Sachin Tendulkar start his 200th test in Mumbai

Finally the 200th test match of Sachin Tendulkar is start on 14th November 2013. Everyone wants to see Sachin Tendulkar playing live in Mumbai. But the sad news that the only 5000 ticket for common man and unfortunately these all tickets are sold out very early even in the one night. In 200th match of Sachin Tendulkar his mother and family members are in stadium to watch the Sachin Tendulkar playing live cricket on stadium. The all fan of a Sachin Tendulkar except a one more big inning by a Sachin Tendulkar. So wait ...... till 14th November.

So today on 14th Nov. Start the historical match in the morning 9:30am . The wankhde Stadium is full of people's and the crowd of Sachin fans is unbelievable and the wankhde Stadium is full of posters of Sachin memories. The family of sachin is also come in wankhde stadium for support Sachin Tendulkar and India team. In the 1st day today India won the toss and India choose a field first. In the morning west Indies play well but after the lunch time West Indies goes all out so early. In 1st day of 2nd match and 200th match of Sachin Tendulkar West Indies all out on 182 run in a 55.2 overs. In the end of a 1st day India on a 157 on fall of a 2 wickets. So overall today India played a so well the bowlers bowled well today Ashwin take his 100th wicket in his test career. P.Ojha take 5 wicket in a 1st inning of a West Indies. Indias batsman playing well Sikhar dhawan playing in his own way. And Murli Vijay also play well but unfortunately both of the openers are out in the end of the day.  Now playing an Pujara and Sachin Tendulkar on not out. Sachin Tendulkar on 38 and Pujara on 34 runs. So Important is that the Sachin playing now and waiting for 2nd day of the match.........where we see the big inning by a Sachin Tendulkar ..... Hope so.
Today on 15th November Sachin and Pujara played well from the morning and Sachin do a fifty very early. After a 74 runs Sachin caught by an semi. After out of a Sachin , Pujara make a 5th century of his test career.  And than Rohit Sharma played a well. And also Virat kohli made a fifty and Rohit Sharma complete his 2nd century back to back in this series. After the 1st inning of India the score of India is all out on 495. In the 2nd inning of west Indies , the result is same that the batsman got out very early. In the end of 2nd day the score of west Indies is 43 on 3 out. So today we see a last inning of Sachin Tendulkar and when he out the crowd is suddenly turned into a peace and feel a so sad when Sachin Tendulkar out.  All over on the 2nd day India is going to a win very soon so wait and watch.

Practicals of B.Tech Civil Engineering Kuk University

Now , Kurukshetra University announce the Practicals of B.tech 1st , 3rd , 5th , and 7th semester of all branch -

Civil 3rd semester Practicals with dates are -

1. Structural Mechanics - 11-12-2013

2. Fluid Mechanics - 12-12-2013

3. Surveying 1st - 13-12-2013

Sachin Tendulkar - A God Of Cricket

Sachin Tendulkar was born in Bombay , India on April 24, 1973. The real name of Sachin Tendulkar is Sachin Ramesh Tendulkar. The name of his father are Ramesh Tendulkar. Ramesh Tendulkar was a reputed Marathi Novelist. The name of Sachin Tendulkar mother name is Rajni Tendulkar. Rajni Tendulkar worked in the insurance company.

Michel Jackson- An Introduction

Narendra Modi - An Introduction

Narendra Modi was born on 17th september 1950 in Vadnagar , Bombay state ( India ) in a very simple Hindu religion family. The real name of Narendra Modi is Damodardas Narendra Modi. He was the 3rd children of all 6 children born to Damodardas Mulchand Modi and his wife (Heeraben). Narendra Modi in a teen age worked on tea stall with his brother. Modi completed his schooling in a small village Vednagar where Modi is a simple student but teachers describe him a keen debater.
Modi began a work in the staff canteen of the state road transport corporation of Gujarat. Modi had received an RSS training in a Nagpur.During these years in the RSS, Modi come in contact with Vasant Gajendragadkar and Nathalal Jaghda, leaders of the Jan Sangh.These person later found a BJP unit of Gujarat state. Later Modi completed his degree of Master in political science from the university of Gujarat.
Later Modi joined a BJP ( Bhartiya Janta Party ) in 1987. Shankarsingh Vaghela and Keshubhai Patel are the establish an names in that Time in. the Gujarat BJP. Modi rose to prominence after organising Murli Manohar Joshi's Ekta yatra (journey for unity). Narendra Modi personaly is pure vegetarian. In 1995 he create His electinal strategy was central to BJP's victory in state elections. And after that modi became appointed to the General Secretary of Bhartiya Janta Party. After that modi is transferred to New Delhi. where BJP put a lots of responsibility on the Modi related to the Haryana and Himachal Pradesh. Later Modi was promoted to the post of National Secretary of the BJP in 1998.

Narendra Modi as a Chief - Minister of Gujarat - First time Narendra Modi selected as a Chief minister of Gujarat On 7 October 2001. Modi was assigned to the responsibility to the prepare the BJP ( Bhartiya Janta Party ) for elections in December 2002. Narendra Modi as chief minister of Gujarat work well in Gujarat and benefit of this is goes to the BJP in elections of 2002. Now the popularity of Narendra Modi is rising on day by day. And this is seen in the election of the 2002 in Gujarat.

In the elections of 2002 the people of Gujarat make the Narendra Modi as chief minister of Gujarat. In the session of 2002 - 2007 Narendra Modi play an important role in the techanically and institutionally development of Gujarat. In these years Gujarat is become a educationally and techanically popular in India.

In 2012 , Narendra Modi is a first choice of people of Gujarat as chief minister. Narendra Modi make the Gujarat in top 4 state in India. Narendra Modi increase the employment in Gujarat and especially attention on the study of the children. Now the popularity of Narendra Modi is become a rise day by day.

In 2013 , Rajnath (BJP) announced the name of Narendra Modi as a candidate of prime-minister from the party of Bhartiya Janta Party against the Rahul Gandhi which is selected by Indian national Congress.

Surveying - An Introduction

Surveying :- Surveying is the that branch of science which deals with the art of determining the relative positions of points on , above or beneath the surface of the earth by means of an direct measurement or indirect measurement of direction , distance and elevation. It also includes the art of establishing points by predetermined angular and linear measurements. The application of surveying requires skill as well as the knowledge of the  mathematics , physics and to some extent , astronomy.

Levelling :- Levelling is a branch of surveying which deals with the object of which is -
1. to find the elevations of points with respect to a given or assumed datum , and
2. to establish points at a given elevation or at different elevations with respect to a given or assumed datum. The first operation is requires to enable the works to be designed while the second operation is required in the setting out of the all kinds of engineering works. Levelling deals with measurements in a vertical plane.
The knowledge of surveying is advantageous in many phases of engineering. The earliest surveys were made in connection with land surveying. Practically , every engineering project such as water supply and irrigation schemes , railroads and transmission lines , mines , bridge and building etc. requires surveys. Before plans and estimates are prepared , boundaries should be determined and the topography of the site should be ascertained. After the plans are made , the structures must be staked out on the ground. As the work progresses , lines and grades must be given.
In surveying , all measurements of lengths are horizontal , or else are subsequently reduced to horizontal distances. The object of a survey is to prepare plan or map so That it may represent the area on a horizontal plane. A plan or map is the horizontal projection of an area and shows only horizontal distances of the points. Vertical distances between the points are , however , shown by contour lines , hachures or some other methods. Vertical distances are usually represented by means of vertical sections drawn separately.

Geology - Interior of the Earth

Lithosphere :- The solid Earth is known as Lithosphere. An idea about the constituents of this solid body of about 6370 km radius , can be had on the basis of several available indirect observations. Say for example , the average density of the whole earth is 5.5 , whereas that for the rocks making most of the upper crust of the Earth is 3 , which infers that the material beneath the surface is of a much higher density. The temperature indications show that it increases with the depth. The hat lava erupted by the volcanoes also indicates that the deep interior parts of the Earth are very very hot. The pressure as also been observed to be increasing with depth. An analysis of the meteorites falling on earth indicates that they essentially consist of iron and nickel in their core. Since the earth is also a celestial body like That of the meteorites , it can be easily inferred that out of Earth may also contains iron and nickel in it's core.
From all such indirect evidence , it has been generally established that the matter inside the earth is of a higher density , and the deep interior part of the Earth may be in liquid state ; or because of high pressure , it may be in semi-liquid state.
In the modern times , however , our knowledge regarding the interior of the Earth has been vastly increases by the experimental results obtained with the help of seismic waves. During an earthquake ( natural or artificial produced by an explosion ) , three types of waves are generated , known as primary (P) , Secondary (S) , and Long (L) waves. These waves radiated in all directions passing through the earth body , moving faster in the higher density medium. The L - waves which confines themselves to the crystal part , travel faster along the ocean floors. This indicates that the ocean floor composed of a material denser than that of the upper crust of the continent basins. The P and S waves which propagate through the deeper parts of the Earth , are subjected to reflection and refrection with the changes in density. The S-Waves are further characterised by their capablity of passing only through the solids. 
Based upon such experimental work, carried out with the help of such seismic waves , the interior of the Earth can be predicted today , with an enough degree of confidence.
In all , the entire 6370 km thickness of the Earth can be divided into the following three major zones :-
(A) The Crust
(B) The Mantle
(C) The Core

(A) The Crust :- The topmost thin layer of the earth body , having solid thickness of about 30 to 40 km In continents and 5 to 6 km in the oceans , is known as the crust. The base of the crust is marked by a sharp boundary , called Mohorovicic discontinuity or M - discontinuity. The depth of the M - discontinuity is greater beneath the continents than beneath the ocean basins.
Intact , it has been concluded that in the continents , the total depth is about 35 km , out of which the bottom of 5 km depth consists of denser Basalt rock ( density = 3.0 ) , and the top 30 km consists of lighter Granite rock ( Density = 2.7 ) . There is no such granite beneath the oceans , and only 5-6 km thick basalt occurs. These granitic rocks of the continents and the basaltic rocks of the oceans , are generally covered by a top layer of unconsolidated sediments deposited since the formation of these continents or oceans.
The earth crust thus provides us with very useful hard and soft rocks , and are classified as , Igneous , Sedimentary , and Metamorphic rocks , depending upon the certain factors.

(B) The Mantle :- Beneath the M - discontinuity , lie the still denser rocks ( average density 3.3 ) known as the ultra basic rocks , and this portion of the earth is known as the Mantle. It's thickness is about 2860 km and it's density increases with depth.

(C) The Core :- Below the depth of about 2900 km from the surface of the earth , starts the cores. It has been inferred by the study of seismic waves that the earths core is probably 12 or more , but it's exact compositions is not known. Most of the scientists is favour in iron - nickel composition , while some other support the idea of iron - silicate core.
An abrupt increase in the velocity of P - waves at about 2170 km below the core boundary , suggests the presence of an inner core.
This may mean a change from the liquid to the solid state , but this is not well established fact.
The presence of earth's magnetic field may also be explained under this theory of the presence of a liquid core. This may be due to the electric current set up by motion in the liquid core. This is possible because the core is thought to be metallic and , therefore , a good conductor.