Saturday 30 September 2017

REGIONAL PLANNING


Concept of a Region

Classification of Region





Regional Imbalances (RI)

Environmental Issues in Regional Planning (RP) and Planning for Sustainable Development


Planning for sustainable development

Spatial or land use planning plays a key role in shaping and directing
resource use and in the resulting impacts of carbon emissions (among
other externalities

valuable environmental and recreational assets in both town and countryside

Rachel Carson’s Silent Spring (1962) and the Club
of Rome’s Limits to Growth (Meadows et al., 1972), were entwined with
environmental agitation, protest and organisation

sustainable development, a number of key principles
can be identified and outlined
1.Environmentalism
Environmentalism incorporates the idea that the full environmental
costs and benefits should be considered in any decision-making process.
2.Development
The two words ‘sustainable’ and ‘development’ (see also Chapter 19) are
put together to stress a process of change and improvement
3. Equity
4.Participation


At the heart
of sustainable development is the simple idea of ensuring a better quality
of life for everyone, now and for future generations’

Urban planning
sustainable
patterns of development as (DETR, 2000, para. 21):
•• concentrating most additional housing development within urban
areas;
•• making more efficient use of land by maximising the reuse of previously
developed land and the conversion and reuse of existing buildings;
•• assessing the capacity of urban areas to accommodate more housing;
•• adopting a sequential approach to the allocation of land for housing
development;
•• managing the release of housing land;
•• reviewing existing allocations of housing land in plans, and planning
permissions when they come up for renewal.


Delineation Of Functional Regions

This method involves the grouping together of units which display a considerable degree of interdependence.
Two basic approaches: (i) Flow analysis- based on actual observations of what people do.   (ii) Gravitational analysis- based on theoretical observations of what they might do.
The two approaches are explained below in detail.
A. Flow Analysis Method

Builds up flows on the basis of the direction and intensity flows between the dominant center and surrounding satellites.
Flows may be of several types: economic (road, rail, shopping or commuting); social (such as flow of students or patients); political (flow of govt. expenditure); information (newspapers, telephone calls), etc.
Graph theory: measures the relationship (economic, social, etc) between selected group of centers on the basis of flows between the centers. The no. of telephone calls is the usual flow criteria.
The flows are plotted in matrix form, from which primary and secondary flows into and out of each center can be identified.
B. Gravitational Analysis Method

It is concerned with the theoretical forces of attraction between centers rather than the actual flows.
This model assumes that the interaction between two centers is directly proportional to the ‘mass’ of centers and inversely proportional to the ‘distance’ between them.
‘Mass’ is represented by variables like population, employment, income, expenditure and retail turnover.
‘Distance’ is represented in physical terms (miles), time, price and intervening opportunities.
Mathematically
By calculating the potential for the centers, lines illustrating relative attractiveness, spheres of influence of various centers can be plotted on a map.
From such lines, functional regions can be identified.


Questions
1. S e z is a tool for Regional development comment

Sunday 24 September 2017

Perspectives in Human Geography

Perspectives in Human Geography

Areal differentiation; regional synthesis; Dichotomy and dualism; Environmentalism; Quantitative revolution and locational analysis; radical, behavioural, human and welfare approaches; Languages, religions and secularisation; Cultural regions of the world; Human development index.

Basic concepts

Humboldt / Ritter / Darwin / Vidal le blcanche /Carl sauer contibution; Khuns paradigm applied in geography; Ideographic vs Nomothetic )/ Ecumen and non ecumen regions

ECUMENE AND NON-ECUMENE REGIONS 

  1. The permanently inhabited lands are referred to as the  ecumene, while the uninhabited, intermittently or sparsely inhabited lands are referred to as the non-ecumene.
  2. The boundaries of these regions are not distinct but diffuse into each other. 
  3. The major limiting factors are climate, drainage, soil, rough terrain, wild vegetation, altitude and the degree of proneness to disease. Although, the Antarctic ice caps and Greenland represent complete, continuous non-ecumene, most of the non-ecumene is in form of unoccupied, isolated and intermittently occupied regions of varying size and is confined to desert wastes, cold barren, high mountains, swamps and primitive forests of tropics and sub Arctic’s. About 60% of the world’s total area could be referred to as ecumene.

MAJOR ECUMENE REGIONS
Four major clusters or ecumene account for 75% of the world’s total population.
1.  East Asia (China, Japan) is the largest ecumene and a sub-tropical region accounting for 25% of the world’s total populations.
2.  South Asia (India and neighbours) ranks second. It is a tropical region accounting for 25% of the world’s population. This is a region having pre-modern subsistence economy which is predominantly agricultural. The population distribution is determined by agricultural potential of the land food supply. Poverty, malnutrition and low levels of living are common. Birth rates are high; death rates are low but not like the developed countries. Therefore high growth rates prevail. This regions account for only 20% of the world’s resources.
3.  Formers USSR, a mid-latitude region, accounts for 20% of the total population.
4.  North America accounts for 5% of the total population. It is a highly industrialized region with specialized pockets and generally high standards of living throughout.

MAJOR NON-ECUMENE REGIONS  These include, generally, the cold, dry and hot-wet lands. Main features of these regions and future prospects for habitation are discussed below.
Cold, High-Latitude Lands. These include the ice caps of Antarctica,
Greenland, Tundra region of North America and Eurasia and the Arctic and sub-Arctic cold deserts. The main limitations of these regions are long sunless periods, extreme cold temperatures, and almost no vegetation. Only towards the southern margins, some habitation is possible. Future prospects for settlement in this region are bleak due to severity of climate.
Dry Lands  These are characterized by deficiency of water, low precipitation, sparse vegetation, unreliable yields. These lands are intermittently occupied by nomadic groups with dense populations only in a few oases. These regions recently witnessed expansion of population with development of irrigation techniques. This is also possible in future, but at high costs.

Hot-Wet lands  These regions show abundance of climatic energy in form of solar energy and precipitation which cause luxuriant vegetation growth that can support large populations. The wet tropics of the old world are better populated than those of the new world. Nearly 20% of the new world wet tropics can be brought under habitation with suitable land use. Thus, only the wet tropics show prospects of dense population concentrations in decades to come.

Areal differentiation

  1. The study of the spatial distribution of physical and human phenomena as they relate to each other spatially proximate and causally linked phenomena in regions or other spatial units. Along with spatial analysis and landscape approaches, this is often seen as one of the three major approaches to understanding in human geography
  2. term coined by hartshorne
  3. terms- chorology by strabo
  4. Reason for revival- study of human geography, study uneven development, linked to humanism , welfare and sociology
  5. feature- ideographic, regional focus (meaning of ideographic- http://www.encyclopedia.com/social-sciences/dictionaries-thesauruses-pictures-and-press-releases/ideographic-versus-nomothetic-approaches)
  6. Advantages-
  7. criticism-Chorology drew to a close during the 1950s, beginning with a famous attack on Hartshorne’s worldview by Frederick Schaefer in 1953. Essentially, Schaefer claimed that the view that geography is an integrative science concerned with the unique was naive and arrogant because such issues were common to many sciences. By refusing to search for explanatory laws, geography condemned itself to what Schaefer called an immature science. Rather than seeking idiographic regions, geographers should seek nomothetic regularities across regions. This critique helped open the door to the rise of positivism and the quantitative revolution.

Regional Synthesis

  1. Brian J.L. Berry in the Annals of the Association of American Geographers, Vol. 54 (1964) has endeavoured to explain regional synthesis by using a geographic matrix
  2. Synthesis of not only spatial but includes temporal also
  3. link: http://www.geographynotes.com/human-geography/regional-synthesis-of-human-geography-2/1040


Dichotomy and dualism

general vs regional/Detterminism vs possibilism/Physical vs human/ Systematic vs regional/ Historical vs contemporary/formal vs functional

Environmentalism
Ellen Churchill semple




Quantitative revolution
Richard hagget
Chorley

Critic-LD stamp and Minshull

Locational analysis
Locational analysis is an approach to human Geography which focuses on the spatial arrangement of phenomena the main objective of location analysis is generalisation models and theories with productive power

Its philosophy is positivism and quantitative revolution
 1950 and
 geographers as like Bunge and mccarty
Based on empiricism
Hagget in his book locational analysis in human Geography appeal to adopt geometrical tradition in order to explain location order and patterns in human geography

Now write merits and demerits


Radical,Behavioral, Human, welfare

Friday 22 September 2017

1.GEOMORPHOLOGY

Geomorphology

This chapter can be divided as three parts for the purpose of convenience:

Part 1:
Origin and evolution of the earth's crust; 
Fundamentals of geomagnetism; 
Physical conditions of the earth's interior; 
Geosynclines; 
Continental drift; 
Isostasy; 
Plate tectonics; 
Recent views on mountain building; 
Vulcanicity; Earthquakes and Tsunamis; 

Part 2:
Factors controlling landform development; 
endogenetic and exogenetic forces; 
Concepts of geomorphic cycles and Landscape development ; 
Denudation chronology; 
Channel morphology; 
Erosion surfaces; 
Slope development ; 

Part 3:
Applied Geomorphology : Geohydrology, economic geology and environment.




VULCANITY

1.Fumaroles
what- Emission of gases +water vapour from vents
associated with volcanic erutions 
when-Takes place after volcanic eruption
why- due to cooling and contraction of magma after termination of eruption.
Fumaroles can be found along linear fracture or found along crater 
contents- gases- co2 , N,S,O2. Fumaroles dominated by S is called Solfatra 
example- Katmai volcano of Alaska- called a valley of ten thousand smokes

2.Geysers
Intermittent spouting of hot water and steam explosively from their craters.
Example- Old Faithful Geysers. Tellow stone national park USA, Iceland

3.Hotspring
A hot spring is a spring produced by the emergence of geothermally heated groundwater that rises from the Earth's crust. There are geothermal hot springs in many locations all over the crust of the earth. While some of these springs contain water that is a safe temperature for bathing

Water issuing from a hot spring is heated geothermally, that is, with heat produced from the Earth's mantle. In general, the temperature of rocks within the earth increases with depth. The rate of temperature increase with depth is known as the geothermal gradient. If water percolates deeply enough into the crust, it will be heated as it comes into contact with hot rocks. The water from hot springs in non-volcanic areas is heated in this manner.

Q)Difference between Geyser and hotspring

5. Intrusive topography

Batholith- long iregular,dome shaped, deep within earth. ex- found in ranchi plateu as ranchi batholith
laccolith- intrusion between sedimentary layers.magma pushes the sedimentary layer of upper strata to arch up.
loppolith- into shallow concave basin
sills- thick beds between bedding planes of sedimentary layers
sheets- thin layers
dykes-perpendicular

6.Discuss extrusive topography
elevated forms- volcanic cones- cinder, composite, parasitic, acid, basic, lava plug, and lava domes
depressed forms- crater caldera

lava plateau and domes
lava plains

7.Crater
depression formed at the mouth of volcanic vent.
crater lake
craterlets- small sized crater witin extensive crater
adventive crater- in parasite cones

8.Caldera.
enlarged form of crater
two concept- 1.due to subsidence 2. due to violent eruption
nested or grouped caldera- smaller caldera housed in big caldera

9. World distribution of volcanoes
Circumpacific- erebus of antartica to mayon of philipines
Mid continental- etna, visuvious, stromboli
mid Atlantic-iceland ,azores and St.helena
Intra-plate- hawaai to kamchatk

10. Plate tectonics and vulcanity
That is a close relationship between plate boundaries and vulcanity
15%active at constructive player margin
80%at destructive plate boundary
Some intra plate -Hawaii, fault zone of east Africa

Plate boundaries and intensity of volcanic activity
1. Diverge divergent played boundaries associated with quite eruption that is fissure eruption the volcanic lava is tholeitte
2. Effective plate boundary in the circum Pacific associated with violent eruption they consist of aand andesite-dacite and rhyolite
3. Active plume - Hawai




Pelean type- Pelee volcano of Martinique island.Most violent and most explosive
Ejected lavas are most viscous and pasty
Great force and intensity and roaring noise

Visuvius-extremely violent expulsion of magma due to enormous volume of explosive gases

Fissure type-slow upwelling of magma and spread over ground surface. Example- Laki fissure eruption in Iceland

1.PHYSICAL SETTING

1.PHYSICAL SETTING

1.Space relation ship of India with neighboring countries

India- B'desh- 4096km
India-China-3917 km


India- pak- 3310 km, saltro ridge, AGPL.
India-Nepal-1752 km


India-Mynmar- 1458 km 
(Hint- BCPNMB)

lat extent and longi extent
Area-
frontiers. 
Maritime borders.7517km
Islands - https://en.wikipedia.org/wiki/List_of_islands_of_India

Unity and Diversity of India

2.Structure and relief

1. Geological Structure- Archaen, Purana, Dravida, Aryan (ArPuDA)

Archean rock system
1. Archean
2.Darwar

Purana rock system
1.Cuddapah
2.Vindhya

Dravida- 600-300 myaPaleozoic- from cambrian to carboniferous- (pals cam 2car)

beginning of life on earth,coal formations

Aryan (GoCreTerQ)

1.Gondawana- upper carboniferous, gondwana coal formations.
2.Cretaceous- 144-65 mya- creta means chalk, deccan trap
3.Tertiary-  from 65mya- origin of Himalayas
4.Quarternary-  from 2mya
  1. very recent, 
  2. because himalayas has been just now completed in tertiary the north indian plains came into existence by alluvial deposits by rivers, 
  3. pleistocene Ice age effects , 
  4. deposits of peninsular plateau



3.Drainage system and watersheds

Inland drainage basin (endorheic basin): When a river does not reach the sea but disappears into the sand, such a region is called an area of inland drainage. Inland drainage streams are ephemeral streams (short-lived). E.g.:
  1. The Ghaggar river in Haryana, which is supposed to be remnant of the proverbial ancient Saraswati river, gets lost in dry sands near Hanumangarh in Rajasthan.
  2. Western slopes of araavalli
  3. The Luni river in Rajasthan originates near Ajmer and after flowing through Thar desert gets lost in the Rann of Kutch.
  4. The Aksai Chin region in Ladakh too has some inland drainage.


4.Physiographic regions

5.Mechanism of Indian monsoons and rainfall patterns, Tropical cyclones and western disturbances

6.Floods and droughts

7.Climatic regions

8.Natural vegetation

9.Soil types and their distributions.

Topics to be covered
Map - showing distribution Soil in India 
Karewas soil
Montane soil

MARINE POLLUTION

MARINE POLLUTION https://en.wikipedia.org/wiki/Marine_pollution Marine pollution Great pacific garbage patch Deep Sea minin...