draw the symbol/s in the corresponding layer of the earth.
1. draw the symbol/s in the corresponding layer of the earth.
Answer: imaginary lines
Explanation: you said EARTH
2. 1. Draw the interior layer of the Earth as shown in Figure 2. 2. Describe the different interior layer of the Earth using symbols from the response grid on the right of Figure 2. 3. Draw the symbol/s in the corresponding layer of the Earth.
Draw the interior layer of the Earth as shown in Figure 2.
2. Describe the
Explanation:
ss
3. Activity 2 Objectives: • • Describe the properties of the layers of the Earth. Tell the composition of the layers of the Earth. Our Dynamic Earth Procedure: 1. Label the drawing corresponding to the Earth's layers. 2. Describe the different layers of the Earth using symbols. 3. Choose from the response grid on the right the symbol that you need to finish the figure on the left. 4. Draw the symbol/s in the corresponding layer of the Earth.
The layers of the earth consist of the crust, mantle, outer core and inner core.
Detail of Explanation:
CrustEarth's crust means the outermost shell of the Earth. Beneath the crust is the mantle, also mostly solid rock and minerals, but broken down by soft areas of semi-solid magma. At the center of the Earth is a hot, dense metal core. The crust and upper mantle are part of a single geological unit called the lithosphere. The Earth's crust is made up of igneous, metamorphic, and sedimentary rocks. Most common rocks are igneous rocks that form when magma cools. Crust is divided into two types: oceanic crust and continental crust. Silicates (primarily compounds of silicon and oxygen) are the most abundant rocks and minerals.
Oceanic crust is composed of various types of basalt, mostly silicate and magnesium-rich rocks. It is dense, about 3 grams per cubic centimeter (1.7 ounces per cubic inch). The age and density of oceanic crust increase with distance from mid-ocean ridge; it breaks down at subduction zones. Subduction is an important geological process in which a tectonic plate melts or falls beneath a less dense lithospheric plate at a converging plate boundary.
Continental crust is composed of various types of granite. Like oceanic crust, continental crust is formed by plate tectonics. The crust stretches unevenly underground and protrudes into the atmosphere. Thickest parts of the continental crust are found in the highest mountain ranges in the world. Some sections of continental crust may be as old as the Earth itself.
MantleThe mantle is 84% of the Earth's total volume and lies between its core and outer layer, the crust. Mantle activity drives plate tectonics and contributes to volcanoes, seafloor spreading, earthquakes, and mountain building. It is mostly hard rock, but less viscous at tectonic plate boundaries and mantle plumes. The mantle rocks there are soft and can move plastically over millions of years under great pressure.
Upper Mantle
The upper mantle is a region of the Earth's interior that extends from the surface to a depth of about 410 kilometers (255 miles). The two parts of the upper mantle - the lithosphere and asthenosphere - are often recognized as distinct regions within the Earth.
LithosphereThe lithosphere is the outer hard part of the Earth, extending to a depth of about 100 kilometers (62 miles). The division of the lithosphere between the crust and mantle is called the Mohorovic discontinuity, or simply Moho. Moho lies about 8 kilometers (5 miles) below the ocean and about 32 kilometers (20 miles) beneath the continent.
AsthenosphereAsthenosphere is a dense and weak layer beneath the lithospheric mantle. It lies between about 100 kilometers (62 miles) and 410 kilometers (255 miles) below the surface. The temperature and pressure in the asthenosphere are so high that the rock softens and partially melts into a semi-molten state. This is where geologists mark the difference in ductility between the two layers of the upper mantle.
Lower Mantle
The lower mantle extends from about 660 kilometers (410 miles) to about 2,700 kilometers (1,678 miles) below the surface. The lower mantle is hotter and denser than the upper mantle and the transition layer. Heat usually responds to rock softening, while strong pressure holds the lower mantle tight.
Outer CoreThe outer core of the Earth is composed primarily of liquid iron and nickel. The hottest part of the core is actually the Bulls discontinuity, reaching temperatures of 6,000 degrees Celsius (10,800 degrees Fahrenheit). The churned metals of the outer core create and maintain the Earth's magnetic field.
Inner CoreThe inner core of the Earth is a hot, dense sphere of (mostly) iron. Unlike the outer core, the inner core is not liquid and is not molten. Pressure and density are too great for iron atoms to be in the liquid state. Some geophysicists prefer to interpret it as a plasma that behaves like a solid rather than a solid.
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4. Activity 6: You can do more!Directions: Label the Structure of the Earth with it's layers and write it'sfunctions, illustrate/Draw lines on how P-Wave and S-wave travel through thelayers of the earth and write it's characteristics. Write your answer in the box.Answer Box:Epicenter of Earthquake13
Answer:
The inner core is solid, the outer core is liquid, and the mantle is solid/plastic.And crust us outer part of the earth.
P waves travel fastest and are the first to arrive from the earthquake. In S or shear waves, rock oscillates perpendicular to the direction of wave propagation. In rock, S waves generally travel about 60% the speed of P waves, and the S wave always arrives after the P wave.
5. Independent Practice Directions: Following is an illustration of the earth's interior and what state of matter each layer is made of. Re-draw the illustration and determine which body wave(s) pass/passes through each layer by labeling them with “P", "S", or "Pand S". Remember: P-waves pass through solids and liquids and S-waves pass only through solids.kung sino Po Sana Yung maysagot Po nito pakisagutan Po ng maayos salamat Po
Answer:
crust - P
mantle - S
outer - P
inner - S
Explanation:
hihi sorry kung mali huhu
6. Directions: Read the statements with understanding. Draw a smiley () if the statement isTrue. If it is false, box the word or group of words that make/s it wrong, then write theappropriate word in the space provided for1. Earthquake waves are waves of energy that travel throughEarth, and radiates in all directions from the epicenter in the form of wave.2. Body waves travel through the exterior of the Earth.3. There are two types of surface waves: the Love waves and theRayleigh waves4. Surface waves are able to travel though the Earth's innerlayers, they are used by scientists to study the Earth's interior.5. Love waves cause the most damage to structures during anearthquake
Answer:
1. smile
2. wrong-exterior, right-interior
3. smile
4. wrong-surface wave, right-body wave
5. smile
7. Activity 5: What's Within Directions: Label each layer of the earth and draw a P and S wave as it passes through the earth. Start from the focus (arrow) on top down to the dot below the illustration. Use the rubrics for the illustrations of the Seismic waves. A. B. C. D.
Answer:
If the entire earth was of uniform composition, then P and S waves would travel through the earth along essentially straight lines.
Explanation:
8. Materials: water sauce pan small bowl fresh egg.Procedures:1. Using the sauce pan and water cooked the egg for 15 mins., (Be careful with the fire and the hot pan with water)2. After 15 min. put off the fire then carefully transfer the boiled egg to the small bowl with water.3. Try to hold the egg if the temperature subsides (not cold), and observe. You can grasp and shake the egg.4. While you can feel it`s(egg) hotness, roll it on the table with a little force then observe.5. Slowly fell off the shell and observe.6. Cut the egg into half and observe clearly and thoroughly. Touch the egg yolk and the outer part of the white part of the egg observe its temperature. Is there a distinct portion in the center of the yolk?Questions:1. What did you observe when you shake the egg?2. What happens to the shell as you roll it with force on the table? 3. What did you notice when you slowly fell off the shell? Was there a thin plastic like sheet before the white part? 4. Is there a slight difference of temperature between the yolk and the albumin(white).5. What is the shell if the egg represents the earth?What does the albumin and the egg yolk represents?6. What are the 4 layers of the solid earth comparable to that of the egg?7. Draw the earth with the 4 layers and label.
Answer:
Materials:
water sauce pan small bowl fresh egg.
Procedures:
1. Using the sauce pan and water cooked the egg for 15 mins., (Be careful with the fire and the hot pan with water)
2. After 15 min. put off the fire then carefully transfer the boiled egg to the small bowl with water.
3. Try to hold the egg if the temperature subsides (not cold), and observe. You can grasp and shake the egg.
4. While you can feel it`s(egg) hotness, roll it on the table with a little force then observe.
5. Slowly fell off the shell and observe.
6. Cut the egg into half and observe clearly and thoroughly. Touch the egg yolk and the outer part of the white part of the egg observe its temperature. Is there a distinct portion in the center of the yolk?
Questions:
1. What did you observe when you shake the egg?
2. What happens to the shell as you roll it with force on the table?
3. What did you notice when you slowly fell off the shell? Was there a thin plastic like sheet before the white part?
4. Is there a slight difference of temperature between the yolk and the albumin(white).
5. What is the shell if the egg represents the earth?
What does the albumin and the egg yolk represents?
6. What are the 4 layers of the solid earth comparable to that of the egg?
7. Draw the earth with the 4 layers and label?
Eh saan po yung TANONG?
9. Activity 5: What's Within Directions: Label each layer of the earth and draw a P and S wave as it passes through the earth. Start from the focus (arrow) on top down to the dot below the illustration. Use the rubrics for the illustrations of the Seismic waves. A. B C. D
Answer:
A.Crust
B.Mantle
C.Core
D.Inner Core
Pa Brainlies and
pa fallow nadin
10. Fill in the blanks with the correct word/s states that the oldest layer is at the bottom of a rock layer white the youngest is at the top. refers to the process when sediments pile up which eventually form into a layer. 3. The gradual movement of continents over a period of time is called 4. The movement of plates in Earth's crust is called refers to the deformation of rock layers due to the compressive forces. A. Directions: Draw the concept of stratification. You may write your concept map in a separate sheet. B. Directions: Observe the photo below. Then answer the question that follows. Amur Plate convergent boundary divergent boundary transform boundary subduction zone speed (ref: African plate> (mimiyy orogeny ** name of plata Pacific Plate Yangtze Plate Mariana Plate 102 BA Philippmes Orogany Sunda Plate Caroline Platepatulong po please
Answer:
1. The pronciple of Superposition
2.lithification
3. continental drift
4. Tectonic shift
5. Folds
11. Guide Questions: (You must answer these Guide Questions)Q1. Describe the velocity of the seismic waves as they move deeper into the earth. Is itconstant? Or changing?Q2. Which of the two seismic waves has a faster velocity? P-wave or s-wave?Q3. What is happening to the velocity of both p-wave and s-wave in the mantle?Increasing or decreasing?Q4. What happened to the velocity of the p-wave at the D-layer?Q5. What is the reason why the s-wave disappear at the D-layer?Q6. Based on your own understanding of our lesson. Illustrate through drawing the twotypes of seismic waves (p-wave and s-wave)
Answer:
VELOCITY OF SEISMIC WAVEExplanation:
P-waves are pressure waves that movement quicker than different waves through the earth to show up at seismograph stations first, henceforth the name "Essential". These waves can go through a material, including liquids, and can travel almost 1.7 occasions quicker than the S-waves. Speeds of P wave and S wave are 8.1 and 4.5 km/s separately. Peridotite is the stone kind found in mantle. From 50 to 250 km seismic wave speed diminishes, showing an adjustment of piece. The speed of S-waves diminishes inside a zone just beneath the lithosphere. This recommends that the peridotite inside this zone contain a couple of percent fractional liquefy, however insufficient to totally stop the S-waves. This district is consequently alluded to as the low speed zone or asthenosphere.
the speed of the seismic wave depends on:
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12. Mul Identification: Write the word/s being described by the statement or question. Write your answer on the space provided before the number. Refer your answer to the listed words inside the box. Conserve renewable resources Eclipse Amihan Equator Latitude Habagat Lunar eclipse Solar eclipse Sea breeze Land Breeze Longitude Monsoon Nonrenewable resources Troposhere 1. To preserve, or to avoid wasteful use. 2. The imaginary line circling the Earth halfway between north and south poles. 3. Imaginary lines on a map or that globe that measure distance in degrees north or south of the equator. Lines extends horizontally, from east to west on a globe. 4. Imaginary lines on a map or globe that measure distance in degrees east or west of the prime meridian. Lines extends vertically, from pole on a globe. 5. A natural resource such as coal, gas or oil that once consumed, cannot be replaced. 6. These are organic natural resources which can be replenish. 7. Known as the northeast monsoon draws "cold, dry air" from Siberia, China and Japan. 8. Known as southwest monsoon in the Philippines. It is characterized by hot and humid weather, frequently heavy rainfall, and a prevailing wind from the west. 9. It is the seasonal wind of the Indian Ocean and Southern Asia, blowing from the southwest in summer and from the northeast in winter. 10. It is the layer of the atmosphere closest to the earth's surface, where all weather phenomena takes place. asmoo solo apr ar 11. It is the partial or complete blocking from view of one object by another. 12. It occurs when the moon moves through Earth's shadow at full moon. 13. Moon casting a shadow on Earth and blocking our view of the sun. 14. The moving of air or wind from sea to land during daytime. 15. The moving of air or wind from land to sea during night time.
Answer:
I just to search for an answer here.. Just help me
13. MANUEL S. ENVERGA UNIVERSITY FOUNDATION-CATANAUAN INC.Quezon, PhilippinesDate of Submission: April 9 2021Gear & Section:4th Quarter Week 3 (12-16)Learning kit for Grade 7 OnlineLearners Textbook: 354-382Subject: Science 7Topic: Interaction in the AtmosphereOverviewThe atmosphere is the blanket of air that surrounds planet Earth. Air is the mixture ofdifferent gases held by Earths gravity. The gases that compose the atmosphere have important roleto play in the life and functions of all living things. The atmosphere extends from earths surface upto an altitude of about 560 kilometers. As the altitude increases, the atmosphere gets thinner.ObjectivesAt the end of this topic, you should be able to:1. Discuss how energy from the sun enters the atmosphere;2. Explain how some human activities affect the atmosphere;3. Account the occurrence of land and sea breezes, monsoons, and intertropical convergencezone (ITCZ); and4. Describe the effects of certain weather system in the Philippines.I.LoopHow do we use Air?Draw a conclusion about the following1. Fact: People use air to2. Fact: People use air to3. Fact: People use air toTo make other kinds of energyConclusion:Air isPeople use air in many ways.II.Remembering ContentSet A: Multiple choice. Choose the best answer that will make each sentencecomplete. Write the letter of your choice in the blank before the number.1. The instrument that measures air pressurea. Thermometer b. barometer c. hygrometer d. Anemometer2. Wind that occurs during nighttime is calleda. Land breezeb. Frontc. Sea breezed. calm wind3. Cold air masseswarm air masses.a. Are lighter thanc. is heavier thanb. Have the same weight asd. are less dense than4. The is the atmospheric layer that reflects radio waves back to Earth.a. Exosphereb. thermospherec. ionosphered. ozone
Answer:
1 B
2C
3B
4A
I am not sure if correct or wrong
Answer:
1. D.
2. D.
3. B.
4. A.
Explanation:
Yan po sagot ko
14. 1.label the drawing corresponding to the Earth's layers2.describe the different layers of the earth using symbols3. choose from response grid on the right the symbol that you need to finish the figure on the left4draw the symbol/s in the corresponding layer of the earth
Below the image is a description of the tasks. The Earth's layers are the crust, mantle, outer core, and inner core.
Explanation Specification:
Earth's crust refers to the planet's outermost shell. Below the crust is the mantle, which consists primarily of solid rock and minerals and is broken up by regions of semi-liquid lava. Finally, a heated, dense metal core is at the Earth's center. The crust and upper mantle comprise the lithosphere, a single geological structure. The Earth's crust is composed of igneous, metamorphic, and sedimentary rocks. Igneous rocks, which form as magma cools, are the most prevalent type of rock. There are two forms of crust: oceanic crust and continental crust. The most abundant rocks and minerals are silicates (mainly silicon and oxygen molecules).
The oceanic crust is predominantly composed of silicate- and magnesium-rich basalt rocks. It is dense, weighing around 3 grams per cubic centimeter (1.7 ounces per cubic inch). The age and density of the oceanic crust grow with distance from the mid-ocean ridge, and it disintegrates in subduction zones. Subduction is a crucial geological process in which a tectonic plate melts or sinks into a thinner lithospheric plate at a boundary between converging plates.
Various varieties of granite make up the continental crust. Plate tectonics forms continental crust similarly to oceanic crust. The crust protrudes from the Earth and extends irregularly into the atmosphere. The thickest portions of the continental crust are located in the world's highest mountain ranges. A portion of the continental crust may be as old as the Earth itself.
Mantle
The mantle comprises 84% of the Earth's total volume and is located between the core and crust. Plate tectonics is driven by mantle activity, which contributes to volcanism, seafloor spreading, earthquakes, and mountain formation. The rock is less dense at tectonic plate borders and mantle plumes than elsewhere. In contrast, mantle rocks are flexible and can move plastically over millions of years while being subjected to immense pressure.
Upper Mantle
The upper mantle is a part of the Earth's interior that reaches approximately 410 kilometers below the surface (255 miles). The lithosphere and asthenosphere are typically recognized as two different zones on Earth.
Lithosphere
The lithosphere is the hard outer layer of the Earth, reaching approximately 100 kilometers deep (62 miles). The boundary between the crust and mantle of the lithosphere is known as the Mohorovic discontinuity, or simply Moho. Moho is located approximately 8 kilometers (5 miles) beneath the ocean and 32 kilometers (20 miles) beneath the continent.
Asthenosphere
The asthenosphere is a dense and fragile layer beneath the mantle of the Earth's crust. It is between 100 and 410 kilometers (62 and 255 miles). In the asthenosphere, the temperature and pressure are so great that the rock becomes pliable and partially molten. This is where geologists identify the difference in flexibility between the upper mantle's two layers.
Lower Mantle
The lower mantle spans from approximately 660 to 2,700 kilometers (410 to 1,670 miles) below the surface. The lower mantle is denser and has a higher temperature than the upper and transition layers. Typically, heat causes the rock to soften, whereas high pressure contracts the lower mantle.
Outer Core
The Earth's outer core is mainly made of liquid iron and nickel. The Bulls discontinuity is the hottest section of the core, with temperatures reaching 6,000 degrees Celsius (10,800 degrees Fahrenheit). The outer core's molten metals generate and maintain the Earth's magnetic field.
Inner Core
The Earth's inner core is a hot, dense sphere of (mostly) iron. Contrary to the outer core, the inner core is neither liquid nor molten. Iron atoms cannot be in a liquid form because the pressure and density are too high. Some geophysicists prefer to understand it as plasma with solid-like properties rather than as a solid.
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15. II. Directions: Read the statements with understanding. Draw a smiley (0) if the statement is True. If it isfalse, box the word or group of words that make/s it wrong, then write the appropriate word in the spaceprovided for1. Earthquake waves are waves of energy that travel through Earth, and radiatesin all directions from the epicenter in the form of wave.2. Body waves travel through the exterior of the Earth3. There are two types of surface waves: the Love waves and the Rayleigh waves4. Surface waves are able to travel though the Earth's inner layers, they areused by scientists to study the Earth's interior.5. Love waves cause the most damage to structures during an earthquake.
My Answer:
1. False
2. False
3. True
4. False
5. True
Explanation:
1. The energy of Seismic Waves radiates outward from the fault in all directions.
2. Surface Waves travel along the Earth's surface.
3. Two examples of surface waves are Rayleigh waves and Love waves.
4. Body waves can travel through the earth's inner layers, but surface waves can only move along the surface of the planet like ripples on water.
5. Out of the two types of surface waves, the L-waves (Love waves) are the most destructive. They can literally move the ground beneath a building faster than the building itself can respond, effectively shearing the base off of the rest of the building.
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