Definition of Analysis
In linguistics, analysis is the study of language to examine in depth the structure of language. While laboratory activities, said analysis or analysis can also mean the activities carried out in the laboratory to examine the substances in the sample. However, in its development, the use of word analysis or academic analysis is in the spotlight, especially among linguists. The use must be analysis. This is because word analysis is a loan word from a foreign language (English) is analysis.
From the suffix -isys when absorbed into Indonesian it becomes -isis. So it must be for us to straighten out the use of any language in order to create good practice and correct language for the sake of the nation appearing a logical, better order.
Definition of Analysis According to Experts
1. ACCORDING TO WIRADI
Analysis is an activity that contains the activities of sorting, breaking down, distinguishing things to be classified and grouped according to certain criteria and then looking for their significance and their relevance.
2. ACCORDING TO KOMARUDDIN
Analysis is an activity of thinking to decompose a whole into components so that they can recognize the signs of components, relationships with each other and their respective functions in an integrated whole.
3. ACCORDING TO DWI PRASTOWO DARMINTO
The analysis is interpreted as a breakdown of a subject on the various parts and a review of the part itself, as well as the relationships between the parts to obtain an appropriate understanding and understanding of the overall meaning.
4. DICTIONARY ACCOUNTING
The analysis is to evaluate the conditions of the verses relating to accounting and possible reasons for differences that arise.
5. ANNE GREGORY
Analysis is the first step of the planning process.
6. SYAHRUL
Analysis means evaluating the conditions of the items or verses relating to accounting and possible reasons for differences that arise.
7. EFFREY LIKER
Analysis is the time to gather evidence, to find the source of a problem, namely its roots.
8. HANIF AL FATTA
Analysis is the initial stage in the development of a fundamental stage which determines the quality of the information system developed.
9. HUSEIN UMAR
Analysis is a work process of a series of stages of work before research is documented through the stages of writing a report.
10. MINTO RAHAYU
Analysis is a way of dividing a subject into components; it means letting go, letting go of, describing something which is bound together.
11. ROBERT J. SCHREITER, 1991
Analysis is the "reading" of the text, which locates the signs that place the signs in dynamic interactions, and the messages conveyed.
12. RIFKA JULIANTY
Analysis is an elaboration on the subject of the part and the study itself, as well as the relationship between the parts to get the right understanding and understanding of the overall meaning.
13. MOHAMMAD AFDI NIZAR
Analysis is an evaluation of the conditions of the verses relating to accounting and the reasons for allowing differences to emerge.
Implementation Stage
For the application of this media must go through 4 stages, namely: (1) planning (plan): planning of action (Plan of Action) and research planning (Plan of Research), (2) actions (act): implementing actions (implementing actions) and observing actions (monitor action), (3) investigation (research): get data (produce data) and data analysis (analyze data), and (4) reflection (reflect). Of the four stages form a cycle.
Climate and Weather of Earth's Atmosphere
Climate and Weather of Earth's Atmosphere
Earth's atmosphere has no definite limits, slowly thinning and blurring into outer space. Three quarters of the mass of the atmosphere is at an altitude of 11 kilometers from the surface of the Earth. This lowest layer is called the troposphere. Energy from the Sun heats this layer, and the surface below it, which causes air to expand.
The air in this layer then moves up and is replaced by cold air with higher humidity. As a result, atmospheric circulation occurs which triggers the formation of weather and climate through the redistribution of heat energy.
The main effects of atmospheric circulation are the occurrence of trade winds in the equatorial region which are at latitude 30 ° and west winds in the mid-latitude regions between 30 ° and 60 °. Ocean currents are also an important factor in determining climate, especially thermohaline circulation that spreads heat energy from the ocean at the equator to the polar regions.
Water vapor generated through evaporation on the surface of the Earth is transported by circulating patterns in the atmosphere. When the atmosphere lifts warm and humid air, water vapor will condense and settle to the surface of the Earth through the process of precipitation. Water that is lowered to the surface of the Earth in the form of rain is then transported to lower heights by rivers and usually returns to the sea or empties into lakes.
This event is called the water cycle, which is an important mechanism to support the survival of life on land and the main factor that causes erosion on the surface of the Earth in the geological period. The pattern of precipitation is very diverse, ranging from a few meters of water per year to less than one millimeter. Atmospheric circulation, topology, and temperature differences also determine the average rainfall that falls in each region.
The amount of solar energy reaching the Earth will decrease with increasing latitude. At higher latitudes, sunlight reaches the Earth's surface at a lower angle and must pass through thicker atmospheric columns. As a result, the average temperature at sea level decreases around 0.4 ° C per degree of latitude from the equator. The earth can be divided into specific latitude zones based on estimates of climate similarity.
This division ranges from the equator to the polar regions, namely tropical (or equatorial) climate zones, subtropical, temperate, and polar. Climate can also be classified according to temperature and rainfall, which is characterized by climate regions with uniform air masses.
The most commonly used is the Köppen climate classification system (coined by Wladimir Köppen). This classification divides the Earth into five climate zones (humid, dry tropics, humid middle latitudes, continental and cold poles), which are then subdivided into more specific sub-types.
Analysis in an effort to understand and explain the process for the problem and various things that are in it. While science (science) is the right understanding and definition of activities carried out analysis to describe substances into its constituent compounds. In chemistry, analysis is used to determine the composition of an ingredient or substance. Examples of the best known areas of the field of food technology from activity analysis.
Earth's atmosphere has no definite limits, slowly thinning and blurring into outer space. Three quarters of the mass of the atmosphere is at an altitude of 11 kilometers from the surface of the Earth. This lowest layer is called the troposphere. Energy from the Sun heats this layer, and the surface below it, which causes air to expand.
The air in this layer then moves up and is replaced by cold air with higher humidity. As a result, atmospheric circulation occurs which triggers the formation of weather and climate through the redistribution of heat energy.
The main effects of atmospheric circulation are the occurrence of trade winds in the equatorial region which are at latitude 30 ° and west winds in the mid-latitude regions between 30 ° and 60 °. Ocean currents are also an important factor in determining climate, especially thermohaline circulation that spreads heat energy from the ocean at the equator to the polar regions.
Water vapor generated through evaporation on the surface of the Earth is transported by circulating patterns in the atmosphere. When the atmosphere lifts warm and humid air, water vapor will condense and settle to the surface of the Earth through the process of precipitation. Water that is lowered to the surface of the Earth in the form of rain is then transported to lower heights by rivers and usually returns to the sea or empties into lakes.
This event is called the water cycle, which is an important mechanism to support the survival of life on land and the main factor that causes erosion on the surface of the Earth in the geological period. The pattern of precipitation is very diverse, ranging from a few meters of water per year to less than one millimeter. Atmospheric circulation, topology, and temperature differences also determine the average rainfall that falls in each region.
The amount of solar energy reaching the Earth will decrease with increasing latitude. At higher latitudes, sunlight reaches the Earth's surface at a lower angle and must pass through thicker atmospheric columns. As a result, the average temperature at sea level decreases around 0.4 ° C per degree of latitude from the equator. The earth can be divided into specific latitude zones based on estimates of climate similarity.
This division ranges from the equator to the polar regions, namely tropical (or equatorial) climate zones, subtropical, temperate, and polar. Climate can also be classified according to temperature and rainfall, which is characterized by climate regions with uniform air masses.
The most commonly used is the Köppen climate classification system (coined by Wladimir Köppen). This classification divides the Earth into five climate zones (humid, dry tropics, humid middle latitudes, continental and cold poles), which are then subdivided into more specific sub-types.
Analysis in an effort to understand and explain the process for the problem and various things that are in it. While science (science) is the right understanding and definition of activities carried out analysis to describe substances into its constituent compounds. In chemistry, analysis is used to determine the composition of an ingredient or substance. Examples of the best known areas of the field of food technology from activity analysis.
Layers and Changes in Earth's Atmospheric Surface
Layers and Changes in Earth's Atmospheric Surface
The atmosphere is a layer of air that covers the earth as a whole with a thickness of more than 650 km. The movement of air in the atmosphere occurs mainly due to the influence of sunlight heating and earth's rotation. This earth's rotation will result in the movement of air mass, so that there will be differences in air pressure in various places in the atmosphere that can cause wind currents.
Atmospheric Evolution
According to geologists, in the beginning the earth's atmosphere contained (carbon dioxide) high levels, so the surface temperature of the earth was also high. At that time oxygen () had not yet been formed so there was no ozone layer in the stratosphere, because of that ultraviolet light from the sun reaching the earth's surface with a very strong radiation intensity. This condition is not possible for life, except there may be life in deep waters so as to avoid ultra violet rays.
About 3.5 billion years ago the evolution of chlorophyll living creatures began to enable the process of photositensis. Because photositensis requires the levels in the atmosphere to decrease and vice versa levels increase. Through this process the ozone layer () is formed.
Atmospheric Layers
Based on the vertical temperature profile, the layers of the atmosphere can be divided into
Troposphere (0 - 10 Km) Is the lowest atmosphere and close to the Earth. In this layer, there are clouds, wind, rain, lightning, and others.
Stratosphere (10 - 30 Km) In this layer, an increase in temperature due to increased altitude. Ozone (O3) is found in this layer with a height of 25 Km from the surface of the Earth.
Mesosphere (30-50 Km) This layer has electrically charged ions or air (Layer D) which functions to reflect radio waves. Because of the electric charge, we can communicate with other people abroad.
Thermosphere (50 - 400Km) This layer serves to protect the earth from meteors by burning it. This is because the atmospheric layer has electrically charged or ionized solar radiation
Exosphere> 400 Km Is the highest layer of the atmosphere. In this layer, the content of atmospheric gases is very low. The boundary between the ekosfr (which is basically also the boundary of the atmosphere) with outer space is not clear. Areas that are included in the ecosphere are areas that can still be affected by the earth's gravity. Imaginary lines that limit the ecosphere with outer space are called magnetopause.
Atmospheric Function
The existence of the atmosphere that covers the entire surface of the earth has a very important meaning for the survival of various organisms on earth. Atmospheric functions include:
Reducing solar radiation that reaches the earth's surface during the day and loss of excessive heat at night.
Distributing water to various regions of the earth's surface
Provides oxygen and carbon dioxide.
As a retaining meteor that will fall to earth.
The role of the atmosphere in reducing solar radiation is very important. If there is no atmospheric layer, the surface temperature of the earth if 100% of the sun's radiation is received by the surface of the earth will be very high and it is feared that no organism can understand life, including humans.
In distributing water between regions on the surface of the earth, the role of the atmosphere is seen in the hydrological cycle. Without an atmosphere capable of storing water vapor, then all the water on the surface of the earth will only collect at the lowest place.
The rivers will dry up, all the ground water will seep into the sea, so that the water will only collect in the ocean and sea. The distribution of water by the atmosphere provides opportunities for all living things to grow and develop throughout the earth's surface. In addition, the atmosphere can provide oxygen for living things. Plant's need for CO2 can also be obtained from the atmosphere.
The atmosphere is a layer of air that covers the earth as a whole with a thickness of more than 650 km. The movement of air in the atmosphere occurs mainly due to the influence of sunlight heating and earth's rotation. This earth's rotation will result in the movement of air mass, so that there will be differences in air pressure in various places in the atmosphere that can cause wind currents.
Atmospheric Evolution
According to geologists, in the beginning the earth's atmosphere contained (carbon dioxide) high levels, so the surface temperature of the earth was also high. At that time oxygen () had not yet been formed so there was no ozone layer in the stratosphere, because of that ultraviolet light from the sun reaching the earth's surface with a very strong radiation intensity. This condition is not possible for life, except there may be life in deep waters so as to avoid ultra violet rays.
About 3.5 billion years ago the evolution of chlorophyll living creatures began to enable the process of photositensis. Because photositensis requires the levels in the atmosphere to decrease and vice versa levels increase. Through this process the ozone layer () is formed.
Atmospheric Layers
Based on the vertical temperature profile, the layers of the atmosphere can be divided into
Troposphere (0 - 10 Km) Is the lowest atmosphere and close to the Earth. In this layer, there are clouds, wind, rain, lightning, and others.
Stratosphere (10 - 30 Km) In this layer, an increase in temperature due to increased altitude. Ozone (O3) is found in this layer with a height of 25 Km from the surface of the Earth.
Mesosphere (30-50 Km) This layer has electrically charged ions or air (Layer D) which functions to reflect radio waves. Because of the electric charge, we can communicate with other people abroad.
Thermosphere (50 - 400Km) This layer serves to protect the earth from meteors by burning it. This is because the atmospheric layer has electrically charged or ionized solar radiation
Exosphere> 400 Km Is the highest layer of the atmosphere. In this layer, the content of atmospheric gases is very low. The boundary between the ekosfr (which is basically also the boundary of the atmosphere) with outer space is not clear. Areas that are included in the ecosphere are areas that can still be affected by the earth's gravity. Imaginary lines that limit the ecosphere with outer space are called magnetopause.
Atmospheric Function
The existence of the atmosphere that covers the entire surface of the earth has a very important meaning for the survival of various organisms on earth. Atmospheric functions include:
Reducing solar radiation that reaches the earth's surface during the day and loss of excessive heat at night.
Distributing water to various regions of the earth's surface
Provides oxygen and carbon dioxide.
As a retaining meteor that will fall to earth.
The role of the atmosphere in reducing solar radiation is very important. If there is no atmospheric layer, the surface temperature of the earth if 100% of the sun's radiation is received by the surface of the earth will be very high and it is feared that no organism can understand life, including humans.
In distributing water between regions on the surface of the earth, the role of the atmosphere is seen in the hydrological cycle. Without an atmosphere capable of storing water vapor, then all the water on the surface of the earth will only collect at the lowest place.
The rivers will dry up, all the ground water will seep into the sea, so that the water will only collect in the ocean and sea. The distribution of water by the atmosphere provides opportunities for all living things to grow and develop throughout the earth's surface. In addition, the atmosphere can provide oxygen for living things. Plant's need for CO2 can also be obtained from the atmosphere.
Earth's Structure and Atmosphere
Earth's structure and Atmosphere
Arrangement of Layers of Planet Earth
In the process of formation or occurrence the earth has the following arrangement.
Atmosphere
The earth is surrounded by a layer of air called the atmosphere. With a thickness of ± 2,000 km. This air layer mainly contains nitrogen, oxygen and gas. The atmosphere keeps the earth from getting too hot in the sun and not too cold. This layer of air also protects the earth against ultra violet rays from the sun. This ray is dangerous for life. Under the atmosphere there is a cloud containing clouds of water that comes from ocean water vapor and land water vapor down to earth as rain.
Hydrosphere / Ocean / Water
The ocean is a large basin filled with water with an average depth of 3,500 m. The area of the ocean reaches two thirds of the earth's surface.
Mesosphere (Earth's Coat)
Under the earth's crust there is a layer of the earth's mantle. This mantle is a layer of rock about 2,900 km thick. the temperature at the bottom of the mantle reaches 3,700 degrees Celsius, but the rock remains solid because it is under high pressure.
Barisfer (Core of the Earth)
The earth's core consists of two layers, namely the inner core and the outer core.
The outer core is ± 2,000 km thick consisting of molten iron, the temperature reaches 2,200 degrees Celsius.
The inner core in the center of the earth is a ball with a diameter of 2,740 km. this ball consists of solid iron and nickel. The center temperature is ± 4,500 degrees Celsius.
Earth's structure
Earth's atmosphere
The atmosphere is the layer of gas that surrounds a planet, including the earth, from the surface of the planet to deep space. On Earth, the atmosphere is from an altitude of 0 km above the ground, up to about 560 km above the Earth's surface. The atmosphere is composed of several layers, which are named after the phenomena that occur in that layer.
The transition between layers is gradual. The study of the atmosphere was first carried out to solve the problem of the weather, the phenomenon of refraction of the sun when it rises and sets, and the star's twinkling. With sensitive equipment installed in space rides, we can get a better understanding of the atmosphere and the phenomena that occur in it.
The Earth's atmosphere consists of nitrogen (78.17%) and oxygen (20.97%), with a small amount of argon (0.9%), carbon dioxide (variable, but around 0.0357%), water vapor, and other gases. The atmosphere protects life on earth by absorbing ultraviolet radiation from the Sun and reducing extreme temperatures between day and night. 75% of the atmosphere is within 11 km of the planet's surface.
The atmosphere does not have a sudden limit, but rather thin out gradually by increasing the height, there is no definite boundary between the atmosphere and outer space.
The atmosphere comes from the Greek "Atmos" which means water vapor or gas and "Sphaira" which means blanket. So the atmosphere can be interpreted as a layer of gas that surrounds a planet, including the earth, from the surface of the planet to deep space with a thickness of approximately 1,000 km from the earth's surface and has a mass of 59 x 1014 tons. On earth, the atmosphere is from an altitude of 0 km above the ground, up to about 560 km above the earth's surface. Atmosper follows the earth's rotation (rotation) and evolves around the sun.
Arrangement of Layers of Planet Earth
In the process of formation or occurrence the earth has the following arrangement.
Atmosphere
The earth is surrounded by a layer of air called the atmosphere. With a thickness of ± 2,000 km. This air layer mainly contains nitrogen, oxygen and gas. The atmosphere keeps the earth from getting too hot in the sun and not too cold. This layer of air also protects the earth against ultra violet rays from the sun. This ray is dangerous for life. Under the atmosphere there is a cloud containing clouds of water that comes from ocean water vapor and land water vapor down to earth as rain.
Hydrosphere / Ocean / Water
The ocean is a large basin filled with water with an average depth of 3,500 m. The area of the ocean reaches two thirds of the earth's surface.
Mesosphere (Earth's Coat)
Under the earth's crust there is a layer of the earth's mantle. This mantle is a layer of rock about 2,900 km thick. the temperature at the bottom of the mantle reaches 3,700 degrees Celsius, but the rock remains solid because it is under high pressure.
Barisfer (Core of the Earth)
The earth's core consists of two layers, namely the inner core and the outer core.
The outer core is ± 2,000 km thick consisting of molten iron, the temperature reaches 2,200 degrees Celsius.
The inner core in the center of the earth is a ball with a diameter of 2,740 km. this ball consists of solid iron and nickel. The center temperature is ± 4,500 degrees Celsius.
Earth's structure
Earth's atmosphere
The atmosphere is the layer of gas that surrounds a planet, including the earth, from the surface of the planet to deep space. On Earth, the atmosphere is from an altitude of 0 km above the ground, up to about 560 km above the Earth's surface. The atmosphere is composed of several layers, which are named after the phenomena that occur in that layer.
The transition between layers is gradual. The study of the atmosphere was first carried out to solve the problem of the weather, the phenomenon of refraction of the sun when it rises and sets, and the star's twinkling. With sensitive equipment installed in space rides, we can get a better understanding of the atmosphere and the phenomena that occur in it.
The Earth's atmosphere consists of nitrogen (78.17%) and oxygen (20.97%), with a small amount of argon (0.9%), carbon dioxide (variable, but around 0.0357%), water vapor, and other gases. The atmosphere protects life on earth by absorbing ultraviolet radiation from the Sun and reducing extreme temperatures between day and night. 75% of the atmosphere is within 11 km of the planet's surface.
The atmosphere does not have a sudden limit, but rather thin out gradually by increasing the height, there is no definite boundary between the atmosphere and outer space.
The atmosphere comes from the Greek "Atmos" which means water vapor or gas and "Sphaira" which means blanket. So the atmosphere can be interpreted as a layer of gas that surrounds a planet, including the earth, from the surface of the planet to deep space with a thickness of approximately 1,000 km from the earth's surface and has a mass of 59 x 1014 tons. On earth, the atmosphere is from an altitude of 0 km above the ground, up to about 560 km above the earth's surface. Atmosper follows the earth's rotation (rotation) and evolves around the sun.
Arrangement, Structure Layer of Planet Earth
Arrangement, Structure Layer of Planet Earth
Layers of Planet Earth - Composition, Structure, Atmosphere, Evolution, Function, Climate and Weather: Earth is home to millions of living things, including humans. Earth's mineral resources and other biosphere products contribute to the provision of resources to support the global human population.
Earth
Earth is the third planet of the Sun which is the most populous planet and the fifth largest of the eight planets in the Solar System. Earth is also the largest of the four earth planets of the Solar System. Earth is sometimes called the world or the Blue Planet.
The earth formed about 4.54 billion years ago, and life appeared on its surface in the first billion years. The Earth's biosphere then slowly changes the atmosphere and other basic physical conditions, which allows the proliferation of organisms and the formation of an ʻozone layer, which together with the Earth's magnetic field blocks harmful solar radiation and allows microscopic living things to breed safely on land. Physical properties, geological history, and Earth's orbit make it possible for life to survive.
The Earth's lithosphere is divided into a number of rigid segments, or tectonic plates, which have moved across the Earth's surface for millions of years. More than 70% of the Earth's surface is covered by water, and the rest consists of continents and islands that have many lakes and other water sources that contribute to the formation of hydrosphere.
The Earth's poles are mostly covered with ice; solid ice in Antarctic ice sheets and sea ice in polar ice packs. The interior of the Earth is still active, with the inner core consisting of solid iron, while the outer core is a liquid that creates a magnetic field, and a relatively thick thick layer in the mantle.
The Earth interacts gravity with other objects in space, especially the Sun and Moon. When circling the Sun in one orbit, the Earth rotates on its axis 366.26 times, which creates 365.26 solar days or one cider year.
The rotation of the Earth on its axis is tilted 23.4 ° from the plane of the orbit, which causes a difference in seasons on the Earth's surface with a period of one tropical year (365.24 solar days). The moon is the only natural satellite of the Earth, which began to orbit the Earth about 4.53 billion years ago. The gravitational interaction between the Moon and the Earth stimulates ocean tides, stabilizes the tilt of the axis, and gradually slows the Earth's rotation.
Earth is home to millions of living things, including humans. Earth's mineral resources and other biosphere products contribute to the provision of resources to support the global human population. The Earth region inhabited by humans is grouped into 200 sovereign states, which interact with one another through diplomacy, tourism, trade, and military action.
Lithosphere (Earth's Crust)
Is the topmost rock layer on the surface of the earth called the earth's crust. Under the continent, the thickness of the earth's crust reaches 70 km, under the ocean is only about 6 km. the temperature in the earth's crust reaches about 1,050 degrees Celsius.
Layers of Planet Earth - Composition, Structure, Atmosphere, Evolution, Function, Climate and Weather: Earth is home to millions of living things, including humans. Earth's mineral resources and other biosphere products contribute to the provision of resources to support the global human population.
Earth
Earth is the third planet of the Sun which is the most populous planet and the fifth largest of the eight planets in the Solar System. Earth is also the largest of the four earth planets of the Solar System. Earth is sometimes called the world or the Blue Planet.
The earth formed about 4.54 billion years ago, and life appeared on its surface in the first billion years. The Earth's biosphere then slowly changes the atmosphere and other basic physical conditions, which allows the proliferation of organisms and the formation of an ʻozone layer, which together with the Earth's magnetic field blocks harmful solar radiation and allows microscopic living things to breed safely on land. Physical properties, geological history, and Earth's orbit make it possible for life to survive.
The Earth's lithosphere is divided into a number of rigid segments, or tectonic plates, which have moved across the Earth's surface for millions of years. More than 70% of the Earth's surface is covered by water, and the rest consists of continents and islands that have many lakes and other water sources that contribute to the formation of hydrosphere.
The Earth's poles are mostly covered with ice; solid ice in Antarctic ice sheets and sea ice in polar ice packs. The interior of the Earth is still active, with the inner core consisting of solid iron, while the outer core is a liquid that creates a magnetic field, and a relatively thick thick layer in the mantle.
The Earth interacts gravity with other objects in space, especially the Sun and Moon. When circling the Sun in one orbit, the Earth rotates on its axis 366.26 times, which creates 365.26 solar days or one cider year.
The rotation of the Earth on its axis is tilted 23.4 ° from the plane of the orbit, which causes a difference in seasons on the Earth's surface with a period of one tropical year (365.24 solar days). The moon is the only natural satellite of the Earth, which began to orbit the Earth about 4.53 billion years ago. The gravitational interaction between the Moon and the Earth stimulates ocean tides, stabilizes the tilt of the axis, and gradually slows the Earth's rotation.
Earth is home to millions of living things, including humans. Earth's mineral resources and other biosphere products contribute to the provision of resources to support the global human population. The Earth region inhabited by humans is grouped into 200 sovereign states, which interact with one another through diplomacy, tourism, trade, and military action.
Lithosphere (Earth's Crust)
Is the topmost rock layer on the surface of the earth called the earth's crust. Under the continent, the thickness of the earth's crust reaches 70 km, under the ocean is only about 6 km. the temperature in the earth's crust reaches about 1,050 degrees Celsius.
Definition of the Litosphere and its Explanatory Section
Definition of the Litosphere and its Explanatory Section
Lithosphere is the outer shell of a rocky planet. The lithosphere is derived from the Greek word, lithos which means rocky and sphere which means solid. This lithosphere is derived from the word lithos which means rock and sphere means layer. Literally the lithosphere is the most extraordinary layer of the earth or commonly referred to as the earth's crust. This layer, broken up into sections or tectonic plates, which moves continuously and is responsible for geological activities on earth, the lithosphere is about 60 miles far in most places.
Lithosphere
The lithosphere is preceded by the asthenosphere, the mantle and the outer and inner strata of the Earth's core. Because the lithosphere is always moving. According to geologists, they believe that all darata on earth originate from a single continent called (Pangea) as a result of thousands of years of stable movements that form continents.
Some Other Facts
The outer lithosphere layer consists of Sio2 and A1203 or, unfortunately, the deepest lithosphere layer consists of chemical compounds SiO2 and MgO or sima.
The boundary between the pesky and sima layers in the earth's surface is irregular.
Between the earth's core and the earth's crust there is a layer of rock.
The earth's core is called Barisfer / Nife, consisting of a composition of nickel and ferum metals.
Earth's lithosphere includes the crust and the top part of the earth's mantle (is dense) which results in the hardness of the outer layers of the planet Earth. Batasa between the matel and the earth's crust is called the moho layer. The lithosphere is supported by the asthenosphere which is the weaker, hotter and deeper part of the mantle. The boundary between the lithosphere and the asthenosphere is distinguished in terms of its response to stress, the lithosphere remains dense over a relatively long geological period and changes elasticly due to cracks while the asthenosphere changes like a thick liquid.
Parts of the Litosphere (Earth Skin)
Damn Layer
The layer of the earth's crust is composed of silisium metal and aluminum, the compounds are in the form of SiO2 and AL 2 O3. In the pesky layer (silisium and aluminum) there are sedimentary rocks, andesite granite types of metamorphic rocks and other rocks found on continental land. The pesky layer is also called the crustal layer and the average 35 km of sandstone.
The crust is divided into two parts, namely:
Continent Crust
It is a solid body consisting of granite rocks at the top and basaltic igneous rocks at the bottom, this crust is a continent.
Ocean crust
It is a solid body consisting of sea sediment at the top, then beneath the volcanic rocks and the lowest is composed of igneous gabro and peridolite. This crust occupies the ocean floor.
Sima Coating (magnesium silicium)
Earth's crust is composed of silisium metals and magnesium in the form of Si O2 and Mg O compounds. This layer has a specific density greater than the pesky layer because it contains iron and magnesium, namely ferrous minerals magnesium and basaltic rocks and has an average thickness averaging 65 km.
Thus the discussion on Understanding the Litosphere along with the Parts and Explanations hopefully with this review can add insight and knowledge of you all, thank you very much for your visit
Lithosphere is the outer shell of a rocky planet. The lithosphere is derived from the Greek word, lithos which means rocky and sphere which means solid. This lithosphere is derived from the word lithos which means rock and sphere means layer. Literally the lithosphere is the most extraordinary layer of the earth or commonly referred to as the earth's crust. This layer, broken up into sections or tectonic plates, which moves continuously and is responsible for geological activities on earth, the lithosphere is about 60 miles far in most places.
Lithosphere
The lithosphere is preceded by the asthenosphere, the mantle and the outer and inner strata of the Earth's core. Because the lithosphere is always moving. According to geologists, they believe that all darata on earth originate from a single continent called (Pangea) as a result of thousands of years of stable movements that form continents.
Some Other Facts
The outer lithosphere layer consists of Sio2 and A1203 or, unfortunately, the deepest lithosphere layer consists of chemical compounds SiO2 and MgO or sima.
The boundary between the pesky and sima layers in the earth's surface is irregular.
Between the earth's core and the earth's crust there is a layer of rock.
The earth's core is called Barisfer / Nife, consisting of a composition of nickel and ferum metals.
Earth's lithosphere includes the crust and the top part of the earth's mantle (is dense) which results in the hardness of the outer layers of the planet Earth. Batasa between the matel and the earth's crust is called the moho layer. The lithosphere is supported by the asthenosphere which is the weaker, hotter and deeper part of the mantle. The boundary between the lithosphere and the asthenosphere is distinguished in terms of its response to stress, the lithosphere remains dense over a relatively long geological period and changes elasticly due to cracks while the asthenosphere changes like a thick liquid.
Parts of the Litosphere (Earth Skin)
Damn Layer
The layer of the earth's crust is composed of silisium metal and aluminum, the compounds are in the form of SiO2 and AL 2 O3. In the pesky layer (silisium and aluminum) there are sedimentary rocks, andesite granite types of metamorphic rocks and other rocks found on continental land. The pesky layer is also called the crustal layer and the average 35 km of sandstone.
The crust is divided into two parts, namely:
Continent Crust
It is a solid body consisting of granite rocks at the top and basaltic igneous rocks at the bottom, this crust is a continent.
Ocean crust
It is a solid body consisting of sea sediment at the top, then beneath the volcanic rocks and the lowest is composed of igneous gabro and peridolite. This crust occupies the ocean floor.
Sima Coating (magnesium silicium)
Earth's crust is composed of silisium metals and magnesium in the form of Si O2 and Mg O compounds. This layer has a specific density greater than the pesky layer because it contains iron and magnesium, namely ferrous minerals magnesium and basaltic rocks and has an average thickness averaging 65 km.
Thus the discussion on Understanding the Litosphere along with the Parts and Explanations hopefully with this review can add insight and knowledge of you all, thank you very much for your visit
The Process of Forming Petroleum With Its Understanding and Components
The Process of Forming Petroleum With Its Understanding and Components
Definition of Petroleum
Petroleum dubbed as black gold (petroleum from Latin petrus - less and oleum - oil) is a thick, dark brown, or burnt green liquid, which is in the upper layers of several areas in the earth's crust,
Petroleum consists of a complex mixture of various hydrocarbons, mostly alkane series, but varies in appearance, purity, and composition. Oil is extracted from oil wells in oil mines.
The location of these wells was obtained after going through a process of geological knowledge, sediment analysis, character and source structure, as well as various other knowledge. Then the oil is processed at the refinery and the results are broken down based on boiling points to produce various fuels,
ranging from gasoline and kerosene to asphalt and various chemical reagents needed to make plastics and medicines. Petroleum is used to produce various goods and materials needed by humans.
Process of Forming Earth's Oil
Earth's oil is the result of decomposition (decomposition) of animal and plant material in an area of subsidence (down) slowly. The area is usually in the form of a lagoon (lake) boundary along the coast or lake in the marsh on the mainland,
Sediment is deposited together with the material and the sedimentation speed must be fast enough so that at least a part of the organic material can be stored and buried well before decay occurs.
The geological time and place of deposition continue to sink deeper into the earth's surface, because of the increasing weight of the sediments and materials piled on it, or because of the tectonic forces that cause the effect of subsidence. Organic material sinks deeper so that it experiences increasingly high pressures and temperatures.
The process will cause chemical changes from these organic materials. The material change is the forerunner to the formation of a mixture of hydrocarbon materials whose composition is very complex, both hydrocarbons in the form of liquids or in the form of gases.
The increase in temperature to an average depth of the world around 20 - 55 degrees Celsius per kilometer. Disumatera alone can reach around 100 ° C / km. Whereas new oil habitats are formed at temperatures around 65 - 150 ° C, which are generally located at depths of 1.5 - 3 km. At a depth of 3-6 km the reservoir rock will be dominated by gas rather than oil. For deeper depths the temperature will be different to be higher so that the gas will be higher so that the gas will experience decomposition.
Usually petroleum is deposited in good porous sedimentary rocks which have a porosity value of 45% (so good reseroar). Because the longer the rock is deposited and buried in the material above, then the rock will be compacted and this can cause the value of porosity to decrease.
Oil, gas, and water will be stored or collected in the pore spaces of the porous rock. Due to gravitational pressure, the fluid moves in the rock slowly. Aid that can escape fluid is called permeable rock.
Petroleum is formed from the breakdown of organic compounds derived from the bodies of small organisms that lived in the sea / waters millions of years ago. The process is that these organisms will die, then settle to the bottom of the sedimentary basin to produce a sedimentary basin.
Then this sedimentary basin will gradually be buried by other rocks above it so that it will gradually fall down where the temperature and pressure increase so that the decomposition process and oil will be produced.
The oil produced by the Parent rocks has a lower density than water so that the oil moves upward through the porous hole, but most of the oil is trapped in non-porous rocks so drilling is needed.
Search for Miyak Bumi
The process of finding (exploration) of oil from the bowels of the earth is carried out by geologists. The modern way used by geologists to search for petroleum is by using satellite imagery and analyzing rock surfaces. After the geologist conducts a series of analyzes and states that in the location there is oil, the next task is taken over by the geophysicist.
Geophysicists study the physical properties of soil layers. Various methods are used in this stage to support the results obtained by geologists. The equipment used to search for petroleum is like Gravimetry (to measure the presence of oil flow due to slight differences in earth's gravity),
Magnetometry (to measure changes in magnetic fields due to oil flow), and Sniffers in the form of electronic devices used to detect hydrocarbon odors. The most commonly used is seismology.
Seismology can be used to find oil reserves both on land and at sea. The main part of seismology is the trigger of vibration and signal reception. There are vibration triggers such as Compressed-air gun (specifically used for offshore exploration), Thumper trucks (for exploration of oil on land), and explosives.
The sound or vibration produced by the Thumper truck emits a signal or sound wave, the signal will be reflected back by the boundaries between different layers of rock captured by the geophone, the data is then sent to the truck that functions as the control center.
By detecting these reflections, experts can draw a map of rock structures below the earth's surface to find oil reserves. If petroleum reserves are positive at a location, the drilling process will begin.
If the center of the petroleum is located offshore, the extraction can be done in 2 ways, namely:
If the distance of the oil center is close to the mainland, a pipeline is planted on the seabed and pumps the earth oil to land.
If the oil center is far from the mainland, a drilling rig will be built and then the results will be taken by the tanker to land
Definition of Petroleum
Petroleum dubbed as black gold (petroleum from Latin petrus - less and oleum - oil) is a thick, dark brown, or burnt green liquid, which is in the upper layers of several areas in the earth's crust,
Petroleum consists of a complex mixture of various hydrocarbons, mostly alkane series, but varies in appearance, purity, and composition. Oil is extracted from oil wells in oil mines.
The location of these wells was obtained after going through a process of geological knowledge, sediment analysis, character and source structure, as well as various other knowledge. Then the oil is processed at the refinery and the results are broken down based on boiling points to produce various fuels,
ranging from gasoline and kerosene to asphalt and various chemical reagents needed to make plastics and medicines. Petroleum is used to produce various goods and materials needed by humans.
Process of Forming Earth's Oil
Earth's oil is the result of decomposition (decomposition) of animal and plant material in an area of subsidence (down) slowly. The area is usually in the form of a lagoon (lake) boundary along the coast or lake in the marsh on the mainland,
Sediment is deposited together with the material and the sedimentation speed must be fast enough so that at least a part of the organic material can be stored and buried well before decay occurs.
The geological time and place of deposition continue to sink deeper into the earth's surface, because of the increasing weight of the sediments and materials piled on it, or because of the tectonic forces that cause the effect of subsidence. Organic material sinks deeper so that it experiences increasingly high pressures and temperatures.
The process will cause chemical changes from these organic materials. The material change is the forerunner to the formation of a mixture of hydrocarbon materials whose composition is very complex, both hydrocarbons in the form of liquids or in the form of gases.
The increase in temperature to an average depth of the world around 20 - 55 degrees Celsius per kilometer. Disumatera alone can reach around 100 ° C / km. Whereas new oil habitats are formed at temperatures around 65 - 150 ° C, which are generally located at depths of 1.5 - 3 km. At a depth of 3-6 km the reservoir rock will be dominated by gas rather than oil. For deeper depths the temperature will be different to be higher so that the gas will be higher so that the gas will experience decomposition.
Usually petroleum is deposited in good porous sedimentary rocks which have a porosity value of 45% (so good reseroar). Because the longer the rock is deposited and buried in the material above, then the rock will be compacted and this can cause the value of porosity to decrease.
Oil, gas, and water will be stored or collected in the pore spaces of the porous rock. Due to gravitational pressure, the fluid moves in the rock slowly. Aid that can escape fluid is called permeable rock.
Petroleum is formed from the breakdown of organic compounds derived from the bodies of small organisms that lived in the sea / waters millions of years ago. The process is that these organisms will die, then settle to the bottom of the sedimentary basin to produce a sedimentary basin.
Then this sedimentary basin will gradually be buried by other rocks above it so that it will gradually fall down where the temperature and pressure increase so that the decomposition process and oil will be produced.
The oil produced by the Parent rocks has a lower density than water so that the oil moves upward through the porous hole, but most of the oil is trapped in non-porous rocks so drilling is needed.
Search for Miyak Bumi
The process of finding (exploration) of oil from the bowels of the earth is carried out by geologists. The modern way used by geologists to search for petroleum is by using satellite imagery and analyzing rock surfaces. After the geologist conducts a series of analyzes and states that in the location there is oil, the next task is taken over by the geophysicist.
Geophysicists study the physical properties of soil layers. Various methods are used in this stage to support the results obtained by geologists. The equipment used to search for petroleum is like Gravimetry (to measure the presence of oil flow due to slight differences in earth's gravity),
Magnetometry (to measure changes in magnetic fields due to oil flow), and Sniffers in the form of electronic devices used to detect hydrocarbon odors. The most commonly used is seismology.
Seismology can be used to find oil reserves both on land and at sea. The main part of seismology is the trigger of vibration and signal reception. There are vibration triggers such as Compressed-air gun (specifically used for offshore exploration), Thumper trucks (for exploration of oil on land), and explosives.
The sound or vibration produced by the Thumper truck emits a signal or sound wave, the signal will be reflected back by the boundaries between different layers of rock captured by the geophone, the data is then sent to the truck that functions as the control center.
By detecting these reflections, experts can draw a map of rock structures below the earth's surface to find oil reserves. If petroleum reserves are positive at a location, the drilling process will begin.
If the center of the petroleum is located offshore, the extraction can be done in 2 ways, namely:
If the distance of the oil center is close to the mainland, a pipeline is planted on the seabed and pumps the earth oil to land.
If the oil center is far from the mainland, a drilling rig will be built and then the results will be taken by the tanker to land
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