lab 7 volcanos Emaglai St Maina kea and whata Use these map.pdf
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lab 7 volcanos Emaglai St Maina kea and whata Use these maps to answer the following questions. Which rwo voleanoef inclode nonss whe the hyther riak of hamards from lava flows (zone 1)? Which voicano has the loasest risk of tararth from fova toves? Which volcano dominates the luva haand rooe map, by corering the laggest ares? Mauna Loa Describe she 2018 cruption, and caplain boe for oot) accuate these mops were for ptedicting th high nsk areas.Why afe the lava harard zoan uneveo in whupe, fakes than beang conceneric amownd the veer of the wotcano? eruporans an Hauati?The second jart of the ewertise concerna the 1990 wrwetgan of Mount Se. Helens. You woun th Fart 2 Me.sit Ileleta morkarg whth satebate imagen ef the arva frisen. Spend some time reading the test and leokine at all the different maps, photos and satelitite map. On the satelite inagos, what colors represent the following features? Vegetation Water lce and snow Ash and mudUsing the map above and/or the satellite image from 1983, estimate the sine of the area of forest (in sq, miles) devastated by the May 18. 1960 eruption. (show your working) Describe what happened to Spirit lake as a result of the eruption. fUSE rour OWN WORDS) What changos, identified in the 1963, 19e8, 1992 and 1999 sateuilie images and on the current Google Earth image, indicate that the area is recovering from the 1980 ervption?Name least 5mm m? unaffected by ash deposits? Using Google Farth, find and name 3 echer miqhbering wolcanoes in the Cascade Fange chat have the potential to crupt like Mout Solet kleiens.Use your answets and graphs from today's lab to write your report. Titie - Brief, but descriptive. Introduction - Hriefly introduce volcanie hamards and the 2 volcanoes you shudied is detail. What is the purpose of the lab exercise? Method What information did your obtain from the maps and images? How did you use that data to assess past damage and future risk from these volcanoes? Results - What types of hatard does each volcano present? How are they similar, and how do they differ? How large are the areas affected or potentially affected by these hazands? Discussion - Discuss the relationships betweeh magma type and hatard for each volcano. How does the location of each volcano affect the nature of the eruption and the type and sitie of hamard? Conclusions - Brief summary of your findings:.
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MODULE 1.pptx
The document discusses plate tectonics and provides examples of activities to help students understand the theory. It begins by introducing the three main types of plate boundaries: divergent boundaries where plates move apart, convergent boundaries where they move together, and transform boundaries where they slide past each other. Later activities illustrate how convergent boundaries between oceanic and continental plates can result in subduction and volcanic island arcs. They also explain how the Philippines' geology has been shaped by the collision and subduction of tectonic plates over millions of years.
INFORMATIVE OUTLINE – REQUIRED OUTLINESPECIFIC PURPOSEC.docx
INFORMATIVE OUTLINE – REQUIRED OUTLINE
SPECIFIC PURPOSE:
CENTRAL IDEA/THESIS:
INTRODUCTION:
1. GET ATTENTION:
2. CLEARLY REVEAL TOPIC:
3. LISTENER RELEVANCE:
4. ESTABLISH CREDIBILITY:
5. PREVIEW MAIN POINTS:
Transition:
BODY:
I. MAIN POINT
A. Sub-point
1. Sub-sub point
2.
B.
Transition/Connective:
II.
A.
B.
Transition/Connective:
III.
A.
B.
Signal End:
CONCLUSION:
1. RESTATE CENTRAL IDEA:
2. REVIEW MAIN POINTS:
3. CLINCHER:
BIBLIOGRAPHY
1
LAB MODULE 12: INTERNAL STRUCTURE OF THE EARTH
Note: Please refer to the GETTING STARTED lab module to learn tips on how to set up and
maneuver through the Google Earth ( ) component of this lab.
KEY TERMS
The following is a list of important words and concepts used in this lab module:
Asthenosphere Extrusive igneous Metamorphic rocks
Chemically precipitated sedimentary
rocks
Geologic time scale Organic sedimentary
Cinder cone volcanoes Igneous rocks Rock cycle
Clastic sedimentary Intrusive igneous Sedimentary rocks
Composite Volcanoes Lithification Seismic waves
Core Lithosphere Shield Volcanoes
Crust Mantle
LAB MODULE LEARNING OBJECTIVES
After successfully completing this module, you should be able to:
Recognize and interpret the spatial patterns of volcanoes and volcanic activity at the
global scale
Identify and characterize different rock types
Define the process of lithification
Recognize and differentiate the various internal layers of the Earth
Distinguish and describe the different types of volcanoes
Outline and explain the rock cycle
Interpret the topographic profile of a landscape
2
INTRODUCTION
In this lab module, you will examine some of the fundamental concepts and principles related
to the internal structure of the Earth. Topics include rock types, the rock cycle, geologic time
and volcanoes. While these topics may seem disparate, you will learn how they are inherently
related.
The module starts with four opening topics, or vignettes, which are found in the accompanying
Google Earth file. These vignettes introduce basic concepts related to Earth’s internal structure.
Some of the vignettes have animations, videos, or short articles that provide another
perspective or visual explanation for the topic at hand. After reading each vignette and
associated links, answer the following questions. Please note that some components of this lab
may take a while to download or open, especially if you have a slow internet connection.
Expand INTERNAL STRUCTURE, and then expand the INTRODUCTION folder. Double-click
Topic 1: The Earth’s Internal Composition.
Read Topic 1: The Earth’s Internal Composition
Question 1: What is the depth of the Kola borehole as a percentage of the Earth’s
radius? Calculate using the following equation:
A. (123km / 637km) * 100 = 19.3%
B. (123km / 6370km) * 100 = 1.93%
C. (12.3km / 637km) * 100 = 1.93%
D. (12.3km / 6370km) * 10 ...
1 LAB MODULE 12 INTERNAL STRUCTURE OF THE EARTH .docx
1
LAB MODULE 12: INTERNAL STRUCTURE OF THE EARTH
Note: Please refer to the GETTING STARTED lab module to learn tips on how to set up and
maneuver through the Google Earth ( ) component of this lab.
KEY TERMS
The following is a list of important words and concepts used in this lab module:
Asthenosphere Extrusive igneous Metamorphic rocks
Chemically precipitated sedimentary
rocks
Geologic time scale Organic sedimentary
Cinder cone volcanoes Igneous rocks Rock cycle
Clastic sedimentary Intrusive igneous Sedimentary rocks
Composite Volcanoes Lithification Seismic waves
Core Lithosphere Shield Volcanoes
Crust Mantle
LAB MODULE LEARNING OBJECTIVES
After successfully completing this module, you should be able to:
Recognize and interpret the spatial patterns of volcanoes and volcanic activity at the
global scale
Identify and characterize different rock types
Define the process of lithification
Recognize and differentiate the various internal layers of the Earth
Distinguish and describe the different types of volcanoes
Outline and explain the rock cycle
Interpret the topographic profile of a landscape
2
INTRODUCTION
In this lab module, you will examine some of the fundamental concepts and principles related
to the internal structure of the Earth. Topics include rock types, the rock cycle, geologic time
and volcanoes. While these topics may seem disparate, you will learn how they are inherently
related.
The module starts with four opening topics, or vignettes, which are found in the accompanying
Google Earth file. These vignettes introduce basic concepts related to Earth’s internal structure.
Some of the vignettes have animations, videos, or short articles that provide another
perspective or visual explanation for the topic at hand. After reading each vignette and
associated links, answer the following questions. Please note that some components of this lab
may take a while to download or open, especially if you have a slow internet connection.
Expand INTERNAL STRUCTURE, and then expand the INTRODUCTION folder. Double-click
Topic 1: The Earth’s Internal Composition.
Read Topic 1: The Earth’s Internal Composition
Question 1: What is the depth of the Kola borehole as a percentage of the Earth’s
radius? Calculate using the following equation:
A. (123km / 637km) * 100 = 19.3%
B. (123km / 6370km) * 100 = 1.93%
C. (12.3km / 637km) * 100 = 1.93%
D. (12.3km / 6370km) * 100 = 0.193%
Read Topic 2: Rock Types
Question 2: What are alternative terms used in place of “extrusive” and “intrusive”
igneous rock?
A. Magma and granite
B. Pumice and lava
C. Volcanic and plutonic
D. Vesicular and plutonic
3
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Question 3: During the Devonian Period, where is North America located relative to the
Equator? (Hint: Go to “Close-up: Phanerozoic Eon,” then click on Devonian in the time
scale image)
A. Predomi ...
04VolcanicRelief.ppt
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7.31
Seattle, Washington, with Mount Rainier in the background. (Photo by Ken Straiton/Corbis)
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Until recently the dominant view of Western societies was that humans possess the wherewithal to subdue volcanoes and other types of catastrophic natural hazards. Today it is apparent that volcanoes are not only very destructive but unpredictable as well. With this awareness, a new attitude is developing—"How do we live with volcanoes?"
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Volcanoes produce a wide variety of potential hazards that can kill people and wildlife, as well as destroy property (figure 7.32). Perhaps the greatest threats to life are pyroclastic flows. These hot mixtures of gas, ash, and pumice that sometimes exceed 800°C race down the flanks of volcanoes, giving people little chance to escape.
Lahars, which can occur even when a volcano is quiet, are perhaps the next most dangerous volcanic hazard (figure 7.33). These mixtures of volcanic debris and water can flow for tens of kilometers down steep volcanic slopes at speeds that may exceed 100 kilometers (60 miles) per hour. Lahars pose a potential threat to many communities downstream from glacier-clad volcanoes such as Mount Rainier. Other potentially destructive mass-wasting events include the rapid collapse of the volcano's summit or flank.
Other obvious hazards include explosive eruptions that can endanger people and property hundreds of miles from a
Eruption cloud
Prevailing wind
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2009 steam and ash cloud
(
figure
7.33
Soufriere Hills volcano on the Caribbean island of Montserrat has been active since 1995. A pyroclastic flow destroyed the airport and the capital city, Plymouth. About two thirds of the population have left the island. (NASA Photo)
) (
Lava dome collapse
Pyroclastic flow
) (
Fumaroles
Lava flow
Lahar (mud or debris flow)
figure
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2
Simplified drawing showing a wide variety of natural hazards associated with volcanoes. (After U.S. Geological Survey)
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3) The movement of tectonic plates causes earthquakes, creates volcanoes at plate boundaries, and results in the formation of mountain ranges.
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Recommended
MODULE 1.pptx
The document discusses plate tectonics and provides examples of activities to help students understand the theory. It begins by introducing the three main types of plate boundaries: divergent boundaries where plates move apart, convergent boundaries where they move together, and transform boundaries where they slide past each other. Later activities illustrate how convergent boundaries between oceanic and continental plates can result in subduction and volcanic island arcs. They also explain how the Philippines' geology has been shaped by the collision and subduction of tectonic plates over millions of years.
INFORMATIVE OUTLINE – REQUIRED OUTLINESPECIFIC PURPOSEC.docx
INFORMATIVE OUTLINE – REQUIRED OUTLINE
SPECIFIC PURPOSE:
CENTRAL IDEA/THESIS:
INTRODUCTION:
1. GET ATTENTION:
2. CLEARLY REVEAL TOPIC:
3. LISTENER RELEVANCE:
4. ESTABLISH CREDIBILITY:
5. PREVIEW MAIN POINTS:
Transition:
BODY:
I. MAIN POINT
A. Sub-point
1. Sub-sub point
2.
B.
Transition/Connective:
II.
A.
B.
Transition/Connective:
III.
A.
B.
Signal End:
CONCLUSION:
1. RESTATE CENTRAL IDEA:
2. REVIEW MAIN POINTS:
3. CLINCHER:
BIBLIOGRAPHY
1
LAB MODULE 12: INTERNAL STRUCTURE OF THE EARTH
Note: Please refer to the GETTING STARTED lab module to learn tips on how to set up and
maneuver through the Google Earth ( ) component of this lab.
KEY TERMS
The following is a list of important words and concepts used in this lab module:
Asthenosphere Extrusive igneous Metamorphic rocks
Chemically precipitated sedimentary
rocks
Geologic time scale Organic sedimentary
Cinder cone volcanoes Igneous rocks Rock cycle
Clastic sedimentary Intrusive igneous Sedimentary rocks
Composite Volcanoes Lithification Seismic waves
Core Lithosphere Shield Volcanoes
Crust Mantle
LAB MODULE LEARNING OBJECTIVES
After successfully completing this module, you should be able to:
Recognize and interpret the spatial patterns of volcanoes and volcanic activity at the
global scale
Identify and characterize different rock types
Define the process of lithification
Recognize and differentiate the various internal layers of the Earth
Distinguish and describe the different types of volcanoes
Outline and explain the rock cycle
Interpret the topographic profile of a landscape
2
INTRODUCTION
In this lab module, you will examine some of the fundamental concepts and principles related
to the internal structure of the Earth. Topics include rock types, the rock cycle, geologic time
and volcanoes. While these topics may seem disparate, you will learn how they are inherently
related.
The module starts with four opening topics, or vignettes, which are found in the accompanying
Google Earth file. These vignettes introduce basic concepts related to Earth’s internal structure.
Some of the vignettes have animations, videos, or short articles that provide another
perspective or visual explanation for the topic at hand. After reading each vignette and
associated links, answer the following questions. Please note that some components of this lab
may take a while to download or open, especially if you have a slow internet connection.
Expand INTERNAL STRUCTURE, and then expand the INTRODUCTION folder. Double-click
Topic 1: The Earth’s Internal Composition.
Read Topic 1: The Earth’s Internal Composition
Question 1: What is the depth of the Kola borehole as a percentage of the Earth’s
radius? Calculate using the following equation:
A. (123km / 637km) * 100 = 19.3%
B. (123km / 6370km) * 100 = 1.93%
C. (12.3km / 637km) * 100 = 1.93%
D. (12.3km / 6370km) * 10 ...
1 LAB MODULE 12 INTERNAL STRUCTURE OF THE EARTH .docx
1
LAB MODULE 12: INTERNAL STRUCTURE OF THE EARTH
Note: Please refer to the GETTING STARTED lab module to learn tips on how to set up and
maneuver through the Google Earth ( ) component of this lab.
KEY TERMS
The following is a list of important words and concepts used in this lab module:
Asthenosphere Extrusive igneous Metamorphic rocks
Chemically precipitated sedimentary
rocks
Geologic time scale Organic sedimentary
Cinder cone volcanoes Igneous rocks Rock cycle
Clastic sedimentary Intrusive igneous Sedimentary rocks
Composite Volcanoes Lithification Seismic waves
Core Lithosphere Shield Volcanoes
Crust Mantle
LAB MODULE LEARNING OBJECTIVES
After successfully completing this module, you should be able to:
Recognize and interpret the spatial patterns of volcanoes and volcanic activity at the
global scale
Identify and characterize different rock types
Define the process of lithification
Recognize and differentiate the various internal layers of the Earth
Distinguish and describe the different types of volcanoes
Outline and explain the rock cycle
Interpret the topographic profile of a landscape
2
INTRODUCTION
In this lab module, you will examine some of the fundamental concepts and principles related
to the internal structure of the Earth. Topics include rock types, the rock cycle, geologic time
and volcanoes. While these topics may seem disparate, you will learn how they are inherently
related.
The module starts with four opening topics, or vignettes, which are found in the accompanying
Google Earth file. These vignettes introduce basic concepts related to Earth’s internal structure.
Some of the vignettes have animations, videos, or short articles that provide another
perspective or visual explanation for the topic at hand. After reading each vignette and
associated links, answer the following questions. Please note that some components of this lab
may take a while to download or open, especially if you have a slow internet connection.
Expand INTERNAL STRUCTURE, and then expand the INTRODUCTION folder. Double-click
Topic 1: The Earth’s Internal Composition.
Read Topic 1: The Earth’s Internal Composition
Question 1: What is the depth of the Kola borehole as a percentage of the Earth’s
radius? Calculate using the following equation:
A. (123km / 637km) * 100 = 19.3%
B. (123km / 6370km) * 100 = 1.93%
C. (12.3km / 637km) * 100 = 1.93%
D. (12.3km / 6370km) * 100 = 0.193%
Read Topic 2: Rock Types
Question 2: What are alternative terms used in place of “extrusive” and “intrusive”
igneous rock?
A. Magma and granite
B. Pumice and lava
C. Volcanic and plutonic
D. Vesicular and plutonic
3
Read Topic 3: Geologic Time
Question 3: During the Devonian Period, where is North America located relative to the
Equator? (Hint: Go to “Close-up: Phanerozoic Eon,” then click on Devonian in the time
scale image)
A. Predomi ...
04VolcanicRelief.ppt
Volcanoes commonly occur in belts or clusters at plate boundaries. Forecasting volcanic eruptions involves assessing the character and timing based on the volcano's historic eruptions and measuring parameters like seismic activity, ground deformation, and gas emissions. Determining the timing of eruptions depends on monitoring these precursory signals.
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252 CHAPTER 8 Geologic Time
(
232
chapter 7
Fires Within: Igneous Activity
figure
7.31
Seattle, Washington, with Mount Rainier in the background. (Photo by Ken Straiton/Corbis)
)
Until recently the dominant view of Western societies was that humans possess the wherewithal to subdue volcanoes and other types of catastrophic natural hazards. Today it is apparent that volcanoes are not only very destructive but unpredictable as well. With this awareness, a new attitude is developing—"How do we live with volcanoes?"
Volcanic Hazards
Volcanoes produce a wide variety of potential hazards that can kill people and wildlife, as well as destroy property (figure 7.32). Perhaps the greatest threats to life are pyroclastic flows. These hot mixtures of gas, ash, and pumice that sometimes exceed 800°C race down the flanks of volcanoes, giving people little chance to escape.
Lahars, which can occur even when a volcano is quiet, are perhaps the next most dangerous volcanic hazard (figure 7.33). These mixtures of volcanic debris and water can flow for tens of kilometers down steep volcanic slopes at speeds that may exceed 100 kilometers (60 miles) per hour. Lahars pose a potential threat to many communities downstream from glacier-clad volcanoes such as Mount Rainier. Other potentially destructive mass-wasting events include the rapid collapse of the volcano's summit or flank.
Other obvious hazards include explosive eruptions that can endanger people and property hundreds of miles from a
Eruption cloud
Prevailing wind
Ash fall
2009 steam and ash cloud
(
figure
7.33
Soufriere Hills volcano on the Caribbean island of Montserrat has been active since 1995. A pyroclastic flow destroyed the airport and the capital city, Plymouth. About two thirds of the population have left the island. (NASA Photo)
) (
Lava dome collapse
Pyroclastic flow
) (
Fumaroles
Lava flow
Lahar (mud or debris flow)
figure
7.3
2
Simplified drawing showing a wide variety of natural hazards associated with volcanoes. (After U.S. Geological Survey)
)
Acid rain
Pyroclastic flow
Jf^- Eruption column
Bombs Collapse of flank Lava dome
(
The Chapter in Review
233
figure
7.34
Monitoring South Sister Volcano, Cascade Range, Oregon. This geologist is measuring the degree of infla
tion of the volcano's surface for potential eruptive activity.
)
volcano. During the past 15 years at least 80 commercial jets have been damaged by inadvertently flying into clouds of volcanic ash (Figure 7.33). One of these was a near crash that occurred in 1989 when a Boeing 747, with more than 300 passengers aboard, encountered an ash cloud from Alaska's Redoubt volcano. All four engines stalled after they became clogged with ash. Fortunately, the engines were restarted at the last minute and the aircraft managed to land safely in Anchorage.
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Today a number of volcano-monitoring techniques are employed, with most of them aimed at detec.
1. Volcanoes, Earthquakes, and Mountain Ranges.pdf
1) Earthquakes, volcanoes, and mountain ranges are distributed in patterns related to plate tectonic theory.
2) Most earthquake epicenters and volcanoes are located near plate boundaries like the "Ring of Fire" in the Pacific.
3) The movement of tectonic plates causes earthquakes, creates volcanoes at plate boundaries, and results in the formation of mountain ranges.
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The document discusses techniques seismologists use to predict earthquakes, including satellite imagery, infrared radiation, and interferometric synthetic aperture radar. It analyzes the 10 areas most overdue for earthquakes based on historical seismic activity and few quakes occurring in 2010. These areas include California, Alaska, Guatemala, Chile/Peru, Turkey, Burma/China, Japan, the Philippines, Afghanistan, and Mongolia. Seismologists study where large quakes have previously struck and use new technologies to detect ground movements and hot spots that could signal future seismic activity.
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Question 1
Recall from your reading about the nature of volcanoes to choose the best answer: Magma tends to rise toward Earth's surface principally because __________.
of convection in the mantle
of magma cooling
mounting pressure within the reservoir
rocks become more dense when they melt
Question 2
Recall from your reading about the nature of volcanoes to choose the best answer: Which type of basaltic lava flow has a fairly smooth, unfragmented, ropy surface?
Scoria
Aa
Pahoehoe
Pumice
Question 3
Refer to the following relative time scale diagram to answer the question: which of the following represents the longest subdivision of the geologic time?
Mississippian
Precambrian
Eocene
Carboniferous
Question 4
Recall from your reading about the nature of volcanoes to choose the best answer: A volcanic eruption is driven by __________ and __________ which forces its way upward and may ultimately break though zones of weaknesses in the Earth's crust.
buoyancy; water pressure
heat; water pressure
heat; gas pressure
buoyancy; gas pressure
Question 5
Recall from your reading about the relative time scale and refer to the following diagram of a composite geologic section to answer the question. Which of the following is the oldest rock layer observed in the diagram?
Bright Angel shale
Hermit Shale
Tapeats Sandstone
Kaibab limestone
Question 6
· Recall your reading of Relative Time Scale and Radiometric Time Scale and match the term with the definition.
Isotopes
Half-life
Carbon 14
Igneous rocks
Hutton
Petrology
Index fossil
Stratigraphy
A.
Isotope found in all living plants and animals
B.
Atoms of the same element with differing atomic weights
C.
The Scottish geologist who first proposed the fundamental principle used to classify rocks according to their relative ages
D.
Studies on the origins of the various kinds of rocks
E.
The time it takes for one-half of a particular radioactive isotope in a sample to decay
F.
Studies of rock layering
G.
Forms of life which existed during limited periods of geologic time and thus are used as guides to the age of the rocks in which they are preserved
H.
Rocks that generally do not contain fossils
Question 7
· Recall from your reading of Principal Types of Volcanoes, and match the description to the type of volcano.
Large, fairly steep-sided cones composed of alternating layers of lava flows and pyroclastic material.
Small basaltic cones built during one, short, eruptive episode; dominated by cinders.
Volcanoes of southwestern Alaska and the Aleutian Islands.
Big volcanoes of Hawaii
Volcano Paricutin in Mexico
Forms dikes from lava
Lava is produced after the eruption and flows from the bottom
Volcanoes with gentle slopes spreading over large areas
A.
Cinder cones
B.
Composite/stratovolcanoes
C.
Shield volcanoes
Question 8
· Recall from your reading about the radiometric time scale to put the following isotopes in order of use, from oldest rock to youngest.
Ca ...
3
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3. While some attempts have been made to control lava flows, volcanic eruptions cannot fully be controlled. The most effective approaches are hazard mapping, land use planning, education and preparedness activities to reduce vulnerability and respond to eruptions.
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The document summarizes information about earthquakes and volcanoes. It discusses what causes earthquakes, provides examples of major earthquakes including photos, and describes effects like ground shaking, surface faulting, liquefaction, landslides, fires, and tsunamis. It also defines what a volcano is, describes the different parts of a volcano, classifies the main types of volcanoes, and explains volcanic eruptions and their products. Safety tips are also mentioned. Maps of fault zones in the Philippines are presented.
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Prompt:
What is the goal of education? How successful is America’s educational system at achieving that goal for all of this nation’s children? Examine these questions through two in-class texts and one outside source.
Assignment Requirements:
1. You must have a clearly defined main point (thesis). The purpose of the paper is not to tell a story. Rather, use the readings and your analysis to prove a point or argue an idea.
2. For this paper you must examine the ideas of two readings from this unit and one outside source.
a. In-class readings: The authors all write about the education in some manner. You will choose two writers who help you address your thesis.
b. Outside source: A source not discussed in class that portrays or examines education. Consider consulting:
i. the media (movies, television, advertisements, etc.).
ii. magazines or newspaper articles
iii. appropriate internet sites
iv. journals (available through the library’s website)
3. You must include a minimum of six quotes from your sources, but make sure these references are relevant to your essay. Be sure to give distinctive details, descriptions, explanations, etc.
4. You must write about an issue, an idea, and not primarily about your personal experiences.
a. You may draw on personal knowledge to exemplify a point—indeed, that can be wonderful and effective‐‐, but your personal story should not take up the bulk of your essay.
5. Your paper should be five to eight pages typed, double spaced, 12 pt. Times New Roman font and have one inch margins all the way around. Your essay must also have an original title.
6. You must use MLA format/conventions for in- text citations and work cited page.
7. All final drafts of essays must be submitted onto turnitin.com by the due date. A printed copy of the essay must also be given to the instructor in class on the day due.
IN CLASS READING:
“Still Unequal, Still Separate” by Jonathan Kozol
“Report of the Massachusetts Board of Education” by Horace Mann
6 Quotations in total.
OUTSIDE SOURCE:
http://www.nytimes.com/roomfordebate/2015/05/04/is-testing-students-the-answer-to-americas-education-woes
Geology
doi: 10.1130/G31017.1
2010;38;1067-1070Geology
G.C. Koteas, M.L. Williams, S.J. Seaman and G. Dumond
Granite genesis and mafic-felsic magma interaction in the lower crust
Email alerting services
articles cite this article
to receive free e-mail alerts when newwww.gsapubs.org/cgi/alertsclick
Subscribe to subscribe to Geologywww.gsapubs.org/subscriptions/click
Permission request to contact GSAhttp://www.geosociety.org/pubs/copyrt.htm#gsaclick
official positions of the Society.
citizenship, gender, religion, or political viewpoint. Opinions presented in this publication do not reflect
presentation of diverse opinions and positions by scientists worldwide, regardless of their race,
includes a reference to the article's full citation. GSA provides this and other forums for the
the abstracts only ...
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The document discusses the biological effects of several types of natural explosions:
1) The Big Bang created the universe 15 billion years ago from a single point containing all matter and energy.
2) Hypernova explosions emit gamma rays that have the potential to cause global environmental changes and damage life through ionizing radiation.
3) Large volcanic eruptions can devastate landscapes and communities through pyroclastic flows, ash falls, and lahars, in addition to changing global climate.
Earthquakes.pptx
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Lesson 1 describes earthquakes and faults. It defines key terms like fault, focus, and epicenter. Faults occur along breaks in the earth's crust where significant movement has taken place. There are two main types of faults: dip-slip faults which involve vertical movement, and strike-slip faults which involve horizontal movement. The focus is where an earthquake originates within the fault plane, while the epicenter is the point directly above on the surface. The lesson provides safety tips for before, during, and after an earthquake occurs.
Living in an Active Zone Revision
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Secrets in the Solar System preview
Preview of full presentation about anomalies in the solar system which NASA won't talk much about.
Links:
This presentation will be on http://www.checktheevidence.com/
Slide 002
http://ida.wr.usgs.gov/html/m15012/m1501228.html
Slide 003
http://web.archive.org/web/20090511150126/http:/hirise.lpl.arizona.edu/PSP_007230_2170
Slide 004
http://hirise.lpl.arizona.edu/PSP_007230_2170
Slide 005
http://hirise.lpl.arizona.edu/PSP_007230_2170
http://hirise.lpl.arizona.edu/
Slide 006
http://hirise.lpl.arizona.edu/PSP_007230_2170
Slide 007
http://hirise.lpl.arizona.edu/PSP_007230_2170
Slide 014
http://www.shultslaboratories.com/SL2D004.htm
http://www.shultslaboratories.com/SL2D007.htm
Slide 015
http://marsrovers.jpl.nasa.gov/gallery/all/1/m/443/1M167510798EFF55B0P2956M2M1.JPG
Slide 018
http://hirise.lpl.arizona.edu/PSP_007230_2170
Slide 020
http://news.bbc.co.uk/1/hi/sci/tech/3387903.stm
Slide 021
http://www.aulis.com/mars.htm
Slide 023
http://photojournal.jpl.nasa.gov/catalog/PIA10369
http://hirise.lpl.arizona.edu/phobos.php
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defined:Given the classes above, what output is produced by the following code? (Since the code
loops over the elements of an array of objects, write the output produced as the loop passes over
each element of the array separately.) Arya[] thrones ={ new Oberyn(), new Arya(), new Brienne(),
new Tyrion() }; for (int i=0;i< thrones.length; i++){ thrones[i].a(): System, out.printin(); System.
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inventory. What is Landow's income under absorption costing?.
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Question 1
Recall from your reading about the nature of volcanoes to choose the best answer: Magma tends to rise toward Earth's surface principally because __________.
of convection in the mantle
of magma cooling
mounting pressure within the reservoir
rocks become more dense when they melt
Question 2
Recall from your reading about the nature of volcanoes to choose the best answer: Which type of basaltic lava flow has a fairly smooth, unfragmented, ropy surface?
Scoria
Aa
Pahoehoe
Pumice
Question 3
Refer to the following relative time scale diagram to answer the question: which of the following represents the longest subdivision of the geologic time?
Mississippian
Precambrian
Eocene
Carboniferous
Question 4
Recall from your reading about the nature of volcanoes to choose the best answer: A volcanic eruption is driven by __________ and __________ which forces its way upward and may ultimately break though zones of weaknesses in the Earth's crust.
buoyancy; water pressure
heat; water pressure
heat; gas pressure
buoyancy; gas pressure
Question 5
Recall from your reading about the relative time scale and refer to the following diagram of a composite geologic section to answer the question. Which of the following is the oldest rock layer observed in the diagram?
Bright Angel shale
Hermit Shale
Tapeats Sandstone
Kaibab limestone
Question 6
· Recall your reading of Relative Time Scale and Radiometric Time Scale and match the term with the definition.
Isotopes
Half-life
Carbon 14
Igneous rocks
Hutton
Petrology
Index fossil
Stratigraphy
A.
Isotope found in all living plants and animals
B.
Atoms of the same element with differing atomic weights
C.
The Scottish geologist who first proposed the fundamental principle used to classify rocks according to their relative ages
D.
Studies on the origins of the various kinds of rocks
E.
The time it takes for one-half of a particular radioactive isotope in a sample to decay
F.
Studies of rock layering
G.
Forms of life which existed during limited periods of geologic time and thus are used as guides to the age of the rocks in which they are preserved
H.
Rocks that generally do not contain fossils
Question 7
· Recall from your reading of Principal Types of Volcanoes, and match the description to the type of volcano.
Large, fairly steep-sided cones composed of alternating layers of lava flows and pyroclastic material.
Small basaltic cones built during one, short, eruptive episode; dominated by cinders.
Volcanoes of southwestern Alaska and the Aleutian Islands.
Big volcanoes of Hawaii
Volcano Paricutin in Mexico
Forms dikes from lava
Lava is produced after the eruption and flows from the bottom
Volcanoes with gentle slopes spreading over large areas
A.
Cinder cones
B.
Composite/stratovolcanoes
C.
Shield volcanoes
Question 8
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6. You must use MLA format/conventions for in- text citations and work cited page.
7. All final drafts of essays must be submitted onto turnitin.com by the due date. A printed copy of the essay must also be given to the instructor in class on the day due.
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“Report of the Massachusetts Board of Education” by Horace Mann
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Email alerting services
articles cite this article
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Subscribe to subscribe to Geologywww.gsapubs.org/subscriptions/click
Permission request to contact GSAhttp://www.geosociety.org/pubs/copyrt.htm#gsaclick
official positions of the Society.
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divorced several years ago, Wanda was awarded custody of their two children, Penny and Kyle.
(Note: Wanda has never issued a Form 8332 waiver.) Under the divorce decree, John was
obligated to pay alimony and child support - the alimony payments were to terminate if Wanda
remarried.In July, while going to lunch in downtown Santa Fe, Wanda was injured by a tour bus.
Because the driver was clearly at fault, the owner of the bus, Roadrunner Touring Company, paid
her medical expenses (including a one-week stay in a hospital). To avoid a lawsuit, Roadrunner
also transferred $90,000 to her in settlement of the personal injuries she sustained.Medical
expenses, not covered by insurance. 7,200 dollars. Taxes. Property taxes on personal residence
3,600 dollars. State of New Mexico income tax, includes amount withheld from wages during
2018. 4,200 dollars. Total 7,800 dollars. Interest on home mortgage, first National Bank. 6,000
dollars. Charitable contributions. 3,600 dollars. Life insurance premiums, policy on Lance's life.
1,200 dollars. Contributions to traditional IRA, on Wanda's behalf. 5,000 dollars. Traffic fines. 300
dollars. Contribution to the reelection campaign fund of the mayor of Santa Fe. 500 dollars.
Funeral expenses for Wayne Boyle. 6,300 dollars. The life insurance policy was taken out by
Lance several years ago and designates Wanda as the beneficiary. As a part-time employee,
Wanda is exeluded from coverage under her employer's pension plan. Consequently, she
provides for her own retirement with a traditional IRA obtained at a local trust company. Because
the mayor is a member of the local Chamber of Commerce, Lance felt compelled to make the
political contribution.The Deans' household includes the following, for whom they provide more
than half of the support:Penny graduated from high school on May 9, 2021, and is undecided
about college. During 2021, she earned $8,500 (placed in a savings account) playing a harp in the
lobby of a local hotel. Wayne is Wanda's widower father who died on December 20 , 2021. For the
past few years, Wayne qualified as a dependent of the Deans. Federal incont tax wit.
Lakevicw Propertess is eraluating a real extato inventment o.pdf
Lakevicw Propertess is eraluating a real extato inventment of Seabreezo Estatos Management
plans to biy the properfy lodis and seff it 8 rears from today. The intal cost of the property a 510
milion and ne expeded salo price is $14 malion. What is the IRR of the investrient? Eater your
answor as a porcentage. and rounded to 2 OECMAL, PLACES Do not includo the percentage nog
in your answet Entar your response bolow.
Lake Shore Medical Center wants to keep track of all adminis.pdf
Lake Shore Medical Center wants to keep track of all
administrative appointments, including dates of appointment
and dates of termination (Hint: Time-variant data is at work).
The Medical Center administrator may want to know how
many department directors worked in each of the seven
departments between January 1, 1965, and December 31,
2021, and who was the IT Director in 2015. Given this
information, create the complete ERD that contains all primary
keys, foreign keys, and main attributes..
label the following structures if they are visible on the im.pdf
label the following structures if they are visible on the image. Please label both images using lines
or arrows. thank you
Primordial follicle
Primary unilaminar follicle
Primary multilaminar follicle
Primary oocytes
Follicular cells
Secondary oocyte, mature oocyte (metaphase 2)
Oocyte Nucleus
Zona pelucida
Mature or Graafian follicle
Interstitial cells
Blood vessels.
Lab8 Controlling traffic using Extended ACL Objectives Per.pdf
Lab8 Controlling traffic using Extended ACL
Objectives
Perform basic configuration tasks on a router.
Applying Static routes and default route.
Exploring the routing table entry.
Applying Extended (named) access control lists (ACLs).
Testing the access control lists (ACLs).
Required Resources
2 Cisco Routers (1841)
2 Cisco Switches (2950-24)
3 Computers
UTP (straight through and cross over) cables
Tasks:
A. Build up the topology.
B. Perform Basic Router Configurations
Steps:
1. Connect the components as shown in Fig 1.
2. Configure the router hostname to match the topology diagram.
3. Configure IP addresses and masks on all devices.
4. Configure a loopback interface (loopback 0) on R2 to simulate the ISP. (search on the internet
how to configure loopback interface)
C. Enable Static route for all networks.
Steps:
1. For Router 1
R1(config)# ip route 192.168.20.0 255.255.255.0 serial 0/0/0
Default root can be configured as:
R1(config)# ip route 0.0.0.0 0.0.0.0 10.1.1.2
2. For Router 2
R2(config)# ip route 192.168.10.0 255.255.255.0 serial 0/0/1
R2(config)# ip route 192.168.11.0 255.255.255.0 serial 0/0/1
D. Verify full IP connectivity using the ping command and the routing table of routers.
Step#1:
For R1 and R2, use the command show ip route, take a snapshot for the resulting routing table,
and discuss the outputs:
*Routing table of R1(Screenshoot)
*Routing table of R2 (Screenshot)
Step#2:
Make sure that the whole network nodes can ping each other.
Before configuring and applying this ACL, be sure to test connectivity from Laptop1 to the
loopback interface (ISP - 209.165.200.225)
E. Configuring an Extended ACL
In this section, you are configuring an extended ACL on R1 that blocks traffic originating from any
device on the 192.168.10.0/24 network to access the 209.165.200.255 host (the simulated ISP).
This ACL will be applied outbound on the R1 Serial 0/0/0 interface.
Steps:
1. Configure a named extended ACL.
R1(config)#ip access-list extended EXTEND-1
R1(config-ext-nacl)#deny ip 192.168.10.0 0.0.0.255 host 209.165.200.225
2. Apply the ACL.
With standard ACLs, the best practice is to place the ACL as close to the destination as possible.
Extended ACLs are typically placed close to the source.
R1(config)#interface serial 0/0/0
R1(config-if)#ip access-group EXTEND-1 out
3. Test the ACL.
From Laptop1; ping the loopback interface on R2.
R1(config-ext-nacl)#permit ip any any
**Please provide full code and screenshoots from Cisco packet tracer.
Table -1 begin{tabular}{|c|ccc|} hline Device & Interface & IP Address & Default Gateway & & & R1
& Fa0/0 & 192.168.10.1/24 & N/A & Fa0/1 & 192.168.11.1/24 & N/A & So/0/0 & 10.1.1.1/24 & N/A
& Fa0/1 & 192.168.20.1/24 & N/A R2 & So/0/1 & 10.1.1.2/24 & N/A & loopback 0 &
209.165.200.225/8 & N/A & & & & & 192.168.10.10/24 & 192.168 .10 .1 hline Laptop1 & NIC &
192.168.11.10/24 & 192.168 .11 .1 hline Laptop2 & NIC & 192.168.20.254/24 & 192.168 .20 .1
hline hline PC3 & NIC & & hline end{tabular}.
Lab Task 2 Use the below code and fill it in where appropri.pdf
Lab Task 2: Use the below code and fill it in where appropriate to prompt the user to insert
numbers into the tree, display tree nodes, search the tree nodes for a number, and delete a node
from the tree. The program must show this message when it starts: Enter first letter of show,
insert, find, delete, or traverse:.
Lab Task 5 Points As a programmer in a company you were .pdf
Lab Task: (5 Points) As a programmer in a company, you were assigned to create a program that
can register employees' information and their dependents. The program should: - Register
employee information (id, name and department) - Register dependent/s for each employee - View
all records, showing the employee details and its registered dependent/s. As an initial step, the
design team draws the following class diagram to give the overview of the program. The
implementation team writes more details explaining what input and output is needed. As a part of
the implementation team, your job is to write the proper code to realize the class diagram..
La mutacin del ojo sepia se es una mutacin recesiva no l.pdf
La mutacin del ojo sepia (se) es una mutacin recesiva no letal ubicada en el cromosoma III en
Drosophila (no est ligada al sexo, el cromosoma sexual es el cromosoma I). Prediga los
resultados de un cruce monohbrido (generacin F ) con los siguientes progenitores: una mosca
2
+
hembra homocigtica de tipo salvaje y una mosca macho con ojos sepia. Use un se para el tipo
salvaje y se para la mutacin. Qu son los genotipos parentales? ________ Los genotipos F ?
1
_______ Dibuja un cuadro de Punnett para determinar las proporciones fenotpicas predichas en
la generacin F .
2.
LAB EXERCISES 1 Create a table employee with emp_noemp_n.pdf
LAB EXERCISES: 1. Create a table employee with (emp_no,emp_name, emp_address) 2. Insert
five employees information. 3. Display names of all employees. 4. Display all the employees from
'MANIPAL'. 5. Add a column named salary to employee table. 6. Assign the salary for all
employees. 7. View the structure of the table employee using describe. 8. Delete all the
employees from 'MANGALORE' 9. Rename employee as employee 1. 10. Drop the table
employeel..
La venta al por menor de prendas de vestir ha cambiado Ya n.pdf
La venta al por menor de prendas de vestir ha cambiado. Ya no existe un aspecto estndar al que
se adhieren todos los minoristas durante toda una temporada. La moda es rpida, compleja y
furiosa. Las diferentes tendencias se superponen y las ideas de moda que ni siquiera estn en la
pantalla de radar de una tienda pueden convertirse en "imprescindibles" en seis meses. Muchos
comercios minoristas con sus propias marcas, como H&M y Zara, venden productos de moda de
ltima hora a precios bajos en tiendas que estn claramente enfocadas en un mercado. En el
mundo de la moda rpida, los diseos de pasarela se abren paso rpidamente en las tiendas de la
calle a precios cualquiera.
La calidad de la prenda hace que solo dure una temporada, pero los clientes de moda rpida no
quieren las tendencias de ayer. Como dice Newsweek, "ser un comprador ms rpido" es lo que
hizo que los minoristas de moda H&M y Zara tuvieran xito. Prosperan practicando la nueva
ciencia de la "moda rpida", comprimiendo los ciclos de desarrollo de productos hasta seis veces.
Pero las operaciones minoristas que ven los clientes son solo la parte final de las cadenas de
suministro que los alimentan. Y estos tambin han cambiado.
En su nivel ms simple, la cadena de suministro de moda rpida tiene cuatro etapas. Primero se
disean las prendas, luego se fabrican. Luego se distribuyen a los puntos de venta minorista,
donde se exhiben y venden en operaciones minoristas diseadas para reflejar los valores de marca
de las empresas. En este breve caso examinamos dos operaciones de moda rpida, Hennes and
Mauritz (conocidas como H&M) y Zara, junto con United Colors of Benetton (UCB), una cadena
similar, pero con un posicionamiento de mercado diferente.
Benetton
Hace casi cincuenta aos, Luciano Benetton tom por asalto el mundo de la moda al vender los
suteres brillantes e informales (diseados por su hermana) en toda Europa (y ms tarde en el resto
del mundo), promovidos por publicidad controvertida. En 2005, el Grupo Benetton estaba
presente en 120 pases de todo el mundo. Con la venta de ropa casual, principalmente bajo United
Colors of Benetton (UCB) y sus marcas Sisley, ms orientadas a la moda, produce 110 millones de
prendas al ao, ms del 90 por ciento de ellas en Europa. Su red minorista de ms de 5000 tiendas
produce ingresos de alrededor de $ 2 mil millones. Los productos de Benetton son menos alta
costura pero de un estndar ms alto de calidad y durabilidad, con precios ms altos que H&M y
Zara.
H&M
Establecidos en Suecia en 1947, ahora venden ropa y cosmticos en ms de 1000 tiendas en 20
pases de todo el mundo. El concepto de negocio es moda y calidad al mejor precio. Con ms de 40
000 empleados e ingresos de alrededor de SEK 60 000 millones, su mayor mercado es Alemania,
seguida de Suecia y el Reino Unido. H&M es visto por muchos como el creador del concepto de
moda rpida. Ciertamente, tienen aos de experiencia en reducir el precio de la moda de ltima hora.
Aseguramos el mejor precio, dicen, al tener po.
La Universidad Johns Hopkins cometi recientemente un gran e.pdf
La Universidad Johns Hopkins cometi recientemente un gran error. Sin darse cuenta, dio la
bienvenida a 293 solicitantes rechazados al campus de Baltimore, Maryland. El correo electrnico
deca: Acepta el S! en la lnea de asunto. Bienvenidos a la Clase de 2019! No podemos esperar a
que llegues al campus. Hasta entonces, como uno de los miembros ms nuevos de la familia,
esperamos que muestre su orgullo por el arrendajo azul. Nota al pie de pgina Ese mensaje estaba
destinado a enviarse a los 3065 estudiantes que haban sido aceptados. En cambio, se dirigi a un
subconjunto de estudiantes que haban solicitado pero se les neg. David Phillips, vicerrector de
admisiones y ayuda financiera en Hopkins, culp al error humano por el error. Un subcontratista
que ayuda a la prestigiosa universidad con la comunicacin electrnica us la lista incorrecta de
direcciones de correo electrnico, explic el vicerrector. Pedimos disculpas a los estudiantes
afectados y a sus familias, dijo Phillips. Los das de decisin de admisin son lo suficientemente
estresantes. Lamentamos mucho haber contribuido a la decepcin que sinti un grupo de
estudiantes muy capaces y trabajadores, especialmente aquellos que estaban tan comprometidos
con la idea de asistir a Johns Hopkins que aplicaron la decisin anticipada. Nota a pie de pgina Un
solicitante, que ya haba recibido un rechazo de Hopkins, Sam Stephenson, estaba confundido,
dijo su madre. Qu podra hacer la universidad para corregir este desliz masivo? Para David
Phillips, vicerrector de admisiones y ayuda financiera, escriba un mensaje de malas noticias
apropiado para los estudiantes que recibieron el mensaje por error. Muchos solicitantes se
preguntarn cul es su estado real de admisin..
La transcripcin es el proceso mediante el cual la enzima _.pdf
La transcripcin es el proceso mediante el cual la enzima, ____________________ , hace una
__________________ a partir de una plantilla ______________ .
1. La traduccin es el proceso por el cual las estructuras, ____________________ , hechas de
subunidades especficas, junto con _________ ARN, forman un ________________ a partir de
una plantilla de ARN.
2. En qu extremo de una cadena de ARN en crecimiento se agregan nuevos nucletidos?.
La ventaja potencial de la dilucin de acciones es que R E.pdf
La ventaja potencial de la dilucin de acciones es que:
R. El capital recibido por la empresa despus de la dilucin puede mejorar la rentabilidad de la
empresa y el precio de sus acciones.
B. La propiedad de la empresa se vuelve ms concentrada.
C.La compaa aumentar sus pagos de dividendos a corto y mediano plazo.
D. No hay potencial alcista en la dilucin de acciones.
R. El capital recibido por la empresa despus de la dilucin puede mejorar la rentabilidad de la
empresa y el precio de sus acciones.
B. La propiedad de la empresa se vuelve ms concentrada.
C.La compaa aumentar sus pagos de dividendos a corto y mediano plazo.
D. No hay potencial alcista en la dilucin de acciones..
La transcriptasa inversa es conocida por tener poca activida.pdf
La transcriptasa inversa es conocida por tener poca actividad de revisin. Cul sera una
consecuencia de esto?
Qu dogma central de la gentica tuvo que ser revisado tras el descubrimiento de un
retrovirus y por qu?
Un medicamento antiviral modifica especficamente los receptores virales en una clula
husped eucariota. Cmo podra afectar esto al ciclo reproductivo viral?.
La teora del orden jerrquico de MyersMajluf predice que l.pdf
La teora del orden jerrquico de Myers-Majluf predice que las empresas financiarn sus proyectos
utilizando la siguiente secuencia de fuentes de financiacin:
A. Fondos internos; equidad externa; deuda segura; deuda riesgosa
B. Equidad externa; deuda segura; deuda riesgosa; fondos internos
C. Fondos internos; deuda riesgosa; deuda segura; patrimonio externo
D. Equidad externa; deuda riesgosa; deuda segura; fondos internos
E. Ninguna de las anteriores.
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Chapter-1
Introduction to objective, scope and outcome the subject
Chapter 2
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Chapter 3
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Chapter 6
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Date: May 29, 2024
Tags: Information Security, ISO/IEC 27001, ISO/IEC 42001, Artificial Intelligence, GDPR
-------------------------------------------------------------------------------
Find out more about ISO training and certification services
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