres above sea level, these trees grow on drier slopes. However, commercial plantations have come up recently for producing Turpentine, timber-wood and fuel.
- Mixed Chir-oak forests: Moist forests at slightly higher altitudes with a predominant mix of Baanj, Chir Pine, Rhododendron, Kaafal trees. These forests exist at an altitudes ranging from 1800 to 2200 metres.
- Temperate broadleaf forests: The main species found in these forests are Maple, Oak, Hazelnut, Alder and Hornbeam. These forests are found at an altitude of 2200 to 3100 in shady and cool locations often with moisture.
- Alpine Coniferous forests: The dominant species are Silver Fir, Deodar, Cypress, Juniper and Spruce. Sometimes these trees exist in the same habitat but at many locations, there are stands of one species. These forests grow at an altitude of 2200 to 3100 metres.
Transport
NH 121 runs along the Nayaar river, both forming backbone of the region. Several arterial roads lead to remoter parts and serve as lifelines of the region. Still, a lot of high altitude and remote villages have not got roads yet. Some of these villages, specifically in Dodhatoli range, have a good population. Maroda and Daida are noteworthy examples.Demographics
As of 2005, Thalisain Block had an area of 584 km2. and a population of 56746 giving it an average population density of 85.46 persons per km2. Sex ratio is 1209 which is considerably higher than the national average of 940 females per 1000 males. Thalisain is pre-dominantly a Hindu majority region, people of other religions have settled here as recently as late 1990s in the last two decades. Hinduism is practised by 99.7% of population, Muslims are 0.2%, and 0.1% didn't state their religion. Total literacy rate is 72.15%, where male literacy rate is at 88.23% and female at 59.09%.Most of the population of this region is confined to valleys and mid slopes of the hill ranges. The area is totally rural with few rural service centers which are developed in urban characteristics. Most of the population is concentrated on the valleys where as fertile agricultural land is available on the terraces. Moderate concentration of population is found on the gentle slope convex spurs. Very sparse population with scattered settlements is located on the water divides and ridges. Concentration of most of the population is in the valleys with lowest altitude. As the altitude increases the distribution of population decreases, hence the hill ranges have less population compared to valley. Since the very beginning the settlements were located near the source of water. In the valley areas, dense population is the reason of, abundance of water in the form of perennial springs and rivers. Lack of water resources on the high hill ranges are responsible for scattered settlements with low population density.