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there is presence of salt in coastal rivers. due to which they are SHORT in length.

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Parallels of latitudes and meridians of LONGITUDES create a web like STRUCTURE CALLED grid . Grid helps us in locating places on the globe

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The factory is big & works throughout. It is the most air polluting FACTOR in the environment as it EMITS gases into the atmosphere. The workers are SPECIALIZED in various sectors in the industry. Sugarcane is transported to the factory by means of lorries & tractors. Packaging of sugar is done & distributed to the various market. And this is how in my FIELD VISIT to a sugar factory.

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The RED sea ,the GULF of Aden and Suez canal SEPARATED Asia and AFRICA

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Majhi was a little weak in GEOGRAPHY so her mother called for a county Inspector and the county Inspector FIX the level of the computer teachers to the level that MARGI can do

India's geographical location PROVIDES a lot of strategic benefits to it:

1) India is located above the Indian ocean This Indian ocean route provides a lot of benefit to the country due to the reason that it connects DIFFERENT countries of Europe  and other popular places with the ocean. Which ultimately provide a huge benefit in trade causing country to have success,

2) No other country has a long COAST line except India.

3) Very SUCCESSFUL and most populated countries lies very CLOSE to India which is China, Japan and South East Asia.

4) The oil rich countries of the Persian Gulf are not very far from the India hence India is able to get bulk of oil supplies.

5) India is very well connected with countries through airways and sea routes.

Conservation of resources is IMPORTANT so to PROTECT resources for FUTURE GENERATION

To FIND the time meridian of a country, take the WESTERNMOST longitude and the easternmost longitude of that country, take the mean, and find the nearest multiple of 7.5 degree. As India's longitudinal extent is from 68° 7' 53" E to 97° 24' 47" E. The mean comes out to be 82°46'20".

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These passes are in SAHYADRIS or U can say the western ghats.

Thalghat, PALGHAT, and Bhorghat are the 3 main passes in the sahyadhris (Western Ghats).

Thalghat ---- is located between Mumbai and Pune
Palghat ---- is located between Palakkad and CoimbatoreBhorghat ---- is located between Mumbai and Nasik


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a narrow variable band of very strong predominantly westerly AIR CURRENTS encircling the GLOBE several miles above the earth. There are typically TWO or three jet STREAMS in each of the northern and southern hemispheres.



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❇️ A very large, heavily POPULATED CITY or urban complex.

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TURAN plain  is bounded by the Saryarqa (Kazakh uplands) in the NORTH, the outliers of the Tien Shan, Pamir, and Alay mountains in the east, the Kopet-Dag Range in the SOUTH, and the Caspian SEA in the west. It is traversed by the LOWER courses of the Syr Darya and Amu Darya, both of which drain into the Aral Sea.

Metamorphic foliation can be defined either by preferred mineral orientation (aligned inequant CRYSTALS) or by compositional banding. ... The class of FOLIATED ROCKS includes SLATE, phyllite, schist, and gneiss.

Each of these LONGITUDES is called a degree the o degree longitude PASSING through greewich near londaon is considered as STANDARD and at the time off all other times zones are CALCULATED accordingly

So that the TRACK do not MOVE if it LOOSES

DUE to  this great  longitudinal extent the sun rises or sets almost two hours earlier in the eesternmost part than in the westernmost part.To avoid any confusion with respect to time at different PLACES in India ,the almost centrally located LONGITUDE of 82 1/2°E has been SELECTED as the standard meridian for the whole country.The local time of the standard meridian is used as the standard time for India and is called the Indian Standard Time.

The type of BEHAVIOR EXHIBITED when an animal RECOGNIZES itself in a MIRROR comes within the domain of “theory of mind,” thus is best studied as part of the field of animal cognition. .

Here is ur nation SYMBOLS i THINK this will help U

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India has a variable CLIMATE. This can be proved with the help of the following examples. 1. In summer, the mercury occasionally touches 50°C in some parts of the Rajasthan desert, whereas it MIGHT be around 20°C in Pahalgam in Jammu and Kashmir. 2.In winter, night temperature at Drass in Jammu and Kashmir may be as low as minus 40°C. Thiruvananthapuram on the other hand may have a temperature of 22° C. 3. The annual rainfall in Rajasthan is hardly 10 cm. whereas it is above 400 cm. in Meghalaya. 4. During monsoons, whole country receives rainfall except Tamilnadu. 5. Coastal region does not experience much VARIATION in temperature pattern due to the moderating influence of the sea.


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Raw Materials: ADVERTISEMENTS: ...Power: Regular supply of power is a pre-requisite for the LOCALISATION of industries. ...Labour: ...TRANSPORT: ...Market: ...Water: ...SITE: ...Climate:

The Great LAKES of USA from west to east: ONTARIO ,ERIE, HURON, Michigan and SUPERIOR.

Bhuvan BAM (And MAND KA tola, Jo Na jaane, woh

our BODY is made of cells. cells die and get replaced by new cells . our body is not able to always produce or repair cells as age increases. nature of earth tries to degrade EVERYTHING into its simplest form .so as age increases our immune system functions become LESS ACTIVE . we don't die because of age but because of effects of natur on our body.

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Hey! Mate Here is your answer Here it is: The center-left Institutional Revolutionary PARTY governed the country continuously for 70 years until being defeated by the center-right NATIONAL Action Party in 2000. The PRI regained the presidency under current President Enrique Peña Nieto, whose single six-year term runs through 2018. His focus is on implementing ambitious structural reforms adopted in 2013–2014. With drug-related CRIME rising, perennial left-wing candidate Andrés Manuel López Obrador of the Democratic Revolution Party may be well POSITIONED to compete in the JULY 2018 presidential election. The PRD faces longer odds in winning a majority in Congress, however, and this makes radical policy shifts that would threaten macroeconomic stability less likely.

In the middle course of a river the gradient decreases (it flattens out) and the DISCHARGE increases. This is due to the fact that many more tributaries have joined the main channel, leading to an increased volume of water, as well as the fact that the high level of gravitational potential energy which was found in the upper course of the river has been converted to kinetic energy.
This enables the river to erode laterally as well as vertically, thus widening the river channel. The river also starts to deposit load due to variations in energy in the channel cross-section and longitudinally (caused by differences in geology, gradient, land use and weather conditions). River energy fluctuations along its course leads to a dynamic environment whereby the form of the river can change season by season.

Many landforms are formed in the middle course as a direct consequence of the relative energy balance changing, resulting in both erosion and deposition. The most obvious example of this is a meander.

Meanders

Meanders are the characteristic bends in a river that are found all along the length of a river but particularly in the middle course. They can vary in size, but GENERALLY have deposits of different sized sediment on the inside of the bend called a slip-off slope or point bar, and a concave section on the opposite bank of the river on the outer bend called a river cliff or bluff.

The initial cause of meandering rivers is related to the way in which different types of flow within a river:

LAMINAR flow – horizontal movement in a plane.
turbulent flow – horizontal and vertical eddies in the water sometimes producing mini-whirlpools
helicoidal flow – corkscrew movement of water which is thought to transport eroded material downstream from one meander bend to the next
These, combined with the natural sinuosity (the movement of a river in an S shape ACROSS the landscape) of water leads to different rates of erosion and deposition. It is thought that the frictional drag exerted on the water by the riverbed and banks causes lower layers of water to move more slowly and in a SINUOUS manner. They interfere with upper layers of water and cause them to move in a more exaggerated pattern of sinuosity. Inevitably, once sinuous flow is established it causes the river to collide with the banks and results in erosion.

The increase in discharge typically found in the middle course leads to an increase in the rate of erosion (both vertical and lateral) and the formation of pools in the channel. The rate of formation of pools increases in times of higher discharge and leads to more efficient movement of water. In addition, erosion of the channel causes there to be an increase in the availability of material being transported. This material is often deposited further along the channel in less efficient sections with a lower velocity, to form riffles. Riffles reduce the efficiency of channel flow still further by increasing the wetted perimeter (the length of channel in contact with water) and consequently increases friction. This reduces the velocity of the water and leads to further deposition. Coarse particles in riffles are more angular and generate greater flow resistance than the fine particles in pools so more energy is expended as water flows over them (the water is shallower). This, in turn, encourages further deposition. Pools have a shallower sediment gradient so less energy is expended by the deeper water flowing over them, further increasing channel efficiency.

Pool and riffle sequences cause changes in the efficiency of a river channel which, in turn, causes changes to the way in which the water moves within the channel. The swing of flow caused by riffles forces the line of greatest velocity (the thalweg) to the outside of the channel where it starts to erode the bank by hydraulic action and abrasion.

At the source of the river the land are usually MOUNTAINOUS nd the slope are steep thus high speed of flow. On the other HAND the land are usually plain at the MIDDLE and MOUTH of the river thus rivel flowing SLOW

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However, old craters can be eroded by new impact events. Mercury and the MOON have very old surfaces. One of the youngest large craters on the Moon is Tycho, which was formed about 109 million YEARS AGO. ... Three images of Tycho CRATER and its CENTRAL peak, located at 43 S, 11 W, on the Moon.

The direction of monsoon WIND change because of the change in CLIMATE. During summer the land is warmer than the OCEAN. Thus wind moves from land to sea. While in the summer ocean in warmer than land THEREFORE wind moves from land toward the sea

The Andromeda GALAXY (M31) is the CLOSEST SPIRAL galaxy to us, and though it's gravitationally bound to the Milky WAY.

A wet/dry spell is defined as the CONSECUTIVE DAYS with precipitation amount greater/less than a threshold. The frequency of wet/dry SPELLS, the contributions of wet/dry spells with different lengths to the total number of wet/dry days and total precipitation amount were analyzed for different CLIMATE types.

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As u know india is agricultural country , so farmers depend on monsoon for their further production , so here monsoon plays a very important role . It plays that much role in a farmer's life that a farmer can live or can die becoz of it .

From wheat and rice to vegetables, cotton, and tea, Indian farmers grow a wide range of crops and the country uses more land for crops than any other country in the world (215 million acres). Crops depend on rain and, in India, more than three quarters of the annual rainfall occurs during the four months of the SUMMER monsoon season. But during years when there is less rainfall than usual, crops die in the fields or cannot be planted at all.

Each monsoon season brings fears of flooding, mudslides and other dangerous conditions that can devastate the lives of millions of people. With these kinds of reports, many people forget that the monsoon also brings a positive, life-sustaining bounty. For millions of people AROUND the world, the monsoon is critical to survival, playing a vital role in everything from food production to the economy.


Thanks to the important role that the monsoon plays in the economy, newspapers often refer to the monsoon as "India's true finance minister." More than HALF of India's 1.2 billion people WORK on farms, and agriculture makes up 15 percent of the Indian economy. When the monsoon fails or rainfall totals are lower than expected, farmers harvest fewer crops. 



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Stevenson screen or instrument SHELTER is a shelter or an enclosure to shield meteorological instrument against precipitation, and DIRECT heat radiation from outside SOURCES, while STILL allowing air to circulate freely around them.
A Stevenson screen is a prominent feature on most weather stations. It is used to house weather instruments, for example the six’s thermometer, HYGROMETER, barometer, thermograph and hydrometer.

A river's course can be divided into three STAGES; UPPER, middle, and... probably because the sediment is slowing it down; there's more friction in this smaller channel. The upper course is characterized by large ANGULAR sediment, narrow shallow channels, vertical erosion and low velocity. Common land  forms include waterfalls, gorges, V shaped valleys and interlocking spurs. Meanders are found in the middle course and the channel BECOMES wider and can migrate through lateral erosion. In the lower course sediment becomes smaller, rounder and smoother, channels are wide and deep and velocity is high in the channel. Common land forms are floodplains, levees and oxbow lakes. Estuaries or deltas are found at the MOUTH of some rivers.  

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The TERTIARY sector or service sector is the third of the three economic sectors of the three-sector theory. The others are the secondary sector, and the primary sector. The service sector CONSISTS of the PRODUCTION of services instead of END PRODUCTS.

Most of this air pollution we cause results from the burning of fossil FUELS, such as coal, oil, NATURAL gas, and gasoline to produce electricity and POWER our vehicles. Carbon dioxide (CO2) is a good indicator of how much fossil fuel is burned and how much of other pollutants are EMITTED as a result

Rocks, minerals, LANDFORMS and the processes are just some of the things in the geosphere.The geosphere has four layers: the MANTLE,the CRUST, the INNER CORE and the outer core.