BASIC INFORMATION
- Area 1129.93 sq.km.
- Height 300 to 1140 meters
- Rainfall 1036 mm
- Temperature 1°C (min.) 50°C (max.)
- Seasons: Summer (March-June), Monsoon (July –September), Winter (October-February)
HISTORY
Palamau Tiger Reserve was established when India was introducing the famous Project Tiger in the year 1973 to save the endangered asset of our country. It was believed that with the introduction of this reserve the endangered species of tigers along with other wild counts would be preserved and cared under the Wildlife Protection Act. Year ago before the establishment of Palamau Tiger Reserve, the management of these forests was highly commercial. There were some cattle camps and the area were open for grazing. The entire forest area used to be ravaged by fires every year with the unchecked activities of poaching. But today, the present area of the Reserve got duly constituted either as Protected Forest or Reserved Forest under the Indian Forest Act, 1927 way back in 1947.
BIODIVERSITY
Flora as well as fauna in the forests under Palamau Tiger Reserve have been protected andconserved over the last 40 years. The keystone species are Tigers, Elephants, Leopards,Grey Wolf, Gaur, Sloth Bear, Four- horned Antelope, Indian Ratel, Indian Otter and Indian Pangolin. There are 11 Schedule- I species distributed in PTR among mammals only. In total, 47 species of mammals and 174 species of birds have been identified. Apart from these, a total of 970 species of plants, 17 species of grass and 56 species of medicinal plants have also been identified.
MAHUADANR WOLF SANCTUARY
It was declared to be a wildlife sanctuary in 1976 for the protection of the Indian wolf. It is the only wolf sanctuary in the country.It is spread over approx. 63 square kilometres. There are large numbers of wolf dens in the park, where the packs nest and rear their young, and where males court females during the breeding season, between November and February. According to the first count in 1979, there were 49 wolves in the sanctuary. The total population increased substantially over the next several decades, reaching 568 by 2004. In 2009, there were 58 wolves counted in the sanctuary. There were 120 wolves in 2020.
CLIMATE
The climate is typically tropical monsoonal type with four distinct seasons:
- Winter: Mid- November to mid- February
- Summer: Mid- February to mid- June
- Rains: Mid- June to mid- September
- Autumn: Mid- September to mid- November
Winter temperatures can sometimes dip to 4º C. The summer season is very hot and dry and sometimes temperature can reach 45.5º C in the northern portion. The southern areas, being at higher altitudes and with denser forest cover, are comparatively moderate in summer. Frost occurs almost every year, especially in the grassy blanks, but usually it is not of a severe nature. The area is dry with very low humidity during March to early May. Depending upon the season relative humidity in the morning’s ranges from 68% to 83% where as it is 25% to 75% in the evenings.
TERRAIN
The terrain is undulating with several hills and valleys. This forms several primary and secondary level streams in the area. The elevation ranges from 200 to 1700m MSL.
RAINFALL, RIVERS AND STREAMS
Palamau Tiger Reserve is drought-prone area due to rain-shadow effect. Most of the rainfall is received from the southwest monsoon. Mean annual rainfall is 1075mm. Rainfall is higher in the southern portions than northern portion. There are two perennial rivers- North Koel and Burha and many non-perennial rivers, streams and nallahs like Auranga, Satnadiya, Panchnadia, Kohbarwa, Aksi, Pandra, Surkumi, Kotam, Chipru, Jawa, Charu etc. Many aquifers locally called ‘Chuan’ are also present. A sulfur hot spring ‘Tatha’ is present near Barwadih.
GEOLOGYAND ROCK
The characteristic geological formation of the reserve, in brief, is gneiss. The groups of rocks occurring within the tract may be classified for forest descriptive purposes as follows: -
- Laterite – High level Laterite and Bauxite
- Quartzite – Quartzite, microcline, epidosite, biotite schist, diopsidite, pegmatite, biotitehillimanite-schist.
- Gneiss – Hornblende- granulite, hornblende- gneiss, diopsidite, biotite gneiss, microcline and quartz aplite,
- Hornblende – biotite gneiss. Magnetite, tufa, olivine, epidosite and pegmatite.
- Amphibolite– Amphibolite, pyroxene granulite, hypersthene gneiss, hornblende granuliteand quartz.
- Gondwana– Barakar and Mahadeva sandstones, grits, shales, haematite, conglomerate.
- Alluvial– Alluvial deposits consist of silt, sands, clay and gravel and organic matter. All three major rivers North Koel, Auranga and Burha from extensive alluvial deposit in PTR.
TOURIST PLACES
South Division, PTR has many tourist places to visit.