Earths interior
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The document describes the four main layers that make up the Earth - the crust, mantle, outer core, and inner core. The crust is the top-most layer where life exists, ranging from 5-25 miles thick. Below is the mantle, a semi-liquid layer 3000 km wide that causes convection currents moving the continents. Deepest are the solid inner core and surrounding liquid outer core, both composed primarily of iron.
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Micro teach: Layers of the Earth
Correction on slide 7- IS hould be Is
Brief summary of each of the layers
As a handout, play dough models of the Earth will be handed out containing layers for people to cut in half and stick labelled toothpicks in each of the layers
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Earth's Structure
The earth is made up of different layers. These layers are of different thicknesses and temperatures.
K6thgradeweatherchapter1notes6thgrade ch-1sec-3layersoftheatmosphere-10032615...
The atmosphere is divided into layers based on temperature changes:
1) The troposphere is the lowest layer where weather occurs and where humans live.
2) The stratosphere absorbs UV radiation and contains the ozone layer.
3) The mesosphere is the coldest part where most meteoroids burn up.
4) The thermosphere is the outermost layer and contains the ionosphere and exosphere, where communication satellites orbit Earth.
Duncan_Notes_Dynamic_Earth
The Earth is not a perfect sphere, but is slightly flattened at the poles and bulging at the equator. It has multiple interior layers, including a crust, mantle, and core. The crust and upper mantle make up the lithosphere, which overlies the asthenosphere and mesosphere in the mantle. The core is divided into a solid inner core surrounded by a liquid outer core. Seismic waves have revealed details of the Earth's internal structure.
Mechanical layers of the earth
the Mechanical layers of the Earth
Distinct Layers
* Compositional Layers
* Mechanical Layers
Compositional Layers is composed of Crust, Mantle and Core while Mechanical Layers is composed of Lithosphere, Asthenosphere, Mesosphere, Outer Core and Inner Core.
Thank you ^-^
Layers of the earth presentation 4
The document describes the four major layers of the Earth:
1) The crust is the top thin solid rock layer where life exists, ranging from 0-870 degrees C in temperature.
2) The thick mantle is the largest layer made of hot dense rock that flows slowly like asphalt.
3) The outer core is a fluid metallic layer that generates Earth's magnetic field and has temperatures over 7,200 degrees F.
4) The inner core is a solid ball of metal deep in Earth's center, kept solid under immense pressure with temperatures over 9,000 degrees F.
Magnetic field
The document discusses the Earth's magnetic field. It is generated by the dynamo effect in the Earth's liquid outer core. As the liquid core circulates due to convection, electric currents and magnetic fields are created. These fields are recorded in ancient rock crystals over 4 billion years old. The tilted magnetic field interacts with the solar wind and magnetosphere to protect the Earth by deflecting charged particles.
Recommended
Micro teach: Layers of the Earth
Correction on slide 7- IS hould be Is
Brief summary of each of the layers
As a handout, play dough models of the Earth will be handed out containing layers for people to cut in half and stick labelled toothpicks in each of the layers
Mountain building
This document discusses different types of aerial photographs and how they are classified. It describes vertical, horizontal, and oblique photographs based on the camera axis. It also discusses classifications based on the angle of coverage such as normal, wide, and super wide angle photographs. The document notes that photographs can also be classified by whether they are black and white, color, infrared, or multi-spectral images. It provides examples of the information that can be seen from different types of aerial photographs.
Earth's Structure
The earth is made up of different layers. These layers are of different thicknesses and temperatures.
K6thgradeweatherchapter1notes6thgrade ch-1sec-3layersoftheatmosphere-10032615...
The atmosphere is divided into layers based on temperature changes:
1) The troposphere is the lowest layer where weather occurs and where humans live.
2) The stratosphere absorbs UV radiation and contains the ozone layer.
3) The mesosphere is the coldest part where most meteoroids burn up.
4) The thermosphere is the outermost layer and contains the ionosphere and exosphere, where communication satellites orbit Earth.
Duncan_Notes_Dynamic_Earth
The Earth is not a perfect sphere, but is slightly flattened at the poles and bulging at the equator. It has multiple interior layers, including a crust, mantle, and core. The crust and upper mantle make up the lithosphere, which overlies the asthenosphere and mesosphere in the mantle. The core is divided into a solid inner core surrounded by a liquid outer core. Seismic waves have revealed details of the Earth's internal structure.
Mechanical layers of the earth
the Mechanical layers of the Earth
Distinct Layers
* Compositional Layers
* Mechanical Layers
Compositional Layers is composed of Crust, Mantle and Core while Mechanical Layers is composed of Lithosphere, Asthenosphere, Mesosphere, Outer Core and Inner Core.
Thank you ^-^
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The document describes the four major layers of the Earth:
1) The crust is the top thin solid rock layer where life exists, ranging from 0-870 degrees C in temperature.
2) The thick mantle is the largest layer made of hot dense rock that flows slowly like asphalt.
3) The outer core is a fluid metallic layer that generates Earth's magnetic field and has temperatures over 7,200 degrees F.
4) The inner core is a solid ball of metal deep in Earth's center, kept solid under immense pressure with temperatures over 9,000 degrees F.
Magnetic field
The document discusses the Earth's magnetic field. It is generated by the dynamo effect in the Earth's liquid outer core. As the liquid core circulates due to convection, electric currents and magnetic fields are created. These fields are recorded in ancient rock crystals over 4 billion years old. The tilted magnetic field interacts with the solar wind and magnetosphere to protect the Earth by deflecting charged particles.
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The document describes the four main layers of Earth - the crust, mantle, outer core, and inner core. The crust is the thinnest solid outer layer averaging 25 miles thick and composed mostly of oxygen, silicon, aluminum and iron. Below is the mantle, a dense hot semi-solid layer 1,802 miles thick composed of silicate minerals. The outer core is a liquid layer of iron and nickel between 4,000-5,000 degrees Celsius and 1,430 miles thick, generating Earth's magnetic field. Within is the inner core, the planet's hottest center at 5,000-7,000 degrees Celsius and solid iron 750 miles thick under immense pressure.
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The earth is composed of three main layers: the crust, mantle, and core. The crust makes up less than 1% of the earth's mass and is the thinnest layer. Underneath is the mantle, which comprises most of the earth's mass and volume. The mantle originates magma and is divided into upper and lower sections. At the center is the core, with a solid inner core surrounded by a liquid outer core.
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1) The document discusses several aspects of Earth's dynamics including its rotation, revolution around the sun, heat distribution, winds and ocean currents.
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3) The document also examines plate tectonics including what drives plate motions via processes such as slab pull and ridge push in the mantle, and how the three main plate interactions shape ocean basins and landforms.
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The document describes the different layers that make up the Earth. It discusses the crust, lithosphere, asthenosphere, continental crust, oceanic crust, mantle, outer core, and inner core. The crust sits on top and is where life exists, and is made up of either lighter continental crust or denser oceanic crust. Below the crust is the mantle, which makes up 80% of the Earth's mass and is hot and rocky. At the center are the outer core, which is liquid, and inner core, which is solid. Boundaries between the layers include the Mohorovicic discontinuity between crust and mantle, and the Gutenberg and Lehmann discontinuities between the layers within the Earth's core
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The Sun is a normal G2 star located at the center of our solar system. It has a diameter of 1.39 million km and contains over 99% of the mass in the system. The Sun's core generates energy through nuclear fusion, converting hydrogen to helium, and this energy radiates outward through convection and radiation to power life on Earth. It has an 11-year solar cycle where its magnetic field and sunspot activity fluctuate.
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The document discusses Earth's inner and outer core. The inner core is a solid ball of iron, nickel, and other elements with a radius of 1,220 km located at the center of Earth. It was discovered in 1936 by Inge Lehmann using seismic waves. The temperature of the inner core is around 5,700 K and pressure is between 330 to 360 gigapascals. The outer core is a liquid layer of iron and nickel around 2,266 km thick located above the inner core and below the mantle. Convection in the outer core generates Earth's magnetic field, which protects the planet from solar winds.
Earth's layer
The earth is composed of three main layers: the crust, mantle, and core. The crust makes up less than 1% of the earth's mass and is the thinnest layer. Underneath is the mantle, which comprises most of the earth's mass and volume. The mantle originates magma and is divided into upper and lower sections. At the center is the core, with a solid inner core surrounded by a liquid outer core.
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The document discusses the Aurora Borealis (Northern Lights). It explains that the lights are caused by charged particles from the sun interacting with the earth's magnetic field. During solar storms, electrons and protons from the sun enter the earth's atmosphere where they cause nitrogen and oxygen atoms to become energized and glow in colorful patterns. The particles are guided by the magnetic field to the magnetic poles, appearing as lights near the north and south poles. The size and shape of the lights depends on the level of solar activity.
The sun and its radiation effects
The sun is a star at the center of the solar system that comprises 99.86% of the total mass. It has a diameter of 1.39 million km and a temperature of 15.7 million kelvin at its core. The sun has several internal layers including a radiative zone where thermal radiation is the primary means of energy transfer and a convective zone where convection currents develop due to lower temperatures and densities. The sun also has an atmosphere above its visible surface, the photosphere, which includes the chromosphere, transition region, corona, and heliosphere. Exposure to sunlight can cause both immediate and long term negative effects on humans like sunburn, sunstroke, skin damage, eye disorders, and skin
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The document discusses different aspects of the Sun's atmosphere. The chromosphere emits pinkish-blue light and can be seen during solar eclipses. Above the chromosphere is the transition zone and corona, which are visible only during eclipses and have much higher temperatures than the photosphere. The solar wind consists of particles that escape the Sun's atmosphere at around 500 km/hr. Solar magnetism involves strong magnetic fields around sunspots that reverse polarity between the northern and southern hemispheres and cause phenomena like prominences. The solar cycle occurs every 11 years as sunspot activity waxes and wanes.
Solar Prominence
Solar prominences are huge loops of solar material that extend outward from the sun's surface. They can be several miles wide and tall. Prominences form over timescales of about a day and contain cooler plasma than the corona, appearing as bright features against the dark sky. The largest prominence observed was over 350,000 km long. Prominences are anchored in the photosphere by magnetic fields and supported against gravity, existing at boundaries between magnetic polarities. They can persist in the corona for several months before erupting.
Internal structure of earth
The Earth is divided into three main layers - the crust, mantle, and core. The crust is the outermost layer extending up to 40 km deep and contains the continents and ocean basins. Below the crust lies the mantle, which extends from the crust to a depth of 2900 km and makes up over 80% of the Earth's volume. The mantle is divided into an upper and lower mantle. Below the mantle is the core, divided into a solid inner core and liquid outer core, which extends from 2890 km to the center of the Earth.
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The document describes the different layers that make up the Earth's interior. The mantle is made up of three layers from outer to inner: the lithosphere, asthenosphere, and mesosphere. The outer core is composed of molten metal which drives the Earth's magnetic field. The inner core is a solid ball of iron and nickel alloy around 1,228 km in radius with temperatures as high as the sun's surface due to extreme pressure deep within the Earth.
In and out of sun
The Sun is a typical star composed of gas held together by gravity that produces energy through nuclear fusion. It is around 5 billion years old and will become a red giant in approximately 10 billion years, expanding and consuming the inner planets. The Sun emits electromagnetic radiation across all wavelengths, with visible light making up 40% of its output. Its internal structure can be studied through helioseismology, which observes oscillations on its surface to learn about conditions in its interior.
Geo persentaion
explanation of the seismology and study of the earth's interior besides the shadow zone and the Moho. the presentation include the gravity anomalies with the definition of the isostasy.
The Aurora Borealis
The Northern Lights, or Aurora Borealis, are caused by interactions between the Earth's magnetic field and particles from the Sun. When solar storms eject electrons and protons from the Sun's surface, they are guided by the magnetic field toward the magnetic poles, where they collide with gases in the atmosphere and release energy in the form of colorful light displays. The auroral oval, which is the main region where the Northern Lights occur, is centered around the magnetic poles and can vary in size and location depending on the level of solar activity and strength of the solar wind. The solar atmosphere reaches temperatures of millions of degrees, causing hydrogen to break into electrons and protons that are then carried away in the solar wind toward Earth and other planets
activities of the sun
Sunspots are dark, cooler areas on the sun's surface caused by strong magnetic fields that inhibit hot gases from rising. They typically last several days but some can persist for weeks. Solar flares are powerful explosions that heat material to millions of degrees and release energy equivalent to billions of tons of TNT in just minutes. They occur near sunspots along dividing lines of opposing magnetic fields. Solar prominences are dense loops of gases suspended above the sun for days or weeks by magnetic fields but can erupt, releasing a huge sheet of gases into space over hours.
Our Dynamic Earth
The document provides information about the Earth's layers, including the mantle and tectonic plates. It describes how igneous rocks are formed from magma underground or lava above ground. It also explains how sedimentary rocks are formed over millions of years from the erosion and deposition of earth materials. Metamorphic rocks are formed from intense heat and pressure changing other rock types over long periods of time.
Sun's layer
The document describes the different layers of the Sun from the photosphere to the corona. The photosphere is the deepest layer at 250 miles thick and ranges from 6500K to 4000K in temperature. Above is the chromosphere ranging from 250 to 1300 miles and 4000K to 8000K. The narrow transition region between the chromosphere and corona ranges from 8000K to 500,000K. The outer corona extends 1300 miles and reaches temperatures over 500,000K. Various solar phenomena like granules, faculae, sunspots, auroras, and prominences are also mentioned.
Explanation Text About Aurora
Aurora are bright glows caused by collisions between charged particles from the solar wind and atoms in the Earth's upper atmosphere. The solar wind carries the Sun's magnetic field and particles through space at around 400 km/s, shaping the Earth's magnetosphere into an elongated bubble. Under certain conditions, the solar wind's magnetic field can merge with Earth's, creating electrical currents that drive particles into the polar atmosphere, causing the visible auroral displays usually seen in night skies at high latitudes, known as the northern lights in the northern hemisphere and southern lights in the southern hemisphere.
Module 4 the earth's dynamics
1) The document discusses several aspects of Earth's dynamics including its rotation, revolution around the sun, heat distribution, winds and ocean currents.
2) Key concepts covered include how Earth's orbit influences climate and seasons, how heat is transferred both from the sun and within Earth, and how atmospheric circulation forms weather systems like cyclones.
3) The document also examines plate tectonics including what drives plate motions via processes such as slab pull and ridge push in the mantle, and how the three main plate interactions shape ocean basins and landforms.
6.sun
The Sun is a normal G2 star that contains over 99% of the mass in the Solar System. It has a diameter of 1.39 million km and a surface temperature of 5,800 K. Energy is created in the Sun's core through nuclear fusion and radiates outward through convection and radiation zones to the surface. The Sun's 11-year activity cycle causes variations in sunspots, flares, and other magnetic phenomena. In the future, the Sun will expand into a red giant after exhausting its hydrogen fuel supply over many billions of years.
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Similar to Earths interior
Layersoftheearth22
The document describes the layers of the Earth, including the crust, mantle, outer core, and inner core. It provides details on the composition, thickness, and properties of each layer. The crust is the outermost solid layer and is divided into continental and oceanic crust. Beneath the crust is the mantle, which makes up over 80% of the Earth's volume and is divided into the upper, transition, and lower mantle zones. The outer core is liquid, while the inner core is solid.
Interior of the earth
The document discusses the layers of the Earth's interior. It describes the crust, mantle, and core. The crust consists of two types - thin oceanic crust made of basalt and thicker continental crust made of granite. The mantle lies below the crust and makes up 84% of the Earth's volume. It is divided into the rigid lithosphere above and plastic asthenosphere below. The core is divided into a solid inner core and liquid outer core made of iron and nickel.
Module-1-LITHOSPHERE1 (GRADE 10 SCIENCE FIRST QUARTER MODULE )1upload.pptx
The document discusses the layers of the Earth's lithosphere. It describes the lithosphere as the cool, rigid outer layer of the Earth made up of crust and upper mantle. The lithosphere is divided into tectonic plates that float on the asthenosphere. There are two types of plates - continental plates composed of less dense rocks found under land, and oceanic plates made of denser rocks under oceans. The boundaries between plates experience geological events like earthquakes and volcanoes.
Structure and composition.pdf
The document summarizes the three main layers that make up the structure of the Earth:
1. The crust is the outermost layer and is divided into continental and oceanic crust. The oceanic crust is thinner, around 5-10 km thick, and composed mainly of basalt.
2. The mantle is the largest layer and makes up most of the Earth's volume. It is around 2900 km thick and can be divided into upper and lower mantle layers.
3. The core is the innermost layer and can be divided into a solid inner core and liquid outer core which generates the Earth's magnetic field.
STRUCTURE AND COMPOSITION OF EARTH
The document summarizes the three main layers that make up the structure of the Earth:
1. The crust is the outermost layer and is divided into continental and oceanic crust. The continental crust is thicker while the oceanic crust is thinner.
2. The mantle is the largest layer and is divided into upper and lower mantle. It is composed mainly of iron and magnesium and contains most of the Earth's internal heat.
3. The core is divided into a solid inner core and liquid outer core. The outer core is responsible for the Earth's magnetic field and rotation, while the inner core is made mostly of solid iron.
Interior of the earth
This document provides information about the layers of Earth's interior. It is divided into three main layers: the crust, mantle, and core.
The crust is the outermost layer and is divided into two sublayers - the continental crust (Sima) and oceanic crust (Sial). Sima is less dense and older, while Sial is denser and younger. The mantle, the second layer, is also divided into upper and lower sections. The upper mantle is solid while the lower mantle is molten. The core is the innermost layer and consists of nickel and iron. It has a solid inner core and molten outer core. Temperature and pressure increase significantly with depth into Earth.
Earth internal structure
The document summarizes the structure and composition of Earth's interior layers. It describes how seismic waves and samples from deep drilling provide evidence that the Earth has distinct layers, including a crust, mantle, outer core, and inner core. The crust varies in thickness and composition between continental and oceanic crust. Below the crust lies the mantle, which makes up over 80% of the Earth's volume and is divided into an upper and lower mantle. The lower mantle and outer core are liquid, while the inner core is solid.
ramosearthscience.pptx
The document describes the different layers that make up the Earth. It discusses three main layers - the crust, mantle, and core. The crust is the topmost layer and is broken into tectonic plates. Below the crust is the mantle, made of hot dense rock that flows slowly due to convection currents. The core is at the center and has a solid inner core surrounded by a liquid outer core made of iron and nickel.
Internal Structure of The Earth? Major Structural unit of the earth
The document summarizes the internal structure of the Earth in 3 main layers - the core, mantle, and crust. The core is divided into a solid inner core and liquid outer core, mostly composed of iron and nickel. The mantle, making up most of the Earth's mass, is solid but can slowly deform and is composed of silicate compounds. The crust is the coolest and thinnest layer, composed of silicate minerals.
L1_D1_INTERNAL STRUCTURE OF THE EARTH.pptx
The document describes the internal structure of the Earth. It is comprised of several concentric layers from the crust on the outside to the inner core at the center. The crust and upper mantle make up the lithosphere which is broken into tectonic plates. Beneath the lithosphere is the asthenosphere which is hot and plastic allowing the tectonic plates to move via convection currents in the mantle. Driving and resisting forces influence plate motions. Evidence like matching continents and fossil/rock similarities support plate tectonics theory. The mantle comprises most of the Earth's volume and transfers heat via convection currents. The outer core is liquid while the solid inner core is extremely hot. Boundaries between layers are marked
Lesson 3_Science 10- Q1W3_ Plate Movement.pptx
The Earth is divided into three main layers - the crust, mantle, and core - based on their composition. The crust is the outermost solid layer and is divided into continental and oceanic crust. Below the crust is the mantle, which is divided into the upper and lower mantle. The innermost layer is the core, consisting of a solid inner core surrounded by a liquid outer core. These layers move and interact through plate tectonics.
Finalpresentation
The document describes the different layers of the Earth, including the crust, mantle, outer core, and inner core, providing details on the thickness and composition of each layer. It explains that the mantle makes up most of the Earth's volume and drives plate tectonic processes through convective circulation. Additionally, it outlines that the lithosphere and asthenosphere describe the mechanical properties of the Earth, with the lithosphere comprising rigid tectonic plates floating on the weaker asthenosphere.
Finalpresentation
The document describes the different layers of the Earth, including the crust, mantle, outer core and inner core, along with their thicknesses and primary compositions. It explains that the mantle is the thickest layer and is separated into the upper and lower mantle, with most of the Earth's internal heat located in the mantle. The core is divided into the liquid outer core and solid inner core, with the Earth's magnetic field believed to be controlled by the outer core.
Lithosphere
Ophiolites provide evidence for the composition and structure of oceanic crust and the upper mantle. They represent sections of oceanic crust and upper mantle that have been obducted or thrust onto continental margins. Studying ophiolites like the Samail ophiolite in Oman has helped scientists understand the layered sequence of rocks that make up oceanic crust, including extrusive basalts, dikes, and intrusive gabbros.
EARTHS INTERIOR1.pptx
The document discusses the different layers of the Earth - crust, mantle, and core. The crust is the thinnest layer and is made up of two types, continental and oceanic. Below the crust is the mantle, which is divided into upper, middle, and lower sections. The middle mantle's convection currents cause the movement of tectonic plates. The largest layer is the core, with an inner solid section and outer liquid section, which is responsible for the Earth's magnetic field. Temperature, density, and pressure all increase with depth through the layers.
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Earth's internal heat comes from three main sources:
1) The accretion of dust and gas particles during the Earth's formation released gravitational potential energy and caused internal heating.
2) Radioactive decay of elements in the Earth's core and mantle, such as uranium and potassium, continues to generate heat.
3) Frictional heating from convection currents in the mantle also contributes to the Earth's internal heat. Seismic waves have allowed scientists to indirectly learn about the Earth's layered structure despite only drilling about 7 miles deep.
Crust core and mantle
The document summarizes the composition and structure of the Earth's layers. It describes the crust, mantle, and core based on composition, thickness, temperature, and density. The crust is the outermost solid layer and is divided into continental and oceanic crust. The mantle lies below the crust and is also divided into layers. Seismic wave measurements indicate the mantle transitions to a liquid outer core and solid inner core at the Earth's center.
T1 2 tectonica_placas2
Plate tectonic, pioneers of plate tectonics, how do plates move, structure of Earth, layers of Earth, mechanical properties, composition, sismic waves.
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Introduction to Earth
Earth is composed of four main layers - crust, mantle, outer core, and inner core. The crust is the outermost layer and is made up of either continental or oceanic crust. Below the crust is the mantle, which is divided into lithosphere, asthenosphere, upper mantle, and lower mantle. The outer core is a liquid layer made of nickel and iron that generates Earth's magnetic field. The inner core is made of solid iron deep within Earth. Overall, Earth's composition is approximately 34.6% iron, 29.5% oxygen, and 15.2% silicon.
Layers of the Earth and its Composition.pptx
The document describes the three main layers of the Earth - crust, mantle, and core. It explains that the crust is the thinnest layer and is divided into tectonic plates that move due to convection currents in the mantle. The mantle, which is the largest layer, flows slowly due to these convection currents caused by hot material rising and cool material sinking. Temperature, density and pressure all increase with depth in the Earth. The core is the center-most layer and has a solid inner core surrounded by a liquid outer core.
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Bio evolution
Natural selection occurs through a 5 step process: 1) Variation exists within populations, 2) Organisms compete for limited resources, 3) Organisms produce more offspring than can survive, 4) Genetic traits are passed to offspring, 5) Those organisms with traits most beneficial to survival and reproduction are more likely to survive and reproduce. The document also lists key terms related to biological evolution such as mass extinction, homologous structures, and vestigial structures.
Sealey evolution
This document provides an overview of the key concepts and evidence for the theory of evolution through natural selection. It explains that evolution means change over time as life adapts to survive obstacles. Charles Darwin observed variations between populations and that traits enabling survival and reproduction were selected for. His theory of natural selection and evidence like vestigial organs, homologous and analogous structures, and speciation have supported evolution as the foundation of biology.
K/T Extinction
The document discusses the Cretaceous-Tertiary (K-T) extinction event that occurred 65 million years ago. It notes that this was a mass extinction where over 50% of all species died, including non-flying dinosaurs, many marine invertebrates, flying pterosaurs, mosasaurs, and plesiosaurs. The main proposed cause is the Chicxulub impact crater, evidence for which includes the rare metal iridium and shocked quartz found in K-T boundary layers worldwide. The impact would have released huge amounts of energy, darkened skies for years with dust and ash, and caused global climate changes that disrupted ecosystems.
How rocksform
Rocks are classified into three major groups: igneous rock forms when magma or lava cools, sedimentary rock forms when particles are pressed together, and metamorphic rock forms when heat and pressure change any existing rock.
Rocks
The document discusses the three main types of rocks: sedimentary, metamorphic, and igneous. Sedimentary rocks are formed from the compression of sediment layers over time. Metamorphic rocks were once sedimentary or igneous rocks, but were changed by heat and pressure. Igneous rocks form either underground from cooled magma or above ground from volcanic eruptions. Examples of each rock type are also provided.
The rockcycle
The rock cycle describes how rocks are continuously transformed between three main types - igneous, sedimentary, and metamorphic rocks - through geological processes such as erosion, deposition, burial, melting, and crystallization. Igneous rock is weathered into sediment and deposited to form sedimentary rock, which is then buried and altered by heat and pressure into metamorphic rock. Metamorphic rock can be melted into magma and erupt as new igneous rock, restarting the cycle.
Geological evolution
Geological evolution refers to gradual changes in the Earth over time, including through plate tectics. Plate tectonics involves large pieces of the Earth's outer layer called plates that move and change position. One aspect is continental drift, where the shifting plates cause continents to gradually change location. Scientists believe the continents were once joined in a supercontinent called Pangaea. Relative dating uses rock layers and fossils to determine the age of rocks, such as the law of superposition that the top layer is youngest and bottom oldest.
The geological time scale
The document discusses the Geological Time Scale which is used to divide Earth's history into eras, periods and epochs based on fossil and rock evidence. It describes the major eras - Precambrian, Paleozoic, Mesozoic and Cenozoic - along with key environmental conditions and lifeforms that existed during each era, noting major extinction events. The timeline shows how life on Earth has evolved and changed dramatically over its approximately 4.5 billion year history.
Earth’s history intro
Earth's history can be determined through relative and absolute dating methods. Relative dating uses the law of superposition to determine the relative age of rocks and fossils by their position in rock layers, with lower layers being older. Absolute dating provides specific numerical ages by using radiometric dating techniques to measure the decay of radioactive elements. Together these methods are used to construct geologic timescales that reveal the order and ages of events in Earth's development.
Continental drift pp
Alfred Wegener proposed the theory of continental drift in 1912, which stated that approximately 250 million years ago, all the continents were joined together in a supercontinent called Pangaea. Over time, the continents gradually drifted apart to their current locations. The key evidence for continental drift included the matching coastline shapes of continents, the presence of matching fossil distributions on different continents, identical rock patterns found across continents, and evidence of past shared climates from fossil evidence.
Fossils power point
Scientists study Earth's past environments and lifeforms by examining fossils. Fossils form when organisms are buried and their remains are replaced with minerals over time. There are different types of fossils including molds, casts, petrified remains, preserved fossils like those trapped in ice or amber, carbonized remains, and trace fossils like footprints. Together, the analysis of these various fossil types provides evidence about ancient organisms, environments, behaviors and evolutionary relationships.
Geo time
This document discusses the history of determining the age of the Earth. It describes how early estimates ranged from thousands of years based on biblical interpretations to hundreds of millions of years based on experiments measuring cooling of materials and sediment accumulation. The development of radiometric dating in the early 1900s allowed for more precise measurements by analyzing the decay of radioactive isotopes. Radiometric dating of the oldest rocks and minerals has provided evidence that the Earth is approximately 4.5 billion years old and the solar system formed around 4.6 billion years ago.
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Earths interior
- 1. JOURNEY TO THE CENTER OF EARTH
- 2. LAYERS OF THE EARTH Crust Mantle Outer Core Inner Core
- 3. THE CRUST Layer that we live on (Lithosphere) 5-25 miles thick Consists of cooled rock Thinnest layer of the earth There are 2 kinds of Crust: Continental (thicker) and Oceanic (thinner)
- 4. CRUST QuickTime™ and a Sorenson Video 3 decompressor are needed to see this picture.
- 5. THE MANTLESemi-liquid (magma) 3000 km wide softer closer to the surface (Asthenosphe re) Has convection currents that move the continental plates
- 6. THE MANTLE QuickTime™ and a Sorenson Video 3 decompressor are needed to see this picture.
- 7. THE OUTER CORE Liquid, molten rock Very high temperatures Made of Nickel and Iron
- 8. THE INNER CORE Solid layer Solid because of high pressure Mostly Iron 6,000 degree Celsius. 2,100 km wide
- 9. THE CORE QuickTime™ and a Sorenson Video 3 decompressor are needed to see this picture.
- 10. THE CORE QuickTime™ and a Sorenson Video 3 decompressor are needed to see this picture.