Urban morphology

 

Urban morphology is the study of the form of human settlements and the process of their formation and transformation.Morphological studies often deal with development of forms and
pattern of the present city or other urban areas through time.

Urban morphology is the study of the physical form of a city, which consists of street patterns, building sizes and shapes, architecture, population density and patterns of residential, commercial, industrial and other uses, among other things. Special attention is given to how the physical form of a city changes over time and to how different cities compare with each other.

India exhibits a very stable settlement structure such that much of the urban growth that has occurred has been because of the accretion to existing towns and settlements and only marginally because of the emergence of new towns. As a result, the proportion of urban population residing in towns above a certain population cut-off point continues to increase, but there is little evidence of correlation between city size and rates of population growth.

In other words we can state that the development of new urban centers in India has been minimal and the urban growth has been accredited to the development of existing centers.

Prof. E. Ahmad has identified some of the components of urban morphology as site characteristics, historical background, sky-line, green open spaces, and water bodies, physical and cultural dominants.

For the Census of India 2011, the definition of urban area is as follows;

  1. All places with a municipality, corporation, cantonment board or notified town area committee, etc.
  2. All other places which satisfied the following criteria: i) A minimum population of 5,000; ii) At least 75 per cent of the male main working population engaged in non-agricultural pursuits; and iii) A density of population of at least 400 persons per sq. km.

Urban centres of India are of 4 types:
1. Those that have grown from ancient town and villages e.g. Varansi, Madurai, Patna

  1. Those that have grown from medieval towns such as Lucknow, Delhi, Jaipur. These towns have lot of features of medieval Islamic architecture with palaces, minarates, walled city with Meena bazaars.
  2. Cities that have grown from the British administrative centres. Most of them were medieval towns or cantonment areas which retain lot of features of European Victorial architecture.
  3. During the post independence period a number of planned cities have been developed. Chandigarh, Bhuvneshwar, Gandhinagar, Dispur and Bokaro are some of the typical examples of planned cities.

City is a complex agglomeration of multiple activities – economic, social, cultural, etc. Its ‘central area’ also known as Central Business District is its distinct section which is identified as the centre of marketing, business and financial activities as well as dense built-up sector where lines of transportation converge from various parts and nearly from all direction.

functional classification of urban settlements Problems of human settlement in India

 
The definition of function varies across the disciplines. In political science it refers to duties, in mathematics it means the relationship between two variables and in geography it is synonymous to occupation.

Geographers have classified towns on the basis of their site, situation, size, rank, location and relative elevation. Functional classification of towns attempts to categorize towns and cities according to their economic functions, thereby identifying their roles within urban systems. Most classifications use employment and occupational data. In the functional classification approach, towns are classified on the basis of their dominant function. The functional classification of towns has been illus­trated in the following paras:

1.)Administrative town

The main function of administrative cities and towns is to administer the country/state or a specific territory.It includes not only the capital cities of countries, but all the centres of provinces, states, districts and other administrative divisions of the country.

2.Defensive Towns:

During the medieval period, most of the towns and cities used to be developed on the defensive sites.Forts and garrisons used to be constructed at strategic places. The defensive towns have barracks, cantonments, and training facilities for the armed forces, airfields, and harbours for warships.Visakhapatnam, MHOW and Khadakwasla (India);

In many garrison and defensive towns, there is a clear division of land use between the civil and military authorities, so that the military installa­tions are often at a little distance from the town or are grouped together in one part of the town. This is necessary to maintain security, though often many town people are employed by the military.

3.Cultural Centres:

There are numerous towns and cities in the world, almost in each of the countries, which perform cultural functions.The cities of Oxford and Cambridge in England are the most suitable examples of educational towns. In these towns, one may find colleges, libraries, hostels, churches, playgrounds, parks and shopping centres. The environmental pollution in these towns is almost insignificant.

4.) Collection Centres:

The mining towns, fishing ports and lumbering centres fall under the category of collection centres/towns. There are numerous metallic, non-metallics, precious stones and energy resources which are obtained from mines.The towns which serve these mines may be small settlements serving a particular mine such as Zawar near Udaipur (Rajasthan), Bjiladela (Madhya Pradesh) and Digboi (Assam).They may be large in size such as Raniganj, Hazaribagh (Bihar), Ipoh in the tin rich Kinta valley of Malaysia, or Kuwait and Abadan in the oil producing regions of Kuwait and Tehran, respectively.Such towns may have some industries related to the mineral mines, such as smelters and refineries. The shops in such towns sell mining equipments and special clothes needed for miners.

5.) Production Centres:

Urban places, town and cities in which some kind of manufacturing industry is the major function is known as a production centre. The size and appearance of the town are affected by the type of industry located there.

  • For example, Jamshedpur, Rourkela, Bhilai, Durgapur, Dhanbad and Bhadravati in India, Pittsburgh in USA, Magnitogorsk in Russia and Birmingham in UK are dominated by large steel plants. Such iron and steel producing towns are generally located near the coal fields.
  • For the manufacturing towns, as collecting centres, transportation is very important for the transport of raw materials and the finished goods. These days such towns are generally set up on lines of communication.

In manufacturing towns, there is a segregation of houses and estab­lishments; the officer’s quarters may be grouped at one place and that of the labourers at the other.

6.) Towns of Diversified Functions:

As stated at the outset, towns are classified according to their major functions. So, all those towns (such as Mumbai, Kolkata, Chennai, etc.) can be put into a definite category in which a large number of activities are conducted. Such towns are referred as diversified in functions.

Over space and time, the functions of towns change. For example, defensive sites often become restrictive when the town expands.Thus, many towns have restricted centres which were once confined within the town walls and more extensive suburbs which grew up outside the walls or after the walls were demolished.

Shahjahanabad (old Delhi), Padova (Italy), Lahore and Rawalpindi (Pakistan), Baghdad (Iraq) and Baku (Azerbaijan) are some of the examples of such towns.

7.)Residential Towns:

In some towns, the chief function is simply to house a concentration of population. In such areas, most of the land is devoted to houses, parks and hospitals. These towns are very- well-connected with the major cities, which enables the commuters to get to work each day.

  1.  Resorts:

The urban places which cater to the recreation needs of people are known as resorts or recreation towns.These urban places may be based on health-giving water (hot springs), seaside recreation, mountain climbing, cultural attractions, historical monuments, sports facilities, national parks and attractive scenery.Resorts and recreational towns have many hotels to accommodate visitors, and also provide sporting facilities such as golf courses, swimming pools, trekking and skiing. Moreover, they have numerous entertainment facilities, such as theatres, cinemas, and night clubs and children parks.

  1. Transfer and Distribution Centres:

The main functions performed at transfer centres are the trade, commerce and services. Towns which are concerned with the transfer and distribution of goods, however, have trade as their major function.

They include several types of towns. For example, market towns, sea ports and financial towns.Market towns are characterized by markets, a wide range of shops, stores, warehouses, godowns, cold storages and wholesale .markets.Market towns also have banks, insurance companies and other financial organizations. Kanpur, Ahmedabad, Vadodara, Indore, Bhopal, Patna, Lucknow, Ludhiana and Hapur in India, Norwich in England, Alexandria in Egypt, and Kumasi in Ghana are some of the examples of such towns.

 

Problem of Human settlement:

Some of the major problems of urbanisation in India are

  1. Urban Sprawl

Urban sprawl or real expansion of the cities, both in population and geographical area, of rapidly growing cities is the root cause of urban problems. In most cities the economic base is incapable of dealing with the problems created by their excessive size

  1. Overcrowding

Overcrowding is a situation in which too many people live in too little space. Overcrowding is a logical consequence of over-population in urban areas. It is naturally expected that cities having a large size of population squeezed in a small space must suffer from overcrowding. This is well exhibited by almost all the big cities of India.

 

3.Slums and Squatter Settlements:

The natural sequel of unchecked, unplanned and haphazard growth of urban areas is the growth and spread of slums and squatter settlements which present a striking feature in the ecological structure of Indian cities, especially of metropolitan centres.

 

4.)Overcrowding

Overcrowding leads to a chronic problem of shortage of houses in urban areas. This problem is specifically more acute in those urban areas where there is large influx of unemployed or underemployed immigrants who have no place to live in when they enter cities/towns from the surrounding areas.

5.)Seweage problem

Urban areas in India are almost invariably plagued with insufficient and inefficient sewage facilities. Not a single city in India is fully sewered. Resource crunch faced by the municipalities and unauthorised growth of the cities are two major causes of this pathetic state of affairs.

Food scarcity

 

According to FAO Food Security  is “a situation in which all people at all times have access to adequate quantities of safe and nutritious food to lead a healthy and active life”.

This definition requires three basic conditions to be met:

1) adequacy, i.e. supplies from domestic production, stocks and imports are sufficient to meet the nation’s needs,

2) availability i.e. stability of supply both spatially and temporally throughout the year and

3) access, i.e. the population has sufficient purchasing power to gain access to its food needs.

India is one of the few countries which have experimented with a broad spectrum of programmes for improving food security. It has already made substantial progress in terms of overcoming transient food insecurity by giving priority to self-sufficiency in foodgrains and through procurement and public distribution of foodgrains, employment programmes, etc. However, despite a significant reduction in the incidence of poverty chronic food insecurity persists in a large proportion of India’s population.

The range of adverse events, including reduced freshwater availability and more frequent extreme weather events, will considerably increase the risks for more efficient crop production and livestock management. Climate change is also likely to affect soil quality by depleting organic matter – a major contributor to soil fertility. In extreme cases, the degradation of the agricultural ecosystems could mean desertification, resulting in a total loss of the productive capacity of the land in question.

Food security is a multidimensional concept covering even the  micro level household food security,energy intakes and indicators of malnutrition.

Major components of food security are:-

  1. Production and Procurement
  2. Storage
  3. Distribution

Indian Agriculture is rightly called as a gamble with Monsoon, variability in food production and rising population creates food insecurity in the nation and worst effected are the downtrodden section of the society.

While India has seen impressive economic growth in recent years, the country still struggles with widespread poverty and hunger. India’s poor population amounts to more than 300 million people, with almost 30 percent of India’s rural population living in poverty. The good news is, poverty has been on the decline in recent years. According to official government of India estimates, poverty declined from 37.2% in 2004-05 to 29.8% in 2009-10.

Need for Self-Sufficiency:

India suffered two very severe droughts in 1965 and 1966. Food Aid to India was restricted to a monthly basis by USA under the P.L. 480 programme.  The Green Revolution made a significant change in the scene. India achieved self-sufficiency in food grains by the year 1976 through the implementation of the seed- water-fertilizer policy adopted by the Government of India.

Food grain production increased four-fold during 1950-51 and 2001-2002 from 51 million tons to 212 million tones. The country is no longer exposed to real famines. But the regional variation in the success of Green Revolution which was chiefly limited to northern- Western states has lead to the divide in the nation. Evergreen revoloution and Bringing green revolution to eastern India is the need of the hour.

Green revolution was focused on wheat and rice and thus the production of pulses was stagnant.

National Food Security Mission comprising rice, wheat and pulses to increase the production of rice by 10 million tons, wheat by 8 million tons and pulses by 2 million tons by the end of the Eleventh Plan (2011-12). The Mission is being continued during 12th Five Year Plan with new targets of additional production of food grains of 25 million tons of food grains comprising of 10 million tons rice, 8 million tons of wheat, 4 million tons of pulses and 3 million tons of coarse cereals by the end of 12th Five Year Plan.
The National Food Security Mission (NFSM) during the 12th Five Year Plan will have five components

(i) NFSM- Rice;

(ii) NFSM-Wheat;

(iii) NFSM-Pulses,

(iv) NFSM-Coarse cereals and

(v) NFSM-Commercial Crops.

Government through Public Distribution System has tried to counter the problem of food insecurity by providing the food grains through fair price shops.

The central Government through Food Corporation of India has assumed the responsibilities of  procurement,storage,transfer and bulk allocation of food grains to state governments.

The public distribution system (PDS) has played an important role in attaining higher levels of the household food security and completely eliminating the threats of famines from the face of the country, it will be in the fitness of things that its evolution, working and efficacy are examined in some details.

PDS was initiated as a deliberate social policy of the government with the objectives of:

  1. i) Providing foodgrains and other essential items to vulnerable sections of the society at resonable (subsidised) prices;
  2. ii) to have a moderating influence on the open market prices of cereals, the distribution of which constitutes a fairly big share of the total marketable surplus; and

iii) to attempt socialisation in the matter of distribution of essential commodities.

The focus of the Targeted Public Distribution System (TPDS) is on “poor in all areas” and TPDS involves issue of     35 Kg of food grains per family per month for the population Below Poverty Line (BPL) at specially subsidized prices. The TPDS requires the states to Formulate and implement :-

  1. foolproof arrangements for identification of poor,
  2. Effective delivery of food grains to Fair Price Shops (FPSs)

Its distribution in a transparent and accountable manner at the FPS level

Drainage System of India

  • Drainage: Flow of water through well-defined channels. Network of such channels is called a drainage system .
  • Drainage basin: An area drained by a river and its tributaries.
  • Watershed: Boundary line separating one drainage basin from other.
  • River basins are larger watersheds.
  • Drainage pattern of an area depends on the geological time period, nature and structure of rocks, topography, rocks, slope, amount of water and periodicity of flow.

Important drainage patterns:

  1. Dendritic: Resembling the branches of a tree. Eg. Northern Plain rivers
  2. Radial: Originate from a hill and flow in all directions. Eg. Rivers in Amarkantak
  3. Trellis: Primary tributaries parallel to each other and secondary tributaries join them at right angles.
  4. Centripetal: Rivers discharge waters from all directions in a lake or depression

A river drains the water collected from a specific area, which is called its catchment area.

Nearly 77 pc of drainage is towards the Bay of Bengal while about 23 pc is towards the Arabian Sea.

The Himalayan Drainage System

Mainly includes the Ganga, Indus and Brahmaputra river basins.

Over the plains, rivers of this system change the course often. River Kosi is also known as the ‘sorrow of Bihar’ due to flooding by its frequent change of course by deposition of sediments.

Evolution

Geologists believe that a mighty river called Shivalik or Indo-Brahma traversed the entire length of the Himalayas some 5-24 million years ago. Over time this got dismembered into the present three major river systems.

The Indus System

Indus river originates from a glacier near Bokhar Chu in Tibet in the Kailash Mountain range. Known as Singi Khamban (Lion’s mouth) in Tibet. It forms a spectacular gorge near Gilgit in J&K. Enters Pakistan near Chillar in the Dardistan region. Flows only through the Leh distt of J&K.

Smaller tributaries: Shyok, Gilgit, Zaskar, Nubra, Hunza, Shigar, Gasting, Dras. On right bank: Kabul river, Khurram, Tochi, Gomal, Viboa and hte Sangar.

Major tributaries: Satluj, Beas, Ravi, Chenab, Jhelum

Jhelum Origin: Verinag at foot of Pir Pinjal.

Flows through Srinagar and the Wular lake. Joins Chenab near Jhang in Pakistan

Chenab Origin: Two streams (Chandra and Bhaga) which join at Tandi near Keylong in HP.

Largest tributary of Indus. Aka Chandrabhaga. Flows for 1180 KM before entering Pakistan

Ravi Origin: Kullu hills of HP near Rohtang Pass. Enters Pakistan and joins Chenab near Sarai Sidhu
Beas Origin: Beas Kund near Rohtang pass.

Forms gorges at Kati and Largi in the Dhaoladhar range. Meets Satluj near Harike.

Satluj Origin: Rakas lake near Mansarowar in Tibet. Known as Langchen Khambab in Tibet.

Enters India at Ropar. Antecedent river. Bhakra Nangal Project is on this river.

 

The Ganga System

It is the largest river system in India.

Ganga rises in the Gangotri glacier near Gaumukh in the Uttarkashi district. Here it is known as the Bhagirathi. At Devprayag, Bhagirathi meets Alaknanda and is known as Ganga hereafter.

Panchprayag

Vishnu Ganga Joshimath

Dhauli and Vishnu Ganga meet to form Alaknanda

   
   
   
   

 

Alaknanda Origin: Satopanth glacier above Badrinath. Consists of Dhauli and Vishnu Ganga.
Yamuna Origin: Yamnotri glacier on Banderpunch range. Joins Ganga at Prayag (Allahabad).

RBT: Chambal, Sind, Betwa, Ken

LBT: Hindan, Rind, Sengar, Varuna.

Agra canal

Chambal Origin: Mhow in Malwa plateau.

Gandhi Sagar dam, Rana Pratap Sagar dam and Jawahar Sagar dam.

Famour for Chambal ravines.

Gandak Origin: In Nepal between Dhaulgiri and Mt. Everest. Enters Ganga plain in Champaran and joins Ganga at Sonpur near Patna.

Two streams: Kaliganfak and Trishulganga.

 

Ghaghra Origin: Glaciers of Mapchachungo

Tributaries: Tila, Seti and Beri

Deep gorge at Shishpani

Sarda (Kali) joint it and meet Ganga at Chhapra.

Kosi Origin: North of Mt. Everest in Tibet.

Tributaties: Son Kosi, Tamur Kosi, Arun

Changes course often. Sorrow of Bihar.

   

 

  • Ganga enters the plains at Haridwar.
  • Left Bank tributaries (LBT): Ramganga, Gomati, Ghaghara, Gandak, Kosi and Mahananda.
  • Right Bank tributaries (RBT): Son
  • Discharges into Bay of Bengal near Sagar island.

 

 

 

 

 

      Energy Resources of India
       
35. Coal Jharkhand Jharia, Bokaro, Giridh, karanpura, Ramgarh, Daltonganj,
      Aurangabad, Hutar, Deogarh, Rajmahal
36.   Orissa Talcher, Rampur
37.   M.P (Former) Central Indian Coalfields -Singrauli, Sohagpur, Johilla, Umaria
      Satupura Coalfields – Pench, Kanhan, Pathkhera
      North Chhattisgarh – Chirmiri-Kaurasia, Bisrampur, Jhillmili,
      Sonhat, Lakhanpur, Sendurgarh, lakhanpur-Ramkola
      South Chhattisgarh-Hasdo-Arand, Korba, Mand-Raigarh
38.   West Bengal Raniganj, Darjeeling

 

 

 

 

 

 

 

39.   Andhra Pr. Singareni, Kothgundam, Tandur
40.   Maharashtra Chanda-Wardha, Kamptee, Bander
41. Tetiary Meghalaya Daranggiri, Cherpunji, Laitryngew, Mawlong, Langrin, Pendengru,
  coal   Longoi, Waimong
42.   Assam Makum, Jaipur, Nazira
43.   Arunachal Pr Namchuk-Namphuk
44.   J & K Kalakot, Mohogala, Metka
45.   Rajasthan Palana (lignite) & Khari
46. Petroleum North-East Digboi, Naharkatiya, Moran, Rudrasagar, Galeki, Hugrijan, Nigru,
      Borholla
47.   Gujarat Ankeleshwar, Kalol, Nawagam, Kosamba, Kathana,
      Barkol,Mehsana, Sanand, Lunej, Aliabet island
48.   Mumbai High Bombay high, Bassein
49.   East Coast Narimanam, Kovillapal, Amlapur, Rawa
50.   Other Jaiselmer, Jwalamukhi Area (Punjab)
51. Natural Mumbai Bombay high, Bassein
52. Gas Gujarat Jagatia, Gogha
53.   Assam Nahorkatiya & Moran
54.   Tamil Nadu Neypaltur, Mangamadam, Avadi, Virugambakam
55.   Tripura Baranura, Atharnure
56.   Rajasthan Barmer, Charaswala
57.   Arunachal Pr Non Chick, Mia-Pung, Laptan pung
58.   Himachal Pr Jwalamukhi, Kangra
59.   West Bengal Medinipur
60. Uranium   Jaduguda (Jharkhand), Bhatin, Narwapahar under Uranium
      Corportation in India are the only mines worked at present
61. Thorium   Beach Sands (Kerala), Tamil Nadu, Andhra Pr, Orissa

 

Drainage Systems Himalayan and the Peninsular

 

Drainage: Flow of water through well-defined channels. Network of such channels is called a drainage system .

Drainage basin: An area drained by a river and its tributaries.

Watershed: Boundary line separating one drainage basin from other.

River basins are larger watersheds.

Drainage pattern of an area depends on the geological time period, nature and structure of rocks, topography, rocks, slope, amount of water and periodicity of flow.

Important drainage patterns:

  1. Dendritic: Resembling the branches of a tree. Eg. Northern Plain rivers
  2. Radial: Originate from a hill and flow in all directions. Eg. Rivers in Amarkantak
  3. Trellis: Primary tributaries parallel to each other and secondary tributaries join them at right angles.
  4. Centripetal: Rivers discharge waters from all directions in a lake or depression

A river drains the water collected from a specific area, which is called its catchment area.

Nearly 77 pc of drainage is towards the Bay of Bengal while about 23 pc is towards the Arabian Sea.

The Himalayan Drainage System

Mainly includes the Ganga, Indus and Brahmaputra river basins.

Over the plains, rivers of this system change the course often. River Kosi is also known as the ‘sorrow of Bihar’ due to flooding by its frequent change of course by deposition of sediments.

Evolution

Geologists believe that a mighty river called Shivalik or Indo-Brahma traversed the entire length of the Himalayas some 5-24 million years ago. Over time this got dismembered into the present three major river systems.

The Indus System

Indus river originates from a glacier near Bokhar Chu in Tibet in the Kailash Mountain range. Known as Singi Khamban (Lion’s mouth) in Tibet. It forms a spectacular gorge near Gilgit in J&K. Enters Pakistan near Chillar in the Dardistan region. Flows only through the Leh distt of J&K.

Smaller tributaries: Shyok, Gilgit, Zaskar, Nubra, Hunza, Shigar, Gasting, Dras. On right bank: Kabul river, Khurram, Tochi, Gomal, Viboa and hte Sangar.

Major tributaries: Satluj, Beas, Ravi, Chenab, Jhelum

Jhelum Origin: Verinag at foot of Pir Pinjal.

Flows through Srinagar and the Wular lake. Joins Chenab near Jhang in Pakistan

Chenab Origin: Two streams (Chandra and Bhaga) which join at Tandi near Keylong in HP.

Largest tributary of Indus. Aka Chandrabhaga. Flows for 1180 KM before entering Pakistan

Ravi Origin: Kullu hills of HP near Rohtang Pass. Enters Pakistan and joins Chenab near Sarai Sidhu
Beas Origin: Beas Kund near Rohtang pass.

Forms gorges at Kati and Largi in the Dhaoladhar range. Meets Satluj near Harike.

Satluj Origin: Rakas lake near Mansarowar in Tibet. Known as Langchen Khambab in Tibet.

Enters India at Ropar. Antecedent river. Bhakra Nangal Project is on this river.

 

The Ganga System

It is the largest river system in India.

Ganga rises in the Gangotri glacier near Gaumukh in the Uttarkashi district. Here it is known as the Bhagirathi. At Devprayag, Bhagirathi meets Alaknanda and is known as Ganga hereafter.

Panchprayag

Vishnu Ganga Joshimath

Dhauli and Vishnu Ganga meet to form Alaknanda

   
   
   
   

 

Alaknanda Origin: Satopanth glacier above Badrinath. Consists of Dhauli and Vishnu Ganga.
Yamuna Origin: Yamnotri glacier on Banderpunch range. Joins Ganga at Prayag (Allahabad).

RBT: Chambal, Sind, Betwa, Ken

LBT: Hindan, Rind, Sengar, Varuna.

Agra canal

Chambal Origin: Mhow in Malwa plateau.

Gandhi Sagar dam, Rana Pratap Sagar dam and Jawahar Sagar dam.

Famour for Chambal ravines.

Gandak Origin: In Nepal between Dhaulgiri and Mt. Everest. Enters Ganga plain in Champaran and joins Ganga at Sonpur near Patna.

Two streams: Kaliganfak and Trishulganga.

 

Ghaghra Origin: Glaciers of Mapchachungo

Tributaries: Tila, Seti and Beri

Deep gorge at Shishpani

Sarda (Kali) joint it and meet Ganga at Chhapra.

Kosi Origin: North of Mt. Everest in Tibet.

Tributaties: Son Kosi, Tamur Kosi, Arun

Changes course often. Sorrow of Bihar.

   

 

Ganga enters the plains at Haridwar.

Left Bank tributaries (LBT): Ramganga, Gomati, Ghaghara, Gandak, Kosi and Mahananda.

Right Bank tributaries (RBT): Son

Discharges into Bay of Bengal near Sagar island.

Scarcity of water, methods of conservation-rain water harvesting and watershed management, ground water management

 

Scarcity of water

 

Water scarcity is possibly to pose the greatest challenge on account of its increased demand coupled with shrinking supplies due to over utilisation and pollution. Water is a cyclic resource with abundant supplies on the globe. Approximately, 71 per cent of the earth’s surface is covered with it but fresh water constitutes only about 3 per cent of the total water. In fact, a very small proportion of fresh water is effectively available for human use. The availability of fresh water varies over space and time.

According to the United Nation Developement Program ,occurrence of water availability at about 1000 cubic meters per capita per annum is a commonly threshold for water indicating scarcity.

Krishna, Cauvery, Subernarekha, Pennar, Mahi, Sabarmati, Tapi, East Flowing Rivers and West Flowing Rivers of Kutch and Saurashtra including Luni are some of the basins, which fall below the 1000 cubic meter mark- out of which Cauvery, Pennar, Sabarmati and East Flowing rivers and West Flowing Rivers of Kutch and Saurashtra including Luni facing more acute water scarcity with per capita availability of water less than or around 500 cu m.

The need of the hour to change the condition of water scarity are as follows:-

  • The need to change cropping patterns based on scientific advice,
  • use of drip and sprinkler irrigation,
  • fertigation for increasing water use efficiency,
  • community participation, especially women, for better water management
  • Use of treated urban waste water to be used for farming in the adjoining areas
  • desilting of rivers
  • recharging of rivers,
  • check dams and other water storage mechanisms.

Rain water harvesting

 

Rain water harvesting generally means collection of rain water. Its special meaning is a technique of recharging of underground water. In this technique water is made to go underground after collecting rain water locally, without polluting the same.

Rain water harvesting is a low cost and eco-friendly technique for preserving every drop of water by guiding the rain water to bore well, pits and wells. Rainwater harvesting increases water availability, checks the declining ground water table, improves the quality of groundwater through dilution of contaminants like fluoride and nitrates, prevents soil erosion, and flooding and arrests salt water intrusion in coastal areas if used to recharge aquifers.

Rainwater is relatively clean and the quality is usually acceptable for many purposes with little or even no treatment. The physical and chemical properties of rainwater are usually superior to sources of groundwater that may have been subjected to contamination. Rainwater harvesting can co‐exist with and provide a good supplement to other water sources and utility systems, thus relieving pressure on other water sources. Rainwater harvesting provides a water supply buffer for use in times of emergency or breakdown of the public water supply systems, particularly during natural disasters.

Watershed management

 

The term watershed refers to a “contiguous area draining into a single water body or a water course” or “it is a topographical area having a common drainage”. This means that the rainwater falling on an area coming within a ridgeline can be harvested and will flow out of this area thorough single point. Some refer it as a catchment area or river basin.

Watershed management is an efficient management and conservation of surface and groundwater resources. It involves prevention of runoff and storage and recharge of groundwater through various methods like percolation tanks, recharge wells, etc. However, in broad sense watershed management includes conservation, regeneration and judicious use of all resources – natural (like land, water, plants and animals) and human with in a watershed.

Integrated Watershed Management Programme  is to restore the ecological balance by harnessing, conserving and developing degraded natural resources such as soil, vegetative cover and water.  The outcomes are  prevention of soil run-off, regeneration of natural vegetation, rain water harvesting and recharging of the ground water table.  This enables  multi-cropping and the introduction of diverse agro-based activities, which help to provide sustainable livelihoods to the people residing in the watershed area.

The main benefits of watershed management are:-

  1. Supply of water for drinking and irrigation.
    2. Increase in bio-diversity.
    3. Loss of acidity in the soil and free for standing water.
    4. Increase in the agricultural production and productivity.
    5. Decrease in the cutting of forests.
    6. Increase in the standard of living.
    7. Increase in employment.
    8. Increase in personal get together by participation of local people.

Ground water management.

 

Scientific management of ground water resources involves a combination of

  1. A) Supply side measures aimed at increasing extraction of ground water depending on its availability and
  2. B) Demand side measures aimed at controlling, protecting and conserving available resources.

The rainfall occurrence in different parts of India is limited to a period ranging from about 10 to 100 days. The natural recharge to ground water reservoir is restricted to this period only and is not enough to keep pace with the excessive continued exploitation. Since large volumes of rainfall flows out into the sea or get evaporated, artificial recharge has been advocated to supplement the natural recharge.

Ground water resources management requires to focus attention on the judicious utilization of the resources for ensuring their long-term sustainability. Ownership of ground water, need-based allocation pricing of resources, involvement of stake holders in various aspects of planning, execution and monitoring of projects and effective implementation of regulatory measures wherever necessary are the important considerations with regard to demand side ground water management.

 

Water Resources : Availability

 

Water is a prime natural resource, a basic human need and a precious national asset. Planning, development and management of water resources need to be governed by national perspectives.

India accounts for about 2.45 per cent of world’s surface area, 4 per cent of the world’s water resources and about 16 per cent of world’s population. The total water available from precipitation in the country in a year is about 4,000 cubic km. The availability from surface water and replenishable groundwater is 1,869 cubic km. Out of this only 60 per cent can be put to beneficial uses. Thus, the total utilisable water resource in the country is only 1,122 cubic km.

There are four main sources of water:

(i) Surface water

(ii) Underground water

(iii) Atmospheric water, and

(iv) Oceanic water

(i) Surface water

Water found on the surface is called surface water. About two – third of the total surface water flows into three major rivers of the country – Indus, Ganges and Brahmaputras. The water storage capacity of reservoirs constructed in India so far is about 17400 billion cubic metres. At the time of independence, the water storage capacity was only 180 billion cubic metres. Hence water storage capacity has increased about ten times.

India’s average annual surface run-off generated by rainfall and snowmelt is estimated to be about 1869 billion cubic meter (BCM). However, it is estimated that only about 690 BCM or 37 per cent of the surface water resources can actually be mobilised. This is because (i) over 90 per cent of the annual flow of the Himalayas rivers occur over a four month period and (ii) potential to capture such resources is complicated by limited suitable storage reservoir sites.

(ii) Underground water

It refers to all water below the water table to great depths. In the soil, both water and air coexist in the pore spaces. A profound consequence is that the capillary water in the soil can only be extracted by plant roots, within certain range of conditions. Ground water, on the other hand can be extracted by humans through wells. Ground water and soil water together constitute the lower part of the hydrological cycle. The annual potential natural of ground water recharge from rainfall in India is about 342.43 km3 , which is 8.56% of total annual rainfall of the country.

Underground water is used on a large scale in the areas where the rainfall is comparatively less. Underground water is used on a large scale in Punjab, Haryana, Rajasthan, Tamil Nadu, Gujarat and Uttar Pradesh whereas Andhra Pradesh, Madhya Pradesh, Maharashtra, Karnatake and Chhattisgarh are such states where inspite of less rainfall, the use of underground water is less. There is a great need to develop underground water resources here.

(iii) Atmospheric water

Evaporation and transpiration change liquid water into vapor, which ascends into the atmosphere due to rising air currents. Cooler temperatures aloft allow the vapor to condense into clouds and strong winds move the clouds around the world until the water falls as precipitation to replenish the earthbound parts of the water cycle. About 90 percent of water in the atmosphere is produced by evaporation from water bodies, while the other 10 percent comes from transpiration from plants.

(iv) Oceanic water

The Ocean plays a key role in this vital cycle of water. The ocean holds 97% of the total water on the planet; 78% of global precipitation occurs over the ocean, and it is the source of 86% of global evaporation. Besides affecting the amount of atmospheric water vapor and hence rainfall, evaporation from the sea surface is important in the movement of heat in the climate system. Water evaporates from the surface of the ocean, mostly in warm, cloud-free subtropical seas.

Major types of Soils.(ICAR classification) and their distribution. Soil degradation and conservation

 

Soil is defined as upper layer of the earth composed of loose surface material. It is a mixture of many substances including endless variety of minerals, remnants of plants and animals, water and air. It is the end product of continuing interaction between the parent material, local climate, plant and animal organisms and elevation of land. Since each of the elements varies over space, soils also differ from place to place. Soil is an important segment of our ecosystem, as it serves an anchorage for plants and source of nutrients. Thus, soil is the seat, the medium and fundamental raw material for plant growth.
Soils are formed from materials that have resulted from the disintegration of rocks by various processes of physical and chemical weathering. The nature and structure of a given soil depends on the processes and conditions that formed it:

  • Breakdown of parent rock: weathering, decomposition, erosion.
  • Transportation to site of final deposition: gravity, flowing water, ice, wind.
  • Environment of final deposition: flood plain, river terrace, glacial moraine, lacustrine or marine.
  • Subsequent conditions of loading and drainage: little or no surcharge, heavy surcharge due to ice or overlying deposits, change from saline to freshwater, leaching, contamination.

According to ICAR Indian soils are classified as:-

  • Alluvial soils:-Alluvial soils are formed mainly due to silt deposited by Indo Gangetic Brahmaputra rivers. In coastal regions some alluvial deposits are formed due to wave action.
  • Black soils:-The black soils are found mainly on the Deccan lava region covering large parts of Maharashtra, some parts of Gujarat and Madhya Pradesh and small parts of Karnataka, Andhra Pradesh and Tamil Nadu. The soils are formed by disintegration of volcanic basaltic lava. The colour of the soil is generally black due to presence of compounds of aluminium and iron.
  • Red soils:- these soils are light textured with porous and friable structure and there is absence of lime Kankar and free carbonates. They have neutral to acidic reaction and are deficient in nitrogen humus, phosphoric acid and lime.
  • Laterite and Lateritic soils:-These soils are red to reddish yellow in colour and low in N, P, K, lime and magnesia. These soils are formed in-situ under conditions of high rainfall with alternation dry and wet periods. On account of heavy rainfall there is an excessive leaching of soil colloids and silica hence the soils are porous.
  • Forest and Mountain soils:-These soils occur at high elevations as well as at low elevations, where the rainfall is sufficient to support trees. These soils are very shallow, steep, stony, and infertile for the production of field crops. However, they serve a very useful purpose by supplying forest product such as timber and fuel.
  • Arid and Desert soils:-These  soils occur in western Rajasthan, Saurashtra, Kutchchh, western Haryana and southern Punjab . The soil is sandy to gravelly with poor organic matter, low humus contents, infrequent rainfall, low moisture and long drought season. The soils exhibit poorly developed horizons.
  • Saline and Alkaline soils :-These soils occur in areas having a little more rainfall than the areas of desert soils. They show white incrustation of salts of calcium & Magne sium and sodium on the surface. These are poor in drainage and are infertile.
  • Peaty and Marshy soils:-These are soils with large amount of organic matter and considerable amount of soluble salts. The most humid regions have this type of soil. They are black, heavy and highly acidic. They are deficient in potash and phosphate.

Soil erosion is described as the carrying away of soil. It is the removal of the soil by natural elements like water, wind, glacier and wave. Gravity tends to move soil down slope either very slowly as in soil creep or very rapidly as in landslides. The present shape of land has been carved through thousands of years.

Soil conservation is the preventing of soil loss from erosion or reduced fertility caused by over usage,Soil  acidification, salinization or other chemical soil contamination. Slash-and-burn and other unsustainable methods of subsistence farming are practiced in some lesser developed areas.

Mineral Resources of India:Non Metalic

Limestone M.P, Chattisgarh, Andhra Pradesh, Rajasthan
Dolomite Orissa (Birmitrapur in Sundergarh District-largest in India), M.P & Chattisgarh
Phosphate Rajasthan (Udaipur) Uttaranchal (Dehradun), M.P. (Jhabua), U.P. (Lalitpur)
Kaolin Kerala is largest producer.
Mica Andhra Pradesh, Jharkhand (Kodarma-Large) & Rajasthan
Gypsum Rajasthan & J & K.
Steatite Rajasthan. It is also called soapstone/ Potstone.
Magnesite Tamil Nadu
    Pyrite   Bihar is sole producer    
    Graphite   Orissa, Rajasthan    
    Diamond   M.P. (Panna)      
    Beryllium   Rajathan, Jharkhand    
    Salt (NaCl)   Gujarat (60%), Tamil Nadu & Maharashtra
    Marble   Rajasthan      
    Zircon   Beach Sand of Kerala    
    Kyanite   Singhbum distict in Jharkhand-largest. Used as refractory material
    Antimony   Punjab      
    Asbestos   Karnataka & Rajasthan    
    Beryllium   Rajasthan      
    Sulphur   Tamil Nadu      
    Tin   Bihar, Jharkhand  

Types of Settlements : rural and urban

 

Settlement can be defined as any form of human habitation which ranges from a single dwelling to large city. The word settlement has another connotation as well as this is a process of opening up and settling of a previously uninhabited area by the people. In geography this process is also known as occupancy.

Settlements can broadly be divided into two types – rural and urban. Before discussing about meaning and types of rural and urban settlement in India, we should know some basic differences between rural and urban areas in general. (i) The major difference between rural and urban areas is the function. Rural areas have predominantly primary activities, whereas urban areas have domination of secondary and tertiary activities. (ii) Generally the rural areas have low density of population than urban.

Types of Rural Settlements:

Geographers have suggested various schemes of classification. If we group settlements found all over the country, these can broadly be grouped under four categories:

  1. Compact/clustered/nucleated settlement
  2. Semi-compact/Semi-clustered/fragmented settlement
  3. Hemleted settlement
  4. Dispersed settlement

 

Compact Settlements:

  • As the name suggests, these settlements have closely built up area. Therefore in such settlements all the dwellings are concentrated in one central sites and these inhabited area is distinct and separated from the farms and pastures.
  • Maximum settlements of our country comes under this category. They are spread over almost every part of the country.
  • These settlements are distributed over the entire northern Indo-Ganga plain (from Punjab in the north-west to West Bengal in the east), Orissa coast, basins of Mahanadi in Chhattisgarh, coastal areas of Andhra Pradesh, cauvery delta of Tamil Nadu, Maidaus of Karnataka, lower Assam and Tripura, in the valleys of Siwaliks etc.
  • Sometimes people live in compact settlement for security or defence purpose. The greatest example of this type is in Bundelkhand region of Madhya Pradesh and Uttar Pradesh.
  • In Rajasthan also people live in compact settlement because of the scarce availability of cultivable land and water body. Therefore, they want to make maximum use of available natural resources.

Semi compact Settlement:

As the name suggests, the dwellings or houses are not well-knitted. Such settlements are characterized by a small but compact nuclears around which hamlets are dispersed.

  • It covers more area than the compact settlements.
  • These settlements are found both in plains and plateaus depending upon the environmental conditions prevailing in that area.
  • Such settlements are situated along streams in Manipur Mandla and Balaghat districts of Madhya Pradesh, and Rajgarh district of Chhattisgarh. Different tribal groups inhabit such settlements in the Chhota Nagpur region. In Nagaland, such settlements may be in the form of blushing villages.

Hamleted Settlements:

These type of settlements, are fragmented into several small units. The main settlement does not have much influence on the other units. Very often the original site is not easily distinguishable and these hamlets are often spread over the area with intervening fields. This segregation is often influenced by social and ethnic factors. The hamlets are locally named as faliya, para, dhana, dhani, nanglay etc. These settlements are generally found in West Bengal, eastern Uttar Pradesh, Madhya Pradesh and coastal plains. Geographically it covers lower Ganga plain, lower valleys of the Himalayas and central plateau or upland region of the country.

 Dispersed Settlements:

This is also known as isolated settlements. Here the settlement is characterized by units of small size which may consist of a single house to a small group of houses. It varies from two to seven huts. Therefore, in this type, hamlets are scattered over a vast area and does not have any specific pattern. Such type of settlements are found in tribal areas of central part of India covering Chhota Nagpur plateau, Madhya Pradesh, Rajasthan, etc. Such patterns are also common in the hills of north Bengal, Jammu & Kashmir, Tamil Nadu and Kerala.

 

There are three factors that influence the type of settlements in India. These factors are (i) Physical (ii) Ethnic or cultural and (iii) Historical or defence. Let us discuss these factors one by one.

Physical Factors:

These include relief, altitude, soil capability, climate, drainage, ground water level, etc. These factors influence the type and spacing of dwelling or instance, in dry regions of Rajasthan, water is a crucial factor and, therefore, houses are situated along a pond or well which guides the compactness of the settlement.

Ethnic and Cultural Factors:

These include aspects like caste, community, ethnicity and religion. In India it is commonly found that the main land owning caste resides at the centre of the village and the other service providing castes on the periphery. This leads to social segregation and fragmentation of a settlement into several units

Historical or Defence Factors:

In the past, mostly border areas of northwestern plains were conquered or attacked frequently by outsiders. For a long time, apart from attack from outsiders, there had been continuous fight between princely states and kingdom within the country therefore, security concerns favoured the evolution of nucleated settlements.

 

Type of urban settlement:

Like rural settlements, urban settlements are classified on various bases. However, classification based on size and function are most common. Let us discuss them one by one

Classification based on Population Size

According to population size, census of India classifies urban centres into six classes. Classwise urban settlements and their population

Class                              Population

Class I                            1,00,000 and above

Class II                          50,000 – 99,999

Class III                          20,000 – 49,999

Class IV                          10,000 – 19,999

Class V                            5,000 – 9,999

Class VI                          less than 5,000

 

There is another classification of urban settlements. The classification is as follows:

Town                                   Places which have less than one lakh population

City                                     Urban centres having population between one lakh to one million.

Metropolitan Cities          Cities having population in between one million to five million

Mega cities                         Cities having more than 5 million population