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Chandoli National Park , Western Ghats
Chandoli National Park is a national park established in Sangli district on May 2004. Earlier it was a Wildlife Sanctuary declared in 1985. Chandoli Park is notable as the southern portion of the Sahyadri Tiger Reserve, with Koyna Wildlife Sanctuary forming the northern part of the reserve Sahyadri Tiger Reserve The Sahyadri Tiger Reserve, including all of Chandoli National Park and Koyna Wildlife Sanctuary was declared by The National Tiger Conservation Authority as a Project Tiger tiger reserve on May 21, 2007. The Sahyadri Tiger Reserve was then estimated to have nine tigers and 66 leopards. Location Chandoli National Park is located near thChandoli Dambetween longitudes 73°40' and 73°53' E and latitudes 17°03' and 17°20'N in Sangli District of Western Maharashtra. It lies between the Radhanagiri and Koyna Wildlife Sanctuaries and forms the southern part of the Sahyadri Tiger Reserve. it is near about 101 km from sangli History The park includes historical pl ...
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Sangli District
Sangli district (Marathi pronunciation: aːŋɡli is a district of Maharashtra state in India. Sangli city is the district headquarters. It is bordered by Satara district, Solapur district to the North, Karnataka state to South-East, by Kolhapur district to South-West and by narrow portion in East side to Ratnagiri district. It is present on the southern tip of Maharashtra. The district is 25.11% urban. Sangli and Miraj are the largest cities. The industrial cities like Kirloskarwadi and palus is also located in the Sangli District. Industrialist Laxmanrao Kirloskar started his first factory here. It is known as the sugar bowl of India due to its high sugarcane productivity. Sangli District is one of the most fertile and highly developed districts in Maharashtra. The District is very popular as a political power house in the state. It has provided many politicians and bureaucrats and is often referred to as the ''Heaven of Farmers''. Officer Members of Parliament *Sanjay ...
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Maratha Empire
The Maratha Empire, also referred to as the Maratha Confederacy, was an early modern Indian confederation that came to dominate much of the Indian subcontinent in the 18th century. Maratha rule formally began in 1674 with the coronation of Shivaji of the Bhonsle Dynasty as the '' Chhatrapati'' (Marathi: "The title "Chhatrapati" was created by Shivaji upon his coronation"). Although Shivaji came from the Maratha caste, the Maratha empire also included warriors, administrators and other notables from Maratha and several other castes from Maharashtra. They are largely credited for ending the Mughal control over the Indian subcontinent and establishing the Maratha Empire. The religious attitude of Mughal Emperor Aurangzeb estranged non-Muslims, and his inability to finish the resulting Maratha uprising after a 27-year war at a great cost to his men and treasure, eventually ensued Maratha ascendency and control over sizeable portions of former Mughal lands in the north or ab ...
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Dwarf Forest
Dwarf forest, elfin forest, or pygmy forest is an uncommon ecosystem featuring miniature trees, inhabited by small species of fauna such as rodents and lizards. They are usually located at high elevations, under conditions of sufficient air humidity but poor soil. There are two main dwarf forest ecosystem types, involving different species and environmental characteristics: coastal temperate and montane tropical regions. Temperate coastal dwarf forest is common for parts of Southern California. Montane tropical forests are found across tropical highlands of Central America, northern South America and Southeast Asia. There are also other isolated examples of dwarf forests scattered across the world, while the largest dwarf forest is found in the Philippines. High-elevation tropical dwarf forest High-elevation tropical locations in cloud forests contain mossy wet elfin forests due to high-elevation precipitation. These regions are characterized by low rainfall, with most of the wa ...
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North Western Ghats Moist Deciduous Forests
The North Western Ghats moist deciduous forests is a tropical moist broadleaf forest ecoregion of southwestern India. Geography The North Western Ghats moist deciduous forests lies in the northern portion of the Western Ghats (Sahyadri) range. It extends from southeastern Gujarat through Dadra and Nagar Haveli, Maharashtra, Goa, and Karnataka. It covers the eastern and western slopes of the range between 250 and 1000 meters elevation, and surrounds the North Western Ghats montane rain forests ecoregion, which lies above 1000 meters elevation. The ecoregion has an area of . It is bounded on the west by the Malabar Coast moist forests ecoregion, which lies between the 250 meter elevation and the Arabian Sea. At its northern end, the ecoregion extends to the Narmada River, and borders the Khathiar-Gir dry deciduous forests to the northwest and the Narmada Valley dry deciduous forests to the northeast. The Wayanad forests at the southern end of the ecoregion mark the trans ...
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Malabar Coast Moist Forests
The Malabar Coast moist forests are a tropical and subtropical moist broadleaf forests, tropical moist broadleaf forest ecoregion of southwestern India. Geography The ecoregion lies along India's Konkan and Malabar coasts, in a narrow strip between the Arabian Sea and the Western Ghats range, which runs parallel to the coast. It has an area of , and extends from northern Maharashtra through Goa, Karnataka and Kerala to Kanyakumari district, Kanniyakumari in southernmost Tamil Nadu. The ecoregion extends from sea level to the 250 meter contour of the Western Ghats. It is bounded on the east by the North Western Ghats moist deciduous forests in Maharashtra and Karnataka, and the South Western Ghats moist deciduous forests in Kerala. Much of the ecoregion is densely populated, and it includes several large cities, including Mumbai in Maharashtra, Mormugao and Margao in Goa, Mangalore in Karnataka, and Thiruvananthapuram, Kochi, and Kozhikode in Kerala. Climate The climate is trop ...
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Plateau
In geology and physical geography, a plateau (; ; ), also called a high plain or a tableland, is an area of a highland consisting of flat terrain that is raised sharply above the surrounding area on at least one side. Often one or more sides have deep hills or escarpments. Plateaus can be formed by a number of processes, including upwelling of volcanic magma, extrusion of lava, and erosion by water and glaciers. Plateaus are classified according to their surrounding environment as intermontane, piedmont, or continental. A few plateaus may have a small flat top while others have wide ones. Formation Plateaus can be formed by a number of processes, including upwelling of volcanic magma, extrusion of lava, Plate tectonics movements and erosion by water and glaciers. Volcanic Volcanic plateaus are produced by volcanic activity. The Columbia Plateau in the north-western United States is an example. They may be formed by upwelling of volcanic magma or extrus ...
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Laterite
Laterite is both a soil and a rock type rich in iron and aluminium and is commonly considered to have formed in hot and wet tropical areas. Nearly all laterites are of rusty-red coloration, because of high iron oxide content. They develop by intensive and prolonged weathering of the underlying parent rock, usually when there are conditions of high temperatures and heavy rainfall with alternate wet and dry periods. Tropical weathering (''laterization'') is a prolonged process of chemical weathering which produces a wide variety in the thickness, grade, chemistry and ore mineralogy of the resulting soils. The majority of the land area containing laterites is between the tropics of Tropic of Cancer, Cancer and Tropic of Capricorn, Capricorn. Laterite has commonly been referred to as a soil type as well as being a rock type. This and further variation in the modes of conceptualizing about laterite (e.g. also as a complete weathering profile or theory about weathering) has led to c ...
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Elevation
The elevation of a geographic location is its height above or below a fixed reference point, most commonly a reference geoid, a mathematical model of the Earth's sea level as an equipotential gravitational surface (see Geodetic datum § Vertical datum). The term ''elevation'' is mainly used when referring to points on the Earth's surface, while '' altitude'' or '' geopotential height'' is used for points above the surface, such as an aircraft in flight or a spacecraft in orbit, and '' depth'' is used for points below the surface. Elevation is not to be confused with the distance from the center of the Earth. Due to the equatorial bulge, the summits of Mount Everest and Chimborazo have, respectively, the largest elevation and the largest geocentric distance. Aviation In aviation the term elevation or aerodrome elevation is defined by the ICAO as the highest point of the landing area. It is often measured in feet and can be found in approach charts of the aerodrome ...
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Chhatrapati Sambhaji Maharaj
Sambhaji Bhosale (14 May 1657 – 11 March 1689) was the second Chhatrapati of the Maratha Empire, ruling from 1681 to 1689. He was the eldest son of Shivaji, the founder of the Maratha Empire. Sambhaji's rule was largely shaped by the ongoing wars between the Maratha Empire and the Mughal Empire, as well as other neighbouring powers such as the Siddis, Mysore and the Portuguese in Goa. After Sambhaji's death, his brother Rajaram I succeeded him as the next Chhatrapati. Early life Sambhaji was born into a Marathi Hindu family at Purandar fort to the Maratha ruler Shivaji, and his first wife Saibai, who died when he was two years old and he was raised by his paternal grandmother Jijabai. At the age of nine, Sambhaji was sent to live with Raja Jai Singh I of Amber as a political hostage to ensure compliance of the Treaty of Purandar that Shivaji had signed with the Mughals on 11 June 1665. As a result of the treaty, Sambhaji became a Mughal mansabdar. He and his father S ...
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Shivaji Maharaj's
Shivaji Bhonsale I (; 19 February 1630 – 3 April 1680), also referred to as Chhatrapati Shivaji Maharaj, was an Indian ruler and a member of the Bhonsle Maratha clan. Shivaji carved out his own independent kingdom from the declining Adilshahi sultanate of Bijapur which formed the genesis of the Maratha Empire. In 1674, he was formally crowned the ''Chhatrapati'' of his realm at Raigad Fort. Over the course of his life, Shivaji engaged in both alliances and hostilities with the Mughal Empire, the Sultanate of Golkonda, Sultanate of Bijapur and the Colonial India, European colonial powers. Shivaji's military forces expanded the Maratha sphere of influence, capturing and building forts, and forming a Maratha Navy, Maratha navy. Shivaji established a competent and progressive civil rule with well-structured administrative organisations. He revived ancient Hindu political traditions, court conventions and promoted the usage of the Marathi language, Marathi and Sanskrit languages ...
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