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education are the greatest social achievements of the Soviet people. Education at Soviet higher school is free.

There are different types of higher educational establishments in the country, namely, universities, pedagogical institutes, engineering institutes, etc. Engineering institutes, for example, specialize in mining, metallurgy, oil, machine building, chemical technology, electrical engineering, etc.

According to

the demands of economy, science

and culture

the Soviet state determines the list of professions which

the

institutes offer.

 

 

The training of specialists now takes place

in proximity

to industrial

enterprises, collective farms and

plants.

The

institutes keep in touch with these enterprises. Thus, education

is closely connected with scientific, technical,

cultural

and

social

progress and industrial development.

 

 

The curricula consist of three basic divisions: the social

sciences, general science which forms the basis

for the study

of specialized subjects and the subjects which

determine

the

type

of specialization and qualification.

 

 

Electronics has become part of modern higher school. Programming and electronic computer technique are compul-

sory

for most

higher schools.

A

new trend in development of higher education deals

with

training

specialists in environmental protection. Envi-

ronmental protection has become a vital principle of state policy in the USSR.

Laboratory work is an important part of the curriculum. Its aim is to teach the students the latest methods of scientific research and experimentation, to familiarize them with modern equipment and apparatus.

Soviet higher educational establishments offer different specializations which the students may take. Thus, at the geological institutes the students specialize in geology, the science which deals with different problems connected with the earth, its history, the study of rocks, their physical and chemical properties. One of the main tasks of geology is to discover and study the deposits of useful minerals.

The Mining Institutes also offer different specializations. For example, students may leave the Mining Institute as mining engineers, mining mechanical engineers or as mining

electrical

engineers.

 

It is quite obvious that modern mining engineers must

know a wide range of subjects. In their future work

they will

deal with

the

discovery and prospecting of mineral fields,

the driving of

tunnels and hoisting of minerals and

men, the

280

transport

facilities

and mineral processing on

the surface.

They will

also deal

with ventilation and air

conditioning,

rock mechanics, surveying, mineral technology, geology and planning.

The profession of engineer is one of

the most widespread

in the Soviet Union and requirements for this

profession are

growing. Engineers of a

new type cannot be

trained apart

from modern production,

science and

technology.

One of the main principles of the Soviet educational system is its close links with life and practical work. The students go through practical training at industrial enterprises, work at factories, etc. Thus, a student of an engineering institute becomes familiar with all the stages of production and every job from worker to engineer. He gets to know the given enterprise, its equipment, technology, economy, management system, organization of work and wage system. During this period students of engineering institutes study the whole production (a factory shop, department, section, design office and laboratory). Here he gets practical knowledge and experience necessary for his diploma paper.

A lot of students belong to students' scientific societies.

Students take part in the research projects which their

depart-

ments usually conduct, they study various

industrial

techno-

logical processes, they design and build

new

equipment,

offer suggestions on improvements according to the

requests

of industrial enterprises. Many thousands

of postgraduates

carry out extensive researches in different

fields

of

science

and engineering.

 

 

 

The student organizations (trade unions and the Young Communist League) of higher schools are in charge of students' welfare. The students take an active part in socially useful work. There are student amateur performers' groups, sports groups and clubs. There are concerts, lectures and films for

students.

 

 

 

Soviet students take an active part in the social

life of

their country. They

lecture

at the factories, plants, col-

lieries, open-cast and

construction sites bringing the

latest

scientific knowledge

to the

people.

 

The students of Soviet higher school have a tradition to spend their summer vacation working at industrial enterprises, construction sites and in the fields. As is known, construction teams quickly gained popularity and have achieved mass scale now.

The Soviet government takes care of young specialists. There is no unemployment in our country. Every year young

19—2132

2 8 1

engineers, geologists, economists, teachers, doctors and agronomists come to all branches of industry, agriculture, science and culture.

© S O M E FACTS ABOUT GREAT BRITAIN

 

Great Britain

is an industrial capitalist country.

Brit-

ain's traditional

industries were textile manufacture,

ship-

building and coal mining — with its 300 years of reserves —

as major energy source. Leading branches of British

industry

are power engineering, electronic equipment

manufacture,

machine-tool

construction, aircraft, motor-car and

chemistry

but Britain's engineering is the major branch of

industry.

Great Britain is not rich in natural

resources.

Britain's

own natural

resources are inadequate to

supply

its

industry

with essential raw materials.' The only exception is coal which is of good coking quality. Over the last decade the number of mines reduced from 246 to 175. The British miners fought against the closure of mines and a lot of them lost their jobs. „Nevertheless coal reserves are still enough to supply the country with energy. The main consumers of coal are power stations, industry and homes.

In 1965 gas was discovered in the North Sea off Britain's shores and in 1969 oil was discovered in the North Sea. The

reserves of non-ferrous

metal ores are inconsiderable.

Iron

ore production supplies

less than half the total needs and

the

iron ore is low-grade. Britain has to import high-grade iron

ore

from

other countries.

 

In Great Britain deposits of hard coal are found through-

out

the

country. The most efficient coal deposits are in

Yorkshire, Nottinghamshire, and Derbyshire which form the largest and most important coal-field in Britain. The coking coal deposits are also found in Durham and Northumberland

deposits are found in Scotland, South Wales and

Kent.

The mechanization of underground operations

began in

the mid-1950s —• first with coal cutting machines,

then with

power loading machines, and then with self-advancing powered roof supports.

Open-pit operations represent a relatively small proportion.

It is quite obvious that now economy depends on joint

efforts

of educational institutions and

industry.

In

Great Britain there are different

educational institu-

tions where students can get higher education. These are universities with extra-mural and evening departments,

282

university colleges and different courses. The oldest and best known universities of Great Britain are those in Oxford and Cambridge. Oxford is the oldest university, its history goes back to the twelfth century. There are also universities in London, Liverpool, Manchester and Nottingham and in other cities. Each university consists of a number of departments such as medicine, philosophy, natural sciences, economics, engineering, agriculture, education and others. After three years of study, a student may proceed to a Bach-

elor's degree and

later to

the degrees of Master and Doctor.

In Great Britain the tuition

fee at

universities

and

col-

leges is

high and besides a degree

is no

guarantee

of a

job.

One of the most marked features of recent education is the

increasing attention given

to engineering education.

 

At present there are a

number of

technical

colleges

and

departments of universities

which give instructions in.(enei;,.

neering,

mining,

geology,

etc. Such

colleges

p f o v f d e f u u -

time and part-time education. They confer diplomas but not degrees. For example, there are colleges which aim at providing mining engineers who have several years' practical experience in the industry with a chance to broaden their knowledge of administration and operation. The subjects include economic geology, computer techniques, statistics, rock mechanics, industrial psychology and operations research.

Laboratory and field work help the students determine the

behaviour

of

rocks

and

methods of breaking rock-blasting,

drilling,

etc.

The

graduates from these courses can work

in various fields of

mining and geology.

As has been said the students in Great Britain can get

mining

education

at special colleges and at mining depart-

ments

of

universities.

Much attention is paid to training

through post-graduate courses. But a great number of young

British geologists

and mining engineers

are not able to take

advantage of

such courses

through

lack

of

funds.

 

 

4. SOVIET SCIENTIFIC ACHIEVEMENTS

 

 

 

 

 

 

 

The heart

of

scientific

 

research

in

the

Soviet

Union is

the

Academy

of

Sciences,

which

supervises

(руководит)

all

of

the fundamental and applied

research

in

the country.

 

It is difficult to name

a

territory or

region in the USSR

without scientific institutions. The USSR

Academy

of

Sci-

ences has a Siberian branch,

sciences sectors in the

Far

East

and the Urals

and sections

in different

areas of the

Russian

Federation.

 

 

 

 

 

 

 

 

 

 

 

19*

283

 

Each section has its own specialities which largely depend on its geographic peculiarities. Scientists help solve all sorts of problems in all our geographic regions. Scientists on the Kola Peninsula, for example, concentrate on geology, the Urals are a centre for the production of powerful machines, primarily for ferrous metallurgy, etc. Specialists and engineers of the Ural machine-building plant have developed and introduced powerful draglines with buckets having capacity from 10 to 100 cu m and a boom up to 100 m long.

These draglines

are especially efficient

in open-cast

mining

and are now

in

operation.

 

 

In Siberia

the Akademgorodok near Novosibirsk is known

to scientists the

world over. Specialists

from all parts

of the

planet visit the science capital of Siberia, and it is easy to

understand why.

It was there

that a very important discov-

ery was made:

the magnetic

effects of chemical reactions.

The effect of magnetic fields can be used not only for scien-

tific purposes but also to control

a number of

important

industrial

processes such as polymerization, oxidation and

others. Siberian scientists recommend using

blasting in weld-

ing metal

and for fire fighting on

oil and

gas wells.

Oil, coal and gas are Siberia's chief wealth. The Siberian

Branch of

the USSR Academy of

Sciences

has

worked out

the volumetric and genetic method of estimating the deposits

of oil and gas. This method

has helped

discover a

number

of deposits in

the sedimentary layer of the Earth.

 

 

Specialists

from the USSR

Academy

of Sciences have

de-

veloped a device which can

be used

in

prospecting

for

oil

and gas and in various other areas of

geophysics. The

device

is a tracing gas-analyser designed on the basis of diode lasers. Work is under way today to develop the energy technology under which the coal without access of air, is heated to 1000° С and divided into resin, bensol, coke and semi-coke, and coal. It is easy and advantageous to transport liquid and gaseous fuels for electric power production and transport

vehicles.

A considerable part of the Far-Eastern Centre's research is oriented toward geology. Geologists have compiled a pa-

leovolcanic map of the Far

E ^ .

Jgcsearch

is

under way on

the shelf

now. The

devel8|menf

of

resources

on

the

shelf

is a problem of world importance.

The

USSR

cooperates

with many countries and the fruits of

mutually

advantageous

economic,

scientific

and

technical

co-operation

are

quite

obvious.

 

 

 

 

 

 

 

 

 

Rapid progress in science and technology calls for a contin-

284

uous and growing renewal of scientific ideas and developments. The decisive role here is played by the researches of the Academy of Sciences of the USSR which has splendid

traditions and outstanding

achievements.

( P MINERAL DEPOSITS

 

Minerals that make up

the rocks, are defined as inorganic

substances which occur naturally and have a definite chemical composition and physical properties which vary within known limits.

 

Tlje major properties which are used for identification

fftfrposes

are

1) colour; 2) crystal form, where available,

although

most

minerals do not show well-developed

crystals;

3) cleavage which is the property of minerals to split

along

one or more

series

of

parallel

planes;

4)

specific

gravity;

5) hardness which refers to the ability of

minerals

to scratch

or to be scratched; 6) lustre which is described in such

terms

as metallic, glassy, etc. Of these diagnostic

properties, colour

is,

perhaps,

the least

useful. Cleavage,

on

the other

hand,

is

one of

the

most

diagnostically

useful

mineralogical

prop-

erties

that is repeated throughout the mineral.

 

 

 

 

Minerals of use to man can be grouped into two broad

categories:

1)

metals,

such

as

aluminium, copper,

gold,

silver,

iron,

 

tin,

platinum,

chromium,

nickel,

 

lead

and

zinc,

and

2)

non-metals such

as

diamonds,

salt,

limestone,

cement, sulphur, and asbestos. When minerals occur so that they can be worked at a profit they are called ore deposits. Mineral depositsx^re seldom equally rich throughout. After their formation miheral deposits may be deformed by folding, faulting, etc.

Economic minerals are those which are of economic importance and include both metallic (ore minerals) and non-

metallic minerals,

as

cryolite

and

sulphur.

The distinction between metallic and non-metallic de-

posits is at times

an

arbitrary

one.

The principal reasons

for distinguishing non-metallic deposits from metallic are practical ones and include such economic considerations as

methods of recovery and

uses.

 

As has been said, the Earth's crust consists of

igneous,

sedimentary and metamorphic rocks. A convenient

way of

discussing mineral deposits is

to classify them on the basis

of the geologic processes

that

have created them,

namely,

igneous activity, weathering, sedimentation and the formation of the original rock masses.

285

As is known, most minerals are compounds of several elements and it is rare to find pure elements occurring naturally. Elemental composition of the Earth's crust is mostly based on igneous and sedimentary rocks. Such elements as oxygen, silicon, titanium, aluminium, iron, magnesium,

calcium,

sodium,

potassium

and

hydrogen make

up more

than 99

per cent

by weight

of all

the rock-forming

minerals,

Of these, aluminium, iron and magnesium are industrial

metals. The other metals are present in small

quantities,

mostly

in

igneous rocks.

 

 

 

Every mineral deposit has limited

dimensions. All

mineral

deposits are exhaustible. Many of common metals

such as

lead and tin, chrome, nickel, zinc

and copper

are really

rather

rare

and form only a small

per cent of

the

Earth's

crust. It is quite obvious that in future people will use new chemical, physical and biological methods of prospecting. They will develop new refining methods that are effective

with

very low-grade ores.

 

 

 

It

has' already been stated that mineral

deposits are gener-

ally classified on the

basis

of the

geologic processes respon-

sible

for their formation. They may be magmatic,, contact,

metasomatic,

pegmatitic,

hydrothermal,

sedimentary, re-

sidual

and

regional

metamorphic

deposits.

Magmatic deposits originated by cooling and the crystallization of magma and the concentrated minerals form part of the body of the igneous rocks. Magmatic deposits are relatively simple in mineral composition and few in number.

 

Pegmatites,

for example,

are

relatively

coarse-grained

 

rocks found in igneous and metamorphic regions. The great

 

majority of them consists of fejdspar and quartz, often accom-

 

panied by mica, but

complex

pegmatites contain

unusual

i

minerals

and rare elements. Many pegmatites are

regular

i

tabular

bodies;

others

are highly

irregular.

 

 

 

b= e *Sedimentary deposits are bedded deposits

derived from

 

pre-existing material by weathering, erosion,

transportation,

 

deposition and consolidation. Sedimentary deposits

are

the

 

extensive coal beds of the world, the great

petroleum

re-

 

sources, clay deposits, limestone and dolomite

beds,

sulphur

 

deposits,

etc.

 

 

 

 

 

 

 

Chemical evaporites consist of soluble salts formed by evaporation, in closed or partly closed shallow basins. Deposits of gypsum and common salt (halite) are found in many countries, whereas the larger concentrations of potash salt, borates and nitrates are much more restricted in occurrence.,

The most important economic placer deposits are those

286

formed by stream action. Stream and beach placers are widespread in occurrence and include the famous gold placers of the world as well as deposits of magnetite, ilmenite, rutile,

zircon,

monazite

and

garnet. Placer deposits of diamond

and platinum are less common.

Large residual

deposits of clay bauxite, from which alu-

minium

is extracted,

phosphate, iron and manganese have

been worked in

many

parts of the world. Smaller deposits

of nickel and other minerals have also been worked. Organic deposits are formed by the remains of animals and

plants. For example, coal and peat are formed from plant remains and represent concentrations of carbon from the carbon dioxide of the atmosphere.

Petroleum originates by the accumulation of plant and animal remains. Many limestone and silica deposits are also formed by plant and animal activity.

Some uranium, vanadium, copper and other metalliferous

deposits are

considered

to have formed in part at least by

the

activity

of

organisms.

 

 

Many rocks are valuable in the natural condition, and are

usable

without

having

undergone

changes. Stone has

been

used

for several

thousand

years as

a building material

and

is still

being used today.

Some rocks have commercial

value

because of their chemical properties. Limestone, for example,

is used as a flux in purifying metals. Limestone that

contains

limited

amounts

of

impurities

serves

as the raw

material

in

the

manufacture

of cement.

Phosphate rock

is

derived

from accumulations of animal remains and chemical

precip-

itation

from sea water. It is extremely

important

as a

source

of

agricultural

fertilizers.

 

 

 

 

 

 

Minerals are

subject to changes as chemical

processes

act

upon them.

These changes

may

take place

rapidly or

they may proceed very slowly. For example,

weathering of

minerals

may be important

in the forming of

new

minerals

as

well

as

in

concentrating

them.

Deposits

of carbonates

of

copper,

zinc

and lead have been

formed

from

primary

ores by ground water containing COa. Weathering in some tropical regions has produced important deposits of iron, aluminium and manganese ores.

6. ENERGY RESOURCES IN THE NATIONAL AND WORLD ECONOMY

A tremendous upsurge in world industrialization has been particularly marked in the last quarter of the century. This world-wide economic development has been characterized

287

by the growth rates in the demand for raw materials and

especially for primary energy — the

essential key to indus-

trial progress. It should be noted that

despite the

development

of nuclear energy, the expansion of

off-shore oil

and natural

gas production, the extraction of oil from bituminous sands and oil shales, the liquefaction and gasification of coal, and the use of such sources as geothermal and solar energy, the production of fossil fuels will continue for many years to come. This applies particularly to the production of solid fuels.

 

Fossil fuel geological

reserves on the Earth

are estimated

at

12.5 trillion tons,

over 11 trillion of which

is coal. These

reserves are enough

to

meet

mankind's total

energy

needs

for many hundreds of years. This means that

coal will

have

to

play the role of fuel

as the

basic power-supplying source.

The main sources of energy available to man today are coal, oil, natural gas, water power and atomic energy. For example, atomic energy will undoubtedly continue to increase its contribution but at present this is only a little per cent of the total world energy consumption. There are many problems to be solved in future. These problems are connected with the application of nuclear energy for electricity generation. Much progress is being made with research into nuclear

fusion in

the USSR, the USA and some

other

countries,

but still

there is much to be done in this

field.

 

As for hydroelectric power, this form of energy is responsible only for more than 5 per cent of the total energy consumption, though there is still considerable hydropower potential in the world available for harnessing.

Conventional thermal power stations will remain for a long time the world's source of electric power. The exotic sources, geothermal and solar energy, wind and sea tides at present are not significant enough in the world energy supply.

In the USSR research is being conducted into the economic use of solar energy and its transformation into electric power in desert conditions. However, the most promising trend in solar energy harnessing, as the scientists consider, is the obtaining of hydrogen which is an excellent fuel with a calory

content not less

than that of gasolene. As

a

fuel, hydrogen

is ideal in desert conditions, because

water

is produced

when

it burns. Using desert resources is

a very

attractive

idea,

because nearly

a quarter of all the

Earth's

land

territory

is desert, but only about three per cent of the

globe's

popula-

tion live there.

 

 

 

 

 

 

Geothermal energy is widely used

in the USSR. Scientists

288

are developing the fundamentals of designing and operation of circulation systems which make it possible to utilize the

thermal power of hot rocks. The temperature of the

Earth

rises at an average of one degree Centigrade every

30

metres.

If

we pump

water into

a well

drilled to a depth of

about

3

kilometres,

it will be

turned

into steam. From

technical

point of view, it is not very difficult to do now. A power

potential of the Earth only in

the upper

part of

the

crust

makes

up tons

of

conventional

fuel.

If

only

one

per

cent

of these stocks

is

utilized,

mankind

will

be

provided

with

heat for millions of years.

 

 

 

 

 

 

 

Researches are also conducted into producing non-tradi-

tional

energy

sources, for

example,

biogas. Certain results

have already been obtained in bacterial

gasification of peat

and in bacterial gasification of residual

oil.

 

Ф SOME MORE FACTS ABOUT PROSPECTING AND

EXPLORATION

The search for mineral deposits that

can

be worked is

prospecting. Mineral prospecting normally proceeds from the

general

to

the specific,

from consideration

of

large

regions

to smaller areas within the region, and

finally

to

 

individual

prospects.

Following

a preliminary investigation,

including

a

study

of available maps and reports,

prospecting

may

often be concentrated on smaller areas immediately.

 

 

Prospecting methods may be divided into direct and in-

direct methods. Direct methods include geologic and

photo-

graphy

mapping; the study of guides

to ore;

and

the

field

examination of the surface, supplemented by

panning,

trench-

ing, drilling or sampling. Indirect

methods

are

of

two

main kinds: 1) geophysical methods, which

include

magnet-

ic,

electromagnetic

and

radioactivity

surveys,

both

from

air and on the surface, etc., and 2) geochemical and

botanical

surveys.

 

 

 

 

 

 

 

 

 

 

 

Air photographs are of growing importance to mineral exploration. As is known, the use of air photographs is not new in geological studies but much of the development has been achieved lately.

The detailed application of air photographs to mineral exploration is generally indirect, their use allows the geolo-

gists

to

determine

conditions favourable for economic min-

eralization. Such

conditions may include the presence of

jaults

or

fracture

zones, major igneous intrusions, dykes

and

pegmatites.

Geomorphological information from air

photographs may also be of use in mineral exploration. For example, salt domes may be directly located on air photographs.

289