Karnataka has a variety of metallic and non-metallic mineral resources due to its varied geological formations ranging from Precambrian to recent. Some key metallic minerals produced in Karnataka include gold, iron ore, manganese ore, and chromite. Important non-metallic minerals include limestone, dolomite, clay, feldspar, and silica sand. Karnataka has significant reserves of these minerals and occupies a premier position in India for its reserves of gold, manganese ore, magnetite, and limestone.
Among the Subjects of Earth Sciences, Economic Geology deals with all the Mineral resources, mineral fuels, their distribution and their role for the economic development of a nation.
India has a good amount of all natural resources. Among the resources, minerals are the major contributors of the national economy. India is a country, much dependent on the available natural resources for its economy. This lesson is on the “ Mineral Resources in India”.
Eastern Ghats
The eastern ghats run parallel to the eastern coastal plains of India.Unlike the western ghats, they are discontinuous in nature and is dissected by the rivers that drain into the Bay of Bengal. As discussed above, most of these rivers have their origin in the western ghats.It must be noted that the eastern ghats are lower in elevation than the western ghats.The highest peak of Eastern Ghats is the Jindhagada peak (1690 meters). It is also known as Arma Konda or Sitamma Konda.The difference in the elevation levels of the highest peaks in both the ghats can also be compared. Jindaghara of eastern ghats is of 1690 mts. This gives us a fair idea of the differences in elevation levels of the hills in both the ghats.The main crop produced in the eastern ghats is Rice, which is also the staple food of the people living in the region.
Among the Subjects of Earth Sciences, Economic Geology deals with all the Mineral resources, mineral fuels, their distribution and their role for the economic development of a nation.
India has a good amount of all natural resources. Among the resources, minerals are the major contributors of the national economy. India is a country, much dependent on the available natural resources for its economy. This lesson is on the “ Mineral Resources in India”.
Eastern Ghats
The eastern ghats run parallel to the eastern coastal plains of India.Unlike the western ghats, they are discontinuous in nature and is dissected by the rivers that drain into the Bay of Bengal. As discussed above, most of these rivers have their origin in the western ghats.It must be noted that the eastern ghats are lower in elevation than the western ghats.The highest peak of Eastern Ghats is the Jindhagada peak (1690 meters). It is also known as Arma Konda or Sitamma Konda.The difference in the elevation levels of the highest peaks in both the ghats can also be compared. Jindaghara of eastern ghats is of 1690 mts. This gives us a fair idea of the differences in elevation levels of the hills in both the ghats.The main crop produced in the eastern ghats is Rice, which is also the staple food of the people living in the region.
This notes provide the information about tectonic divisions and evolution of Himalayas. movement of Indian plate has also taken up in brief.
Tectonic Division of Himalaya
Evolution of Himalaya
Movement of Indian Plate.
Resource description_ Rasoul Sorkhabi, The himalayan Journal, 2010
This will help you to know Gujarat State with simplicity and clarification.
The Culture, Traditions, Food, lifestyle, politics, facts, tourism, fairs, festivals and some points of attraction are described in this.
famous Cities, Places, and people of Gujarat are described.
The term "trap" has been used in geology since 1785–95 for rock formations. It is derived from the Swedish word for stairs (trapp , trappa) and refers to the step-like hills forming the landscape of the region.
The plateau: also called a high plain or tableland, is an area of highland, usually consisting of relatively flat terrain. A plateau is an elevated land. It is a flat-topped table standing above the surrounding area. A plateau may have one or more sides with steep slopes.
LIP – Large Igneous provinces. (Province = Area / Region)
DVP - The Deccan Volcanic Province is one of the Earth’s giant continental flood basalts and has a total exposed area of about half a million square kilometers in Maharashtra, Madhya Pradesh, Gujrat and some part of Andhra Pradesh. Deccan trap has maximum thickness 3400m in western ghat and its thickness goes decrease toward east side. At Amrakantat on east its thickness is just 160m. Geographical distribution is between latitudes 16° - 24° N and longitudes 70° - 77° E.
IN THIS POWERPOINT I ADDED FULLY HD PHOTO.AND THE INFORMATION AND STYLE ARE ADDED BY ME OWN.
DOWNLOAD AS FAST YOU CAN.
DON'T FORGET TO LIKE AND TO FOLLOW.
FOR ASKING FOR POWERPOINT OF OTHER SUBJECT.CONTACT TO shubhamrathi800@gmail.com or shubhamrathi99@hotmail.com
T H A N K YOU. . . . . .
this helps students of IX CBSE to visualise the picturesqueness the Ganga river system from its source to its delta and the role of each individual to preserve the holy river
Gold is a transitional metal. In its purest form have reddish yellow color, soft, malleable, and ductile metal.
Atomic number : 79
Atomic mass : 196.9 u
Density : 19.32 g/cm3
Melting point : 1,064 °C
Boiling point : 2,700 °C
Founded in different form associated with different rock type in different tectonic setting.
Discovered from earlier time and used for multi purposes.
Formation of gold
The saying among prospectors that "gold is where you find it" suggests its occurrence is unpredictable, but there is some certain geological environments for the formation.
Because gold is very stable over a range of conditions, it is very widespread in the earth’s crust.
Gold dissolved in warm to hot salty water, the fluids are generated in huge volumes deep in the Earth’s crust as water-bearing minerals dehydrate during metamorphism.
Any gold present in the rocks being heated and squeezed is sweated out and goes into solution as complex ions.
In this form, dissolved gold, along with other elements such as silicon, iron and sulphur, migrates wherever fractures in the rocks allow the fluids to pass.
The direction is generally upwards, to cooler regions at lower pressures nearer the Earth’s surface.
Gold eventually becomes insoluble and begins to crystallize, most often enveloped by quartz.
The association of gold and quartz vein forms one of the most common types of "primary gold deposits".
India
In India, gold mineralization of economic importance is mainly restricted to Archean greenstone terranes of the Dharwar Craton (DC).
The eastern block of the DC has a high favorability for hosting major gold deposits such as Kolar, Hutti, and Ramagiri, whereas the western block hosts only a few smaller deposits such as Gadag, Ajjahanahalli, and Kempinkote.
Gold also discoverrd by GSI in the Singbhum Craton, Aravalli Craton, Bastar Craton and Southern Granulite Terrain (SGT).
India is the second-largest consumer of gold after China.
India currently holds about 558 tones of gold, representing 6.6% of its reserves, (World Gold Council, October 2016).
Kolar Gold Field, Hutti Gold Field and Ramgiri Gold Field are the most important gold fields.
Gold Demand and Use
The largest source of demand is the jewelry industry Gold’s workability, unique beauty, and universal appeal make this rare precious metal the favorite of jewelers all over the world.
Besides jewelry, gold has many applications in a variety of industries including aerospace, medicine, dentistry, and electronics for the manufacture of computers, telephones, televisions...
The third source of gold demand is governments and central banks that buy gold to increase their official reserves.
Private investors there are private investors. Depending upon market circumstances, the investment component of demand can vary substantially from year to year.
This notes provide the information about tectonic divisions and evolution of Himalayas. movement of Indian plate has also taken up in brief.
Tectonic Division of Himalaya
Evolution of Himalaya
Movement of Indian Plate.
Resource description_ Rasoul Sorkhabi, The himalayan Journal, 2010
This will help you to know Gujarat State with simplicity and clarification.
The Culture, Traditions, Food, lifestyle, politics, facts, tourism, fairs, festivals and some points of attraction are described in this.
famous Cities, Places, and people of Gujarat are described.
The term "trap" has been used in geology since 1785–95 for rock formations. It is derived from the Swedish word for stairs (trapp , trappa) and refers to the step-like hills forming the landscape of the region.
The plateau: also called a high plain or tableland, is an area of highland, usually consisting of relatively flat terrain. A plateau is an elevated land. It is a flat-topped table standing above the surrounding area. A plateau may have one or more sides with steep slopes.
LIP – Large Igneous provinces. (Province = Area / Region)
DVP - The Deccan Volcanic Province is one of the Earth’s giant continental flood basalts and has a total exposed area of about half a million square kilometers in Maharashtra, Madhya Pradesh, Gujrat and some part of Andhra Pradesh. Deccan trap has maximum thickness 3400m in western ghat and its thickness goes decrease toward east side. At Amrakantat on east its thickness is just 160m. Geographical distribution is between latitudes 16° - 24° N and longitudes 70° - 77° E.
IN THIS POWERPOINT I ADDED FULLY HD PHOTO.AND THE INFORMATION AND STYLE ARE ADDED BY ME OWN.
DOWNLOAD AS FAST YOU CAN.
DON'T FORGET TO LIKE AND TO FOLLOW.
FOR ASKING FOR POWERPOINT OF OTHER SUBJECT.CONTACT TO shubhamrathi800@gmail.com or shubhamrathi99@hotmail.com
T H A N K YOU. . . . . .
this helps students of IX CBSE to visualise the picturesqueness the Ganga river system from its source to its delta and the role of each individual to preserve the holy river
Gold is a transitional metal. In its purest form have reddish yellow color, soft, malleable, and ductile metal.
Atomic number : 79
Atomic mass : 196.9 u
Density : 19.32 g/cm3
Melting point : 1,064 °C
Boiling point : 2,700 °C
Founded in different form associated with different rock type in different tectonic setting.
Discovered from earlier time and used for multi purposes.
Formation of gold
The saying among prospectors that "gold is where you find it" suggests its occurrence is unpredictable, but there is some certain geological environments for the formation.
Because gold is very stable over a range of conditions, it is very widespread in the earth’s crust.
Gold dissolved in warm to hot salty water, the fluids are generated in huge volumes deep in the Earth’s crust as water-bearing minerals dehydrate during metamorphism.
Any gold present in the rocks being heated and squeezed is sweated out and goes into solution as complex ions.
In this form, dissolved gold, along with other elements such as silicon, iron and sulphur, migrates wherever fractures in the rocks allow the fluids to pass.
The direction is generally upwards, to cooler regions at lower pressures nearer the Earth’s surface.
Gold eventually becomes insoluble and begins to crystallize, most often enveloped by quartz.
The association of gold and quartz vein forms one of the most common types of "primary gold deposits".
India
In India, gold mineralization of economic importance is mainly restricted to Archean greenstone terranes of the Dharwar Craton (DC).
The eastern block of the DC has a high favorability for hosting major gold deposits such as Kolar, Hutti, and Ramagiri, whereas the western block hosts only a few smaller deposits such as Gadag, Ajjahanahalli, and Kempinkote.
Gold also discoverrd by GSI in the Singbhum Craton, Aravalli Craton, Bastar Craton and Southern Granulite Terrain (SGT).
India is the second-largest consumer of gold after China.
India currently holds about 558 tones of gold, representing 6.6% of its reserves, (World Gold Council, October 2016).
Kolar Gold Field, Hutti Gold Field and Ramgiri Gold Field are the most important gold fields.
Gold Demand and Use
The largest source of demand is the jewelry industry Gold’s workability, unique beauty, and universal appeal make this rare precious metal the favorite of jewelers all over the world.
Besides jewelry, gold has many applications in a variety of industries including aerospace, medicine, dentistry, and electronics for the manufacture of computers, telephones, televisions...
The third source of gold demand is governments and central banks that buy gold to increase their official reserves.
Private investors there are private investors. Depending upon market circumstances, the investment component of demand can vary substantially from year to year.
i hope dis helps you guys to make ur ppt's
basically I am just giving you all ideas, you can be as creative as you want when you make them.
if any comments or suggestions please let me know
thank you
It is one of my finest works . A detailed packet of information of minerals with their types, how they are formed, mining processes and protection from mining hazards.
Metallogenic Epoch and Province
Metallogenetic Epochs
Metallogenetic epochs, as defined above, are specific periods characterised by formation of large number of mineral deposits. It does not mean that all the mineral deposits formed during a definite metallogenetic epochs. In India the chief metallogenetic epochs were:
1. Precambrian
2. Late Palaeozoic
3. Late Mesozoic to Early Tertiary
Minerals & Energy Resources
What Is Minerals?Its type ? Rocks? sedimentary rocks, igenious rock, etc., energy Consevation , energy -conventional And Non Conventional , Coal , Minerals, petroleum , Electricity, Nuclear Energy , Atomic Energy, Geothermal Energy , Types oF coals, Location Of The minerals . Why Need to conserve Minerals ?Save Earth
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3. Introduction
• Karnataka is one of the mineral rich states in India, with
an area of 1.92 lakh sq.km. Covering 29 districts.
• The state has a vast and varied Geological setting right
from Precambrian to recent formations, with 40,000
Sq. Kms of green stone belts endowed with valuable
mineral resources like gold, silver, copper, iron,
manganese, limestone, dolomite, chromite, magnesite
and other useful rock formations like granite etc.
• Karnataka has the distinction of being the principal
gold producing State in the country.
• The State is the sole producer of felsite and leading
producer of iron ore, chromite and dunite.
4.
5.
6. INTRODUCTION
• Metallic minerals are those minerals which yield metals after
being processed.
• Non-metallic minerals are those which do not yield new
products on melting.
Metallic minerals Non-Metallic minerals
I. These are generally associated with
igneous rocks.
II. They are usually hard and have
shines or luster of their own.
III. They are ductile and malleable.
IV. When hit, they do not get broken.
I. These are generally associated with
sedimentary rocks.
II. They are not so hard and have no
shine or luster of their own.
III. They are not ductile and
malleable.
IV. When hit, they may got broken
into pieces.
8. Gold
• Gold is produced from gold ore by HGML in
Karnataka. HGML operates mines at Hutti,
Uti and Hira-Buddini in Raichur district,
Karnataka.
• Karnataka is the leading producer of
gold accounting for 99% of the total production.
• Much of the mineralisation so far identified in the Kolar, Hutti-Maski,
Gadag and Chitradurga schist belts appears to be essentially shear
controlled, but the gold is also hosted in a variety of rocks.
• The occurrence of gold has been reported from Chitradurga, Dharwad,
Gadag, Gulbarga, Hassan,Haveri, Kolar, Raichur and Tumkur districts.
9. Silver
• Silver was recovered in the past as a
co-product in gold refining at KGF
Complex and Hutti Gold Mines in
Karnataka.
• Silver occurs in Chitradurga and Raichur
district.
• GSI has carried out extensive exploration in the G.R.Halli, C.K.Halli-
Honnemardi of Chitrsdurga district. Drilling has indicated a 575 m
long zone ranging in width upto 4.20 m with gold content of about
3.5 g/t and average silver content of about 80 ppm in the G.R.Halli
South block.
• The proved reserves of silver in the state is 86,81,065 tonnes.
10. Iron ore
• Karnataka hosts 73% of magnetite ore on the country.
• The iron ore deposits of Karnataka are principally of two types,
(i) Lateritoid concentrations, essentially of haematite with minor
limonite and goethite.
(ii) Magnetite mainly occur in the Bababudan Group as lenses or as
beds in the banded magnetite quartzite.
• Hematite occurs in Bagalkot, Bellary, Bijapur, Chickmagalur,
Chitradurga, Dharwad, Gadag, Uttara Kannada, Shimoga and Tumkur
districts. Magnetite is found in Chickmagalur, Hassan, Uttara &
Dakshina Kannada and Shimoga districts.
• Karnataka state produced about 13.2 million tonnes of iron ore in
2011-2012.
11. Manganese ore
• Karnataka has the largest recoverable
reserves of manganese ore in the country.
• Managanese ore minerals in close
association with haematite and carbonates
occur in the lower stratigraphic level of the
Chitradurga Group as stratiform, lenticular,
patchy or pocket deposits of varying dimensions.
• Psilomelane, pyrolusite, wad and polianite are the important minerals
of manganese ore.
• Karnataka produces about 22% of the total manganese ore in the
country. The total reserves in the state stands at 60,56,000 tonnes.
• It is found to occur in Belgaum, Bellary, Chickmagalur, Chitradurga,
Davangere, Uttara Kannada, Shimoga and Tumkur districts
12. Bauxite
• Karnataka accounts for about 2%
of total production of bauxite.
• Bauxite generally occurs as irregular
pockets within a length of about 130 km.
• In situ deposits formed from and occur over meta-basalt, phyllite and
greywacke.
• The thickness of laterite ranges upto 15 m of which the bauxite horizon
is seen 9 m below the surface level with the thickness ranging from 3
to 5 m.
• Bauxite underlies ferruginous laterite and overlies a clay horizon.
• It is found in Belgaum, Chickmagalur, Uttara & Dakshina Kannada and
Udupi districts.
13. Chromite
• The state is one of the leading producers of chromite in the country.
• Chromite occurs in altered ultrabasic rocks (serpentinised dunites
and peridotites) in the form of veins, lenses and segregated
pockets.
• They occur in Chickmagalur, Hassan and Mysore districts.
• In the Byrapur deposit of Hassan district., there are three thick
lenticular bodies and a few thin lenses and veins cutting across the
schistosity of the ultrabasic rocks. The Cr2O3 content ranges from
48-52%
• The state have a total reserve of 0.745 million tonnes of chromite.
14. Copper
• Only a few small low grade deposits of
copper are known from Karnataka.
• But a number of occurrences of
basemetal mineralisation, particularly
copper mineralisation have been recorded.
• It is found i) in association with the greenstone belts of the Dharwar
Supergroup. ii) in association with sheared quartz veins and metabasic
rocks traversing the granitoids, iii) in association with ultramafic
complexes.
• Copper occurs in Chickmagalur, Chitradurga, Gulbarga, Hassan, Uttara
Kannada, Raichur and Shimoga districts.
• The copper ores also carry considerable silver and gold content.
• Copper reserves in the state is estimated as 2510000 tonnes.
15. Molybdenum
• Molybdenum in the state is found associated with copper deposits.
• Sparse disseminations of molybdenite have been noticed in the
later phase of the Peninsular Gneiss and in younger alkali-feldspar
granites or at the interface of pegmatite veins and quartz reefs; as
yet no economic deposit of molybdenite has come to light.
• The total reserves in the state is about 1.32 million tonnes.
• Molybdenum is found to occur in Kolar and Raichur districts.
16. Nickel
• Sparse disseminations of nickel sulphides occur associated with
mafic-ultramafic rocks at Gowanahalli, Mysore district and the
Kaiga-Mothimakki area of North Kanara district.
• In addition, relative enrichment of nickel in saprolitic horizons of
laterite profiles developed over ultramafic bodies have also been
recorded from Golahalli, Byata area of Bangalore district.
• Nickel values of upto 1.03% with an average of 0.38% have been
recorded from Golahalli-Byata area.
• Nickel reserves in the state is estimated as 0.23 million tonnes.
17. Tungsten
• Karnataka accounts for about 42% of the total tungsten productionin
the country.
• Incidence of scheelite associated with gold mineralisation is known
from the Kolar Gold Field, Hutti Gold Mines, Gadag Gold Field and
Chitradurga schist belt.
• The chief sources of tungsten are minerals scheelite (CaWO4) and
wolframite[(Fe,Mn)WO4] which are deposited by hydrothermal
solutions.
• Its occurrence is found in Gadag, Kolar and Raichur districts. Incidence
of tungsten mineralisation is reported from Gulbarga district also.
18. Titanium-vanadium
• Titaniferous-vanadiferous magnetite bodies occur as late stage
differentiation of a maficultramafic complexes and are associated with
both Dharwar and Sargur Group of rocks.
• Titanium and Vanadium bearing magnetite deposits occur associated with
layered gabbro-anorthosite complexes which have intruded the Nuggihalli
and Shimoga schist belts.
• The Ti-V magnetite deposits are the result of magmatic differentiation of
basic magma.
• The total reserves of Vanadium in the state is about 500,000 tonnes.
• Vanadium occurs in Hassan, Uttara Kannada and Shimoga districts.
20. Clay
• Clay occurrences in the state can be classified mainly into three
categories: a) Kaolin, produced by the weathering and decomposition of
granitic rocks, (b) alluvial clay found in the stream courses and terraces
and in tank beds, and (c) lithomergic clay occurring below the extensive
laterite cappings noticed in several parts of the state, particularly on the
Western Ghats.
• China clay occurs in Bengaluru, Belgaum, Bellary, Bidar, Chickmagalur,
Dharwad, Gadag, Hassan, Haveri, Kolar, Uttara & Dakshina Kannada,
Shimoga and Tumkur districts.
• Fire clay occurs in Bengaluru, Chitradurga, Dharwad, Hassan, Kolar,
Shimoga and Tumkur districts.
• The total reserves of china clay and fire clay in the state are estimated to
be 12.85 million tonnes and 8.77 million tonnes, respectively.
21. Dolomite
• The dolomite deposits are categorised as complex deposits
forming part of folded sequence of Bagalkot Group of rocks and
interbedded with shale and limestone sequence.
• A possible reserve of 1112 million tonnes and a probable
category reserve of 16 million tonnes of dolomite deposit have
been estimated in Belgaum and Bijapur districts respectively.
• Dolomite has been found in Bagalkot, Belgaum, Bijapur,
Chitradurga, Mysore, Uttara Kannada and Tumkur districts.
22. Magnesite
• Magnesite occurs as veins traversing serpentinised
dunite/peridotites.
• Economic deposits of magnesite occur in Mysore district.
• Occurrence of small and impersistent veins are reported in Hassan
near Kushalnagar and at Gaddehosahalli near Arkalgud in Coorg
district.
• Many of the altered ultramafics around Kushalnagar near Torenur,
Argod and Rangaswamybetta contain minor magnesite veins.
• Magnesite reserves in the state have been estimated to be 1.229
million tonnes.
23. Feldspar
• Feldspar is mined from coarse pegmatites.
• It is being produced on a small scale from a number of
localities mainly from Bangalore, Mysore, Hassan, Tumkur and
Raichur districts.
• The bulk of the production, however is from Bangalore
district.
• Feldspar is recovered from coarse pegmatite reef traversing
granite gneiss at Neralemaradi Doddi and at Chickbanavara of
Bangalore district.
• The total resources in the state is about 6288 mllion tonnes.
24. Baryte
• The baryte occurrence in the state has been found to occur
in association with fuchsite quartzite and chert or as thin
and interbedded with sillimanite quartzite or as in
persistent thin beds of nodular barytes.
• Baryte reported to occur in the districts of Chitradurga,
Mysore, Gulbarga and Bijapur.
25. Kyanite-Sillimanite
• Kyanite and sillimanite are constituents of high grade pelitic schists
of Sargur Group.
• Kyanite is found to occur in Chickmagalur, Chitradurga, Coorg,
Mandya, Mysore, Shimoga and Dakshina Kannada districts.
• Sillimanite has been found in Hassan, Mysore and Dakshina
Kannada districts.
• Kyanite and sillimanite bearing schists are observed within the
western and southern extension of Holenarsipur schist belt in
Hassan district, in the Gopalapura-Sargur- Nuguvakankote belt in
Mysore district, in Ghattihosahalli and Kudineerkatte belts in
Chitradurga district.
26. Silica sand
• The silica sand is fine grained and light grey to light honey yellow
in colour.
• The frequency curves of grain size show a general reduction in
the grain size of sand from south to north and west to east.
• The silica sand occurs in Bagalkot, Bengaluru, Belgaum, Bellary,
Chickmagalur, Chitradurga, Davangere, Dharwad, Gadag,
Gulbarga, Hassan, Haveri, Kolar, Koppal, Mandya, Mysore, Uttara
& Dakshina Kannada, Raichur, Shimoga, Tumkur and Udupi
districts
• The estimated recoverable reserves are 17.02 million tonnes.
27. Steatite/Soapstone
• Steatite is a massive variety of talc (hydrothermally altered
ultramafic rock.
• Steatite occurs associated with ultramafic rocks of the Sargur
Group and Bababudan Group.
• The steatite occurs in Bellary, Chickmagalur, Chitradurga,
Hassan, Mandya, Mysore, Raichur and Tumkur districts.
28. Corundum
• Corundum occurs in a large number of localities in the state such as
Bengaluru, Bellary, Chitradurga, Coorg, Hassan, Mandya, Mysore
and Tumkur districts.
• Corundum bearing cordierite-sillimanite schist/gneiss occur on
either side of Closepet Granite as enclaves in Peninsular Gneisses.
• Corundum is also developed at the contact of ultramafics and
pegmatite/aplite veins intruding them, and also as disseminated
grains in anorthosite.
• The bulk of the corundum, thus collected is of abrasive (industrial)
quality and a very small proportion of them form gem quality
popularly known as ruby and sapphire.
29. Ochre
• Red and yellow ochres occur associated with
laterite, ferruginous shales, iron ore and banded
ferruginous quartzites.
• Ochre is found to occur in Bellary and Bidar
districts.
30. Asbestos
• Asbestos, mainly the anthophyllite and tremolite variety
with some chrysotile and amosite occurs in a large number
of localities in Bellary, Bijapur, Chikmagalur, Hassan,
Mandya, Mysore, Shimoga and Tumkur districts.
• The anthophyllite-tremolite and chrysotile varieties are
associated with serpentinites and the amosite variety
occurs as layers in Banded Iron Formation.
31. Fuller’s Earth
• Fuller’s Earth is known to occur mainly in Gulbarga and
Belgaum districts, in association with Deccan lava flows.
• Fuller’s Earth occurs as 1 to 1.5 m thick bands below a soil
cover ranging in thickness upto 1.5 m.
• It is usually exposed in a nala section and tank beds.
• The total reserves of Fuller’s Earth in Gulbarga district are
estimated to be 11 lakh tonnes and in Belgaum the inferred
reserve is 4 lakh tonnes.
32. Vermiculite
• Vermiculite has been noticed at the contact of ultrabasic rocks
with the intruding pegmatite/aplite veins.
• Vermiculite forms narrow lenticular masses and patches
varying from a few centimeters to 8 m wide.
• Economically significant deposits are confined to Mysore and
Hassan districts.
33.
34. Conclusion
• Karnataka State occupies the premier position with regard to the
known resources of gold, manganese ore, magnetite and limestone
in the country.
• The percentage of the total resources contributed by the state
being 64% for gold, 36.5% for manganese ore, 80% for magnetite
and 22.5% for limestone.
• Karnataka has substantial resources of haematite, bauxite,
chromite, dolomite, quartz and silica sand alongwith various types
of clay, fuller’s earth, titaniferous/vanadiferous magnetite and talc,
steatite (soapstone).
• The value of mineral production in Karnataka at
• Rs. 7,508 crore in 2010-11 increased by about 24% as
• compared to the previous year.
35. Reference
• Geological Survey of India. Geology and Mineral
resources of the states of India. Part VII –
Karnataka and Goa. 2006. Bangalore.
• Indian Bureau of Mines. Indian Minerals
Yearbook 2011 (Part I). State Reviews(Karnataka).
2012. 50th Edition
• Krishnaswamy. Mineral Resources of Karnataka.
1976.
• R.K Sinha and N.L Sharma. Mineral Economics.
Third Edition.1980