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 Introduction
 Nonrenewable Resource
 Finite Quantity
 Depth Dimension
 Uncertainty about Quantity
 Uncertainty in Quality
 Uncertainty in Usability
 Geological complexities
 Locational and Distributional peculiarities
 Relationship between Mineral Deposits and Political Boundaries
 Perpetuality of mineral Deposits
 Relationship between minerals and Economy
 High Investment Risk
 Conclusion
 References
 Mineral: Naturally occur, inorganic
substance definite chemical composition.
 Mineral deposits are generally compared to
land, flora & fauna of a country.
 Floral resources are best represented by
forests and faunal resources by wildlife.
 The only common factor of these four assets
is all are natural resources.
 Majority of the mineral deposits have formed in
the geological past involving millions of years &
once a mineral deposit is used up it will not be
replenished.
 This feature contrasts mineral deposits from flora
and faunal resources which can be replenished by
nature in a short span of time involving a couple of
years.
 However these are some exception in case of
sulfur deposits that constantly form from hot
springs & borax deposits of ladak & form
continuously from thermal springs.
 Unlike forest & wildlife resources which are
capable of expanding on their own without
activity of man the quantity of a mineral
deposit doesn’t increase.
 However the use of a mineral deposit & its
mining limit can be extended into
uneconomic occurrences by improvement of
technology or by increases in sale price of
the mineral.
 While other natural resources occur on the
surface mineral deposits are mostly in the
subsurface often extending to 1000s of feet
depth.
 In India the KOLAR gold mine has reached
around 10,000s of feet depth.
 This has significance on the cost of
exploitation of mineral resource also the
depth dimension introduces complexity in
assessing a mineral deposit.
 Mineral deposits not only occur in the
subsurface but also occupy a large volume of
space therefore the quantity of an entire
mineral deposits can’t be measured directly
& indirect methods like drilling, pitting etc.
are employed to estimate the quantity of
mineral deposits.
 Since actual measurements are carried out
only at sample points there is an dement of
uncertainty in estimating the quantity of any
mineral deposits.
 As in the case of estimating the quantity, the
quality or grade of mineral deposits is
determined by drawing the sample at various
points.
 By analyzing these samples extrapolations
are made for estimating the grade of entire
deposits.
 Further mineral deposits are not homogenous
in term of chemical or mineralogical
composition. All these factors introduce
complexities in estimating the grade of a
mineral deposit.
 The usability or application of a mineral also
depends on many other factors like price,
availability of mining and processing
technology, infrastructure, accessibility,
discovery of new mineral deposits etc..
 Therefore issues related to usability of
mineral deposits depends on a numbers of
interconnected factors each of which has an
element of uncertainty.
 Since mineral deposits form by a variety of
geological processes there are diverse type
of controls of mineralization which result in
variations in size, shape, quality, form &
depth of mineral deposits.
 Deposits of two or more minerals may be of
the same form or the same mineral may
occur in a variety of forms. This peculiarity
of mineral deposits is not noted in any other
natural resource.
 Mineral deposits having formed from natural
processes without intervention by human beings
are unevenly distributed in the earth’s crust.
 Therefore no country is sufficient in all mineral
although the fertility of the land can be improved
by artificial means
 Areas of agricultural resources can be changed &
forests can be shifted by means of afforestation
program. Mineral deposits have fixed location &
can’t be changed.
 Land surface can be divided into countries,
states, districts & cities whereas mineral
deposits being located on surface as well as
subsurface can’t be subjected to such
divisions or political boundaries.
 A fertile land may become a desert in course
of time & trees may decay either naturally or
due to climatic factors or wild animals die
naturally, but no such thing can happen to
mineral deposits.
 A mineral deposits if not exploited will
remain intact & only under rare
circumstances natural calamities like
volcanic eruption & Earthquake may slightly
disturb the form of mineral deposits.
 Minerals are base for all industrial &
agriculture based products & represent the
foundation of the economy of any country.
 Minerals deposits in the past, present &
future occupy a distinctive place in the
economic resource of any country.
 Many of the uncertainties associated with
mineral deposits about quantity, quality,
usability & geological complexity makes
investment in mining of mineral deposits a
highly risky venture compared to other
industries.
 Added to this risk element is the fairly long
gestation period associated with mining.
 Minerals are nonrenewable resource and
never changing.
 Mineral deposits are generally compared to
land, flora & fauna of a country.
 Minerals are base for all industrial &
agriculture based products & represent the
foundation of the economy of any country.
 Minerals deposits in the past, present &
future will occupy a distinctive place in the
economic resource of any country.
Reference:
 Kaulir Kisor Chatterjee, An Introduction to Mineral
Economics by PP (8-15) Publisher, H.S.Poplai for Wiley
Eastern Limited, New Delhi.
 K.Sinha and N.L.Sharma, Mineral Economics (Fourth
Edition) by PP (8-13), Published by Mohan Primlani For
oxford & IBH publishing Co.Pvt.Ltd , New Delhi
Website
 http://en.wikipedia.org/wiki/mineral deposits
 http://en.wikipedia.org/wiki/peculiarities in mineral
deposits

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Peculiarities in mineral deposits

  • 1.
  • 2.  Introduction  Nonrenewable Resource  Finite Quantity  Depth Dimension  Uncertainty about Quantity  Uncertainty in Quality  Uncertainty in Usability  Geological complexities  Locational and Distributional peculiarities  Relationship between Mineral Deposits and Political Boundaries  Perpetuality of mineral Deposits  Relationship between minerals and Economy  High Investment Risk  Conclusion  References
  • 3.  Mineral: Naturally occur, inorganic substance definite chemical composition.  Mineral deposits are generally compared to land, flora & fauna of a country.  Floral resources are best represented by forests and faunal resources by wildlife.  The only common factor of these four assets is all are natural resources.
  • 4.  Majority of the mineral deposits have formed in the geological past involving millions of years & once a mineral deposit is used up it will not be replenished.  This feature contrasts mineral deposits from flora and faunal resources which can be replenished by nature in a short span of time involving a couple of years.  However these are some exception in case of sulfur deposits that constantly form from hot springs & borax deposits of ladak & form continuously from thermal springs.
  • 5.
  • 6.  Unlike forest & wildlife resources which are capable of expanding on their own without activity of man the quantity of a mineral deposit doesn’t increase.  However the use of a mineral deposit & its mining limit can be extended into uneconomic occurrences by improvement of technology or by increases in sale price of the mineral.
  • 7.  While other natural resources occur on the surface mineral deposits are mostly in the subsurface often extending to 1000s of feet depth.  In India the KOLAR gold mine has reached around 10,000s of feet depth.  This has significance on the cost of exploitation of mineral resource also the depth dimension introduces complexity in assessing a mineral deposit.
  • 8.  Mineral deposits not only occur in the subsurface but also occupy a large volume of space therefore the quantity of an entire mineral deposits can’t be measured directly & indirect methods like drilling, pitting etc. are employed to estimate the quantity of mineral deposits.  Since actual measurements are carried out only at sample points there is an dement of uncertainty in estimating the quantity of any mineral deposits.
  • 9.  As in the case of estimating the quantity, the quality or grade of mineral deposits is determined by drawing the sample at various points.  By analyzing these samples extrapolations are made for estimating the grade of entire deposits.  Further mineral deposits are not homogenous in term of chemical or mineralogical composition. All these factors introduce complexities in estimating the grade of a mineral deposit.
  • 10.  The usability or application of a mineral also depends on many other factors like price, availability of mining and processing technology, infrastructure, accessibility, discovery of new mineral deposits etc..  Therefore issues related to usability of mineral deposits depends on a numbers of interconnected factors each of which has an element of uncertainty.
  • 11.  Since mineral deposits form by a variety of geological processes there are diverse type of controls of mineralization which result in variations in size, shape, quality, form & depth of mineral deposits.  Deposits of two or more minerals may be of the same form or the same mineral may occur in a variety of forms. This peculiarity of mineral deposits is not noted in any other natural resource.
  • 12.  Mineral deposits having formed from natural processes without intervention by human beings are unevenly distributed in the earth’s crust.  Therefore no country is sufficient in all mineral although the fertility of the land can be improved by artificial means  Areas of agricultural resources can be changed & forests can be shifted by means of afforestation program. Mineral deposits have fixed location & can’t be changed.
  • 13.  Land surface can be divided into countries, states, districts & cities whereas mineral deposits being located on surface as well as subsurface can’t be subjected to such divisions or political boundaries.
  • 14.  A fertile land may become a desert in course of time & trees may decay either naturally or due to climatic factors or wild animals die naturally, but no such thing can happen to mineral deposits.  A mineral deposits if not exploited will remain intact & only under rare circumstances natural calamities like volcanic eruption & Earthquake may slightly disturb the form of mineral deposits.
  • 15.  Minerals are base for all industrial & agriculture based products & represent the foundation of the economy of any country.  Minerals deposits in the past, present & future occupy a distinctive place in the economic resource of any country.
  • 16.  Many of the uncertainties associated with mineral deposits about quantity, quality, usability & geological complexity makes investment in mining of mineral deposits a highly risky venture compared to other industries.  Added to this risk element is the fairly long gestation period associated with mining.
  • 17.  Minerals are nonrenewable resource and never changing.  Mineral deposits are generally compared to land, flora & fauna of a country.  Minerals are base for all industrial & agriculture based products & represent the foundation of the economy of any country.  Minerals deposits in the past, present & future will occupy a distinctive place in the economic resource of any country.
  • 18. Reference:  Kaulir Kisor Chatterjee, An Introduction to Mineral Economics by PP (8-15) Publisher, H.S.Poplai for Wiley Eastern Limited, New Delhi.  K.Sinha and N.L.Sharma, Mineral Economics (Fourth Edition) by PP (8-13), Published by Mohan Primlani For oxford & IBH publishing Co.Pvt.Ltd , New Delhi Website  http://en.wikipedia.org/wiki/mineral deposits  http://en.wikipedia.org/wiki/peculiarities in mineral deposits