Introduction
Bundelkhand lies between the Indo-Gangetic Plain to the north and the Vindhya Range
to the south. It is a gently-sloping upland, distinguished by barren hilly
terrain with sparse vegetation, although it was historically forested. The
plains of Bundelkhand are intersected by three mountain ranges, the Vindhya,
Fauna and Bander chains, the highest elevation not
exceeding 600 meters above sea-level. Beyond these ranges the area is further
diversified by isolated hills rising abruptly from a common level, and
presenting from their steep and nearly inaccessible scarps eligible sites for
forts and strongholds of local kings.
Sub Regions
Yamuna Strip: The northern most
part of Bundelkhand, along the Yamuna, is a narrow ravine strip, which is
thinly inhabited and traditionally infested with dacoits.
Bundelkhand
Plain:
As we move southwards, we come across vast flatlands of the Bundelkhand Plain, running across Jalaun, Jhansi, Hamirpur, Banda districts and parts
of Mahoba and Chitrakoot districts. Soil quality and topography vary as we move
from west to east, and the plain can be divided into Jalaun, Hamirpur and Banda
plains. In the western most part of the Jalaun plain, the soil is sandy. The
central and eastern parts of the plain are well served by canal irrigation.
Agriculture productivity is relatively high. The Banda plain is one of the most
fertile areas of Bundelkhand. The eastern part of the Banda plain, which falls
under Chitrakoot district, is however dissected by deep channels of minor
rivers, flowing towards the Yamuna; here the soil is of poor quality and
agriculture production is poor. Moving south, we come across an
intermediate sub-region between Bundelkhand Plains and Bundelkhand Upland.
Bundelkhand
Intermediate:
Most of Jhansi,
Lalitpur, Tikamgarh and Chhatarpur districts fall in the Bundelkhand
Intermediate region. Most of this sub region has light black soils; its eastern
corner, in Chhatarpur district, is most suited for high productivity
agriculture.
Bundelkhand
Plateau :
South of the intermediate region, lies the Bundelkhand Upland or plateau ,
covering southern parts of Lalitpur, Tikamgarh and Chitrakoot districts and
Panna district. This plateau is characterised by large tracts of rocky
wastelands and undulating terrain, which enables natural or manmade storage of
water. A large number of manmade structures, built several centuries ago, are
found in Tikamgarh tehsil, which thus boasts of relatively high agricultural
productivity.
Eastern Forests: In the eastern
portion of Bundelkhand Upland, we see two different kinds of forested
areas. The first, in Panna district, is a narrow belt of flat-topped hill
ranges with steep cliffs. This area was once thickly forested; it is still
Bundelkhand’s most forested region, with a large tribal population, but due to
decades of overexploitation and poor management, much of the jungle is of poor
quality.
Patha Plateau:
As
its name suggests, the Patha is a rocky region, cut by deep valleys of
torrential rivers that are dry a few months after the monsoons. Much of the
region is covered by scrub forests, is thinly populated and till the 1980s, was
largely inaccessible. The majority of the population is of Kol tribals.
Agriculture is done on stretches of thin soil cover.
Sagar Plateau: The southernmost
part of Bundelkhand is formed by the Sagar and Damoh plateaus, which truly
speaking do not belong to the region. The Sagar Plateau forms the eastern edge
of the Malwa plateau. It rises about 1,400 feet and is bound by the Narmada River. A good amount of black cotton
soil is found in this sub region. Black cotton soil is also found in the Damoh plateau, which belongs to the Vindyachal-Baghelkand
region, and is part of a series of stepped plateaus girdled by massive hill
ranges called Bharner and Kaimur. A part of this upland, traversed by a
river called Sonar, is relatively level. Damoh town is located in this portion.
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