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EDITORIAL
Shri Jagannath Singh, I.A.S.(Retd.)

अपना बुंदेलखंड डॉट कॉम परिवार के सदस्यों को "रामनवमी" की शुभकामनायें। राम जिन्होंने बुंदेलखंड के चित्रकूट क्षेत्र में संकल्प लिया कि "निश्चर हीन महि करूँ , भुज उठाहि प्रण (Read More)


 Minerals

Minerals

Diamonds: Diamonds found in Panna district constitute Bundelkhand's most well known mineral wealth and were highly prized in medieval times, when the stone was found only in India. However, after the discovery of diamonds in Brazil in 1725, and in the 1870s in South Africa, the Panna diamonds lost much of their sheen. From a global market perspective, diamond production in Panna is today of little volume or value. extensive limestone deposits in Damoh, Chhatarpur and Datia, basaltic rocks in southern Lalitpur and sandstone deposits in Panna and Sagar. 

Granite: Geologically, Bundelkhand presents a mixture from different areas, from the earliest days of the formation of the earth, when its upper crust cooled and solidified, till recent times. From the earliest period, older than 2500 million years, are granite-like formations called gneiss and so-called Bundelkhand Granite. Massive blocks of medium to coarse-grained varieties of pink, red and grey granite are found in Jhansi, Lalitpur, Mahoba, Banda, Datia, Chhatarpur, Panna and Sagar districts. Multicolored and black granites are found in parts of Sagar and Panna. A variety called Jhansi Red, mined in Chhatarpur, is found in no other country. Another prized variety found in the district is called Fortune Red.

Sandstone: White, buff, cream, pink and red sandstone (flagstone) varieties are found in different layers in the Vindhyan hills; the most extensive deposits are in Panna and Sagar districts. The lowest layer sandstone is an excellent building material, with uniform colour and texture. It can be chiselled easily and in great detail. The temples of Khajurao and its famous sculptures, in Chhatarpur district, are made from locally sourced Kaimur sandstone. Lalitpur is known for sandstone varieties called Lalitpur Grey and Lalitpur Yellow. Other less known varieties of sandstone are mined found in considerable quantities in Chhatarpur.

Pyrophillite: Large reserves of pyrophyllite, a soft, light-coloured stone, are found in Jhansi, Lalitpur, Mahoba, Tikamgarh and Chhatarpur districts, constituting around 80% of the country's reserves of this material. The stone is used for making decorative items. Found in combination with a mineral called doaspore, it has industrial uses also.

Limestone: Stone of lower value, used in crushed form in road and building construction, is available in large quantities in Bundelkhand Intermediate and Bundelkhand Upland sub-regions. The Vindhyan hills provide, in Sagar, Damoh and Panna districts, large quantities of limestone

Silica Sand: UP's main mineral belt lies in Bundelkhand and other southern districts of the state like Allahabad and Sonbhadra. Excluding granite, the most precious resource of UP Bundelkhand is silica sand found in Mau tehsil of Chitrakoot and an adjacent area of Shankargarh of Allabahad district. The deposits are said to be the best source of glass sands in India.

Rock Phosphate: It is Used in the fertilizer industry and found in Lalitpur; it is also mined in Chhatarpur. Large reserves of low grade iron ore (25-30% iron) are found in Lalitpur. Other minerals available in less valuable quantities include feldspar, used in ceramics industry, found in Jhansi and diaspore, used in refractories, found in Lalitpur, Mahoba and Banda districts. 

Clay: Used in lime and cement industries, is found in Datia, Panna and Tikamgarh. Ken river are used for making objects’d art.

Dolomite: It is found in Sagar and Banda districts.

Alluvium: The most recent geological deposits are alluvium, in the form of sand, silt or clay, brought down by north-flowing rivers.

Rocky Ridges:  In Bundelkhand a striking feature is the presence of long and narrow rocky ridges, known as quarts reefs and dolerite dykes. Often, these wall-like natural features intercept the course of streams, leading to formation of water bodies and enabling the creation of large artificial lakes.



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