By Stephen Neill
This e-book, a sequel to Bishop Neill's A background of Christianity in India: The Beginnings to 1707, lines its topic from the dying of Aurunzib to the so-called Indian Mutiny. The heritage of India seeing that 1498 is of a massive war of words of cultures and religions. on the grounds that 1757, the manager half during this disagreement has been performed via Britain; and the Christian missionary firm, specially on its academic aspect, has had a crucial position. This ebook depicts with admirable equity all of the a number of different types of Christian religion that experience made touch with India. during this quantity, the Indian voice within the controversy starts essentially to be heard. Bishop Neill had was hoping it might be heard much more truly in a 3rd quantity tracing the tale to Independence in 1947 and the formation of the Church of South India during which he himself performed so fashionable an element. regrettably, he died earlier than he might write it.
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Extra info for A History of Christianity in India: 1707-1858
11 Land Utilisation The land use or the utilisation of land largely depends upon some physical factors, and it changes spatially and temporarily due to the continuous changing of the physical and human factors. Within the Haora River basin, 38 % of the area is still under the natural land cover system like forest, scrub land, river, water bodies, etc. (Fig. 15). Different agricultural practices (settled and shifting cultivation) are occupying 35 % of the basin. Twelve per cent of the area is marked as rural–urban built-up area and there is 14 % the area which is considered as fallow (Fig.
Tea plantation was seen on the left bank and for planting these tea plants, people were used to deforest the slope (Fig. 26). From the 3-year survey, it is found that the river tends to migrate towards its left bank. Erosion is taking place continuously from the steep left bank and the materials are deposited in the lower part of the bank and some portion is also carried down into the river. 7 m. Here the maximum depth is found near the left bank of the river. The abundant course of the river near right bank is now covered with sand deposition (Fig.
Four tributaries are joining with the Haora River along its right bank and the other three have joined along the left bank. From the source to the confluence, the sequential confluences of the tributaries are Bardowali (right bank tributary), 22 2 Haora River Basin: Location and Geographical Background Yearly Rainfall Graph Monthly Temperature graph Temperature in °C Rainfall in Cm 300 250 200 150 100 50 30 20 10 0 J 1991 1992 1993 1994 1995 1996 1997 1998 1999 2000 2001 2002 2003 2004 2005 2006 2007 2008 2009 0 Years F M A M J J Year 2009 A S O N D Months Min Max Fig.