The Earth

Earth is known to be the third planet from the Sun and the only astronomical object which has life. Earth is said to be formed over 4.5 billion years ago. Earth's gravity interacts with other objects in space, especially the Sun and the Moon, which is Earth's only natural satellite. Earth orbits around the Sun in 365.256 days. During this time, Earth rotates about its axis 366.256 times, that is, a year has 366.256 days.

Image Credit :-Wikipedia

On total the earth’s surface is divided into four parts-

1.    Lithosphere - Earth's lithosphere is divided into several tectonic plates that move across the surface over millions of years. About 29% of Earth's surface is land consisting of continents and islands.

2.    Hydrosphere - The remaining 71% of the earth is covered with water, mostly by oceans but also lakes, rivers and other fresh water, which all together constitute the hydrosphere. The majority of Earth's Polar Regions are covered in ice, including the Antarctica and the sea ice of the Arctic ice pack.

3.    Atmosphere It is termed as the envelope of air surrounding the earth. All the living organisms like plants need co2 and animals need oxygen from the atmosphere.

4.    Biosphere - A planet's life forms inhabit ecosystems, whose total is sometimes said to form a "biosphere". Earth's biosphere is thought to have begun evolving about 3.5 Million years ago.

 The Earth’s biosphere is divided into biomes, inhabited by similar types of plants and animals.

 Four spheres

 Image Credit :- SlideShare

Formation of the Earth

When it comes to how the Earth was formed, it comes out that several billion years ago our Solar System was nothing but a cloud of cold dust particles swirling through empty space. This cloud of gas and dust was disturbed by the explosion of a nearby supernova star, and the cloud of gas and dust started to collapse as gravity pulled everything together, forming a huge spinning disk which was called the solar nebula.

The center of the disk became the Sun, and the particles in the outer rings turned into large balls of gas and molten-liquid that condensed to take on solid form. About 4.5 billion years ago, they turned into the planets.

Geological division

Geology is an earth science concerned with the solid earth rocks of which it composed the processes of change over time. Geology can we study the solid features of any terrestrial planet or natural satellite such as mars or the moon. Modern geology is overlaps all other earth science including hydrology and the atmospheric sciences .so it is treated as one major aspect of integrated earth science and planetary science.

 

Geology describes the structure of earth on the beneath of surface, and the processes that shaped the structure. It also provides tools to determine the relative and absolute ages of rocks and the histories of the rocks. By combining these tools geologists are able to chronicle the geological history of earth demonstrate the age of earth. Geology provides the primary evidence for the evolutionary history of life and past climate.

 

INTERIOR OF THE EARTH

The radius of the earth is 6,370 km. The rapid increase in temperature is also one of the factors that put a limit to direct observation of the earth’s interior.

 What are the Earth's layers?

image credit :-phys.org

Crust

1)    Earth outer layer is hard and brittle in nature. It is less than 1% of Earth volume. The crust is made up of igneous, metamorphic, and sedimentary rocks

2)    The two different types of crust is continental crust (under the land) and the oceanic crust (under the ocean).

3)    The continental crust has an upper part called granitic rock and it forms Silica and alumina called sial.

4)    The lower part has basaltic rock form in Oceanic floor. Silica, iron and magnesium are called Sima.

The Mantle

      1) The mantle is the mostly-solid bulk of Earth’s interior.

      2) The thin outer layer of the mantle is about 2,900 kilometers                                (1,802 miles) and total volume of the earth is 84%.

     3)  It is composed on dense rocks rich in olivine.

     4) The rocks that make up Earth’s mantle are mostly silicates and a    wide variety of compounds that share the silicon and oxygen structure.           

     5) Common silicates are found in olivine, garnet, and pyroxene. The       other type of rock found in the mantle is magnesium oxide and the other mantle element is iron, aluminum, calcium, sodium, and    potassium.

 

THE CORE

1)    The earth core is the central inner part of our planet and It has an also a (solid) inner core and a (liquid) outer core.

2)     It outer core is very thick about 2,260 kilometers and it is made up of iron and nickel.

3)     But it inner core detected by seismology and it is a solid sphere     about 1,216 km (760 mi) in radius or about 70% of the moon and it is made up of nickel and have a temperature of the sun surface.

4)    The outer boundary of earth surface is 2,890km (1800mi).

5)    The transition of inner and outer core is 5,000 km (3,100 mi)                                                  beneath of the earth surface. 

 

NEIGHBOURING CELESTIAL BODIES

 

1)    Sun

2)    Mercury

3)    Venus

4)    Earth

5)    Mars

6)    Jupiter

7)    Saturn

8)    Uranus

9) Neptune

The New Solar System: What We Know So Far
image credit :-thoughtco

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