Skip to main content

Hypsometric Curve and Hypsometric Integral

Hypsometric curve and Integral

A hypsometric curve is essentially a graph that shows the proportion of land area that exist at various elevations by plotting relative area against relative height. It gives Hypsometric integral which may be defined as the proportion lying below the curve of total square graph. When integral lies between 0.6 to 1, it would be complex curve and indicates youthful stage of dissection. 
When the integral lies between 0.35 to 0.60 it would be S shaped curve indicates maturely dissected landforms and less than 0.35 would be concave curve indicates old stage of river.


To calculate Hypsometric curve at first we have to demarcate a drainage basin and also to determine the major contours.
Suppose a drainage basin having major contours of 400m and 500m.
Then measure the total basinal area and also area below the respective contour and highest relief point and lowest relief point in the basin.
In this basin the highest relief point is 560m and lowest relief point is 360m.
Then 
Relative relief=highest relief-lowest relief
                        =560-360
                        =200
The total basin area and area below the respective contour are calculated with the help of stressing paper.
The scale of the basin map is 1:50000.
Thus 1cm = 500m and 2cm = 1Km.

When we take 2cm x 2cm area then the area will be 1 Sq Km.
Here again 1 Sq Km contains 400 small boxes.
Below 360m contour area = 0 Sq Km
Between 360 and 560m contours the total number of small boxes = 1135.
Now we know that in this stressing graph paper 400 small boxes =1 SqKm.
Hence 1 small box = 1÷400 SqKm
Therefore,
1135 small boxes = 1/400x1135 sqkm.
                                = 2.84 SqKm
Similarly,
Area between 400 & 500m=3.60SqKm.
And
Area between 500 & 560m=0.34 sqkm.
Thus total basin area
= 2.84 + 3.60 + 0.34 = 6.78 sqkm.

Now 
Relative area (a/A) 
= (Total area - Area below Respective contour)/Total area.
Relative Height (h/H) =
Relative Relief - ( Value of any contour - Lowest point of the basin)/Relative Relief


To draw the sequence of values of Relative Height (h/H) is be inversed with respect to Relative Area (a/A) values.


Then plot the Hypsometric curve as below
                 Fig. Showing Hypsometric curve.

Hypsometric Integral

Here we calculate the proportion lying below the curve to the total square graph. To calculate the proportion area we draw a horizontal and a vertical lines.
Here total 100 boxes which represents 100% of the area of the square graph. Below the Hypsometric curve there are 35 boxes and hence
35/100X100 = 35%.
Interpretation of Hypsometric curve 
Hypsometric integral is 35% and hence it is 0.35.
It indicates an old stream as 35% of basin landmass is to be old stage of dissection.

Comments

Popular posts from this blog

Minerals : Classification and Physical properties

Mineral is a naturally occurring, homogeneous inorganic compound having fixed chemical composition and atomic structure formed due to inorganic processes of the Earth. Classification of Rock forming Minerals These are mainly of two types I Silicates Silicates again subdivided into 1. Ferromagnesian minerals i)  Olivine group of minerals ii) Pyroxene group of minerals iii) Amphibole group of minerals iv) Biotite 2. Non Ferromagnesian minerals i)  Feldspar group of minerals ii) Quartz group of minerals iii) Muscovite II Non Silicates Oxides Sulphides Sulphates Carbonates Physical Properties of Minerals Minerals are identified on the basis of following physical properties 1. Colour 2. Streak 3. Lustre 4. Fracture 5. Cleavage 6. Hardness 7. Specific Gravity 8. Form and structure  1. Colour The colour of a mineral depends on the absorption of some and reflectance of other of the coloured rays which constitute the white light. 2. Streak Streak of a miner...

Sources of Energy - Primary and Secondary

Primary Energy The source of energy which does not require any transformation before the use is called primary energy. They are directly used as they available in nature. E.g. sun, river water, mountain lakes, wind, coal, crude oil, natural gas, wood, uranium, geothermal heat etc.  Secondary Energy The source which requires transformation before the use is called secondary energy. E.g. Petrol, diesel, kerosene, charcoal, electricity etc. The petrol, diesel and kerosene are derived from the petroleum (crude oil), charcoal derived from the wood, electricity derived from the water, wind, coal and also from the sun.

Renewable and Non Renewable Energy

There are mainly two types of energy 1. Renewable Energy 2. Non Renewable Energy 1. Renewable Energy It includes solar, wind, hydropower, geothermal, biomass etc. These are also called clean energy. The renewable energy resources are displacing fossil fuels in the power sector also offering the benefits of low carbon emissions and other types of pollution. The renewable energy comes from natural sources that can be replenished. For example sun and wind keep shining and blowing, even if their availability depends on time and weather.  Renewable energy is even thought of the new technology, harnessing nature's power has long been used for heating, transportation, lighting and more. Wind energy is made when wind moves the blade on a wind tarbine. This movement creates wind energy which which is converted into electricity. The sun is providing light and warmth which can be converted into solar energy.  Types of Renewable energy A) Solar energy Sun is a powerful source ...