Skip to main content

Methods of Regionalisation

The methods of regionalization could be along the following lines.
1.     It could consider homogeneity, i.e., one set or a combination of physical & socio-economic attributes.
2.     It could be on the basis of nodality or polarization, i.e., forming a region around a core urban place.
3.     It could be on the basis of a programming or policy-oriented region, i.e., one based on administrative coherence or resemblance between the area being studied & the political institutions for effectuating policy decisions. (J.R. Meyer)
Regionalisation of Formal Region:
In identifying formal regions, we consider homogeneity or uniformity on the basis of certain criteria. For example, the economic criterion considers the per capita income level of a formal region.
If more than one feature is taken into consideration, the following methods are employed:
1.The Fixed Index Method:
Under the fixed index method, a common characteristics feature is chosen, i.e., per capita income, percentage of literacy, etc.
2.The Variable Index Method:
Under the variable index method, variable weights are attached to highlight different levels pf activities in different regions.
3.The Cluster Method:
The cluster method is employed to identify homogenous regions. The clusters are mapped with the help of mapping techniques whereas inter-related variables are mapped with the help of superimposed techniques. The composite ranking of areas is used when the variables are too many & have weak relations.
4.Weighted Index Number Method:
Under this method, divided the area into 9 parts on the basis of unemployment & per capita income. First, the area is divided into two parts on the basis of similarity or differences the per capita income & unemployment.
weighted index number method
Fig: Weighted Index Number Method

Regionalisation of Formal Region:
The methods used are 
1.Flow Analysis Method:
Flow analysis considers intra-regional commuting flows, commodity flows, migration flows, trade area, newspaper circulation area & so on.
2.Gravitational Analysis Method:
Gravitational analysis studies the theoretical forces of attraction between two centres. The gravitational force between centres ‘i’ and ‘j’ can be expressed as – 
Gij = K []
Where, Gij = Gravitational force between centres i and j.
Mand M= the masses of the centres i and j.
dij = distance between i and j.

K = constant.

Comments

Popular posts from this blog

Behaviouralism in geography

Behaviouralism Behaviouralism is an approach in human geography that came to prominence in the human geography of the 1960s and 1970s. It goes out of the idea that people are the determining factor in the explanation of space. Behaviouralism tries to give an explanation of the spatiallity of human activities. And thereby they use a complex universally applicable model.  Definition of Behaviouralism: The particular aspect with which geographical content is analyzed using mathematical statistics & human sensitivity, is called behavioralism. Concept of Behaviouralism: The Behaviouralism revolution is a theoretical concept. Its theories are not based on assumptions, but are actually explored through ascending methods based on the experience of human behavior. An analysis of the significance of geographical issues in behavioral perspectives within a system, so therefore is no definite boundary to behavioral geography. The main purpose of behaviouralism geography is to invest

Deep-Ocean Basin

Abyssal Plain:  Abyssal plains is an underwater plain on the deep ocean floor, usually found at depths between 3000 metres & 6000 metres. Characteristics: a)       Abyssal plain is the most extensive relief zone of the ocean floor. b)      The average slope gradient is almost 0.5ᵒ. c)       It covers nearly 40% of the ocean floor. d)      It is flat & rolling submarine plain. Abyssal Hill:  Abyssal hills a small hill that rises from the floor of an abyssal plain. Characteristics: a)       Covering more than 30% of the ocean floor. b)      Height of this hill is less than 100m. Seamounts: Seamounts is an volcanic projections that developed above the abyssal plains that do not rise above the surface of the sea. Characteristics: a)       Seamounts are circular or elliptical. b)      Height is of less than 1 km. c)       Relatively steel slops of 20ᵒ-25ᵒ. d)      Seamounts may be found alone or in groups of from 10 to 100. Guyots:  Guyots are

Positive and Negative Impact of Tide

Tide has many effects on human life. The impact of tide discuss below- Positive Impact of Tide: Shipping:  Tides are helpful in making rivers navigable for large vessels. During the high tide, the amount of river water & height of river water increases. At that time, large vessels/ships can easily come to rive port. Again, during the low tide, ships can be returned from port to sea.  For example - London & Kolkata have become important ports because of the tidal waves in the Thames & the Hooghly rivers respectively. Pollution-free Environment:  When tidal water flows, rivers are free of garbage. As a result, the environment is not pollutant near the river areas. Obstruction of Sediments deposited & Delta Formation:  As a result of the tide, sediments not to deposited & prevents delta formation.  For example-  In the Sundarbans, small creeks are capable of navigating during tides.  Regular Water flow:  During the tide, sea salt water enters the river