Describe the paths of water through the hydrologic cycle. Explain.docx
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Describe the paths of water through the hydrologic cycle. Explain the processes and the energy gains and losses involved in the changes of water between its 3 states. Operationally, we often most concerned with water does when it reaches the solid earth, both on the surface and in the sub-surface. Explain the relationship between the saturated zone, the water table, a ground water well and the cone of depression, all within the sub-surface. The food chain is a valuable concept in biogeography. Give an example of a specific food chain, labeling the various levels of the food chain. After looking at characteristics of food chains, explain how a geographer’s approach to the study of organisms might be different than biologist’s study of organisms; what would each try to emphasize more than the other? What exactly is a biome? Compare/contrast the concept of the biome with that of the zoogeographic region. Compare/contrast the floral characteristics of 2 of the following biomes: Desert, Tundra, Midlatitude Grassland and Boreal Forest. Theorize the difference in soil development in adjoining soils developed on forested, sloped area versus a grassed flat area. What are the soil-forming factors? Explain the importance of the nature of the parent material to soil formation and type. Then, cite at least 2 examples in which the influence of parent materials might be outweighed by other soil-forming factors. Explain the “struggle” between the internal and external processes in shaping the Earth’s surface. What are the different ways that the surface of the Earth is changed over time? Describe the general sequence of events in continental drift since the time of 5 separate continents 450 million years ago. What is the difference between the older continental drift theory by Wegener and the more recent plate tectonic theory? Plate tectonics theory explains many seemingly unrelated phenomena. Explain how the patterns of volcanoes and earthquakes related to plate tectonics. Explain several pieces of evidence that combine to make the theory of plate tectonics the one that is generally accepted. Provide a reason why some scientists believe the Pleistocene is over and a reason why other scientists believe we are now in an interglacial stage. Some believe, for example, that since areas of pack ice and glacial ice still exist we are still in an ice age. Others, on the other hand, seeing the rapid retreat of ice and snow pack in many areas, believes that this period of glaciation has ended. So, using some other justifications, why do we see some differences in interpretation? Is there some scientific data available that can support both sides view? If so, provide it. Why hasn’t this controversy been solved? What impact does this division of views have on the public policies that are enacted by state, national and international bodies? .
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The Final exam primarily covers the areas of the hydrosphere, the bi.docx
The Final exam primarily covers the areas of the hydrosphere, the biosphere and the lithosphere. As in the Midterm, special attention should be paid to the lecture notes and the PowerPoint files, as well as the Discussion Boards. These sections are dependent on the text and the laboratory exercises, but the discussions and the lecture notes are more conducive to explanation and understanding with a essay-driven format. Additionally, the animated PowerPoints are good at achieving an understanding of processes that are in motion, especially when looking at the lithosphere, giving them more of a 3-dimensional quality.
For this final essay exam you are required to answer all five (5) of the questions. Although there is no set word limit for these essay questions, you will be graded on your knowledge of the material and the detail with which you write your answers. You should take care to cite your sources in APA format and provide full references in a Works Cited list.
Describe the paths of water through the hydrologic cycle. Explain the processes and the energy gains and losses involved in the changes of water between its 3 states. Operationally, we often most concerned with water does when it reaches the solid earth, both on the surface and in the sub-surface. Explain the relationship between the saturated zone, the water table, a ground water well and the cone of depression, all within the sub-surface.
The food chain is a valuable concept in biogeography. Give an example of a specific food chain, labeling the various levels of the food chain. After looking at characteristics of food chains, explain how a geographer’s approach to the study of organisms might be different than biologist’s study of organisms; what would each try to emphasize more than the other? What exactly is a biome? Compare/contrast the concept of the biome with that of the zoogeographic region. Compare/contrast the floral characteristics of 2 of the following biomes: Desert, Tundra, Midlatitude Grassland and Boreal Forest.
Theorize the difference in soil development in adjoining soils developed on forested, sloped area versus a grassed flat area. What are the soil-forming factors? Explain the importance of the nature of the parent material to soil formation and type. Then, cite at least 2 examples in which the influence of parent materials might be outweighed by other soil-forming factors. Explain the “struggle” between the internal and external processes in shaping the Earth’s surface. What are the different ways that the surface of the Earth is changed over time?
Describe the general sequence of events in continental drift since the time of 5 separate continents 450 million years ago. What is the difference between the older continental drift theory by Wegener and the more recent plate tectonic theory? Plate tectonics theory explains many seemingly unrelated phenomena. Explain how the patterns of volcanoes and earthquakes related to plate tectonics..
The importance of continents, oceans and plate tectonics for the evolution of...
Within the uncertainties of involved astronomical and biological parameters, the Drake Equation
typically predicts that there should be many exoplanets in our galaxy hosting active, communicative
civilizations (ACCs). These optimistic calculations are however not supported by evidence, which is
often referred to as the Fermi Paradox. Here, we elaborate on this long-standing enigma by showing
the importance of planetary tectonic style for biological evolution. We summarize growing evidence
that a prolonged transition from Mesoproterozoic active single lid tectonics (1.6 to 1.0 Ga) to modern
plate tectonics occurred in the Neoproterozoic Era (1.0 to 0.541 Ga), which dramatically accelerated
emergence and evolution of complex species. We further suggest that both continents and oceans
are required for ACCs because early evolution of simple life must happen in water but late evolution
of advanced life capable of creating technology must happen on land. We resolve the Fermi Paradox
(1) by adding two additional terms to the Drake Equation: foc
(the fraction of habitable exoplanets
with significant continents and oceans) and fpt
(the fraction of habitable exoplanets with significant
continents and oceans that have had plate tectonics operating for at least 0.5 Ga); and (2) by
demonstrating that the product of foc
and fpt
is very small (< 0.00003–0.002). We propose that the lack
of evidence for ACCs reflects the scarcity of long-lived plate tectonics and/or continents and oceans on
exoplanets with primitive life.
Geological time scale & Dating methods
The document provides an introduction to the geological time scale and methods for dating rocks and events in Earth's history. It discusses that the geological time scale is a system that relates geological strata and events to periods of time in Earth's past. Relative dating methods look at principles like superposition to determine the sequence of rock layers, while absolute dating provides numerical ages using radiometric dating techniques like uranium-lead dating. The document outlines important divisions of the geological time scale including eons, eras, periods, and epochs, and summarizes some key boundaries that indicate changes in life forms, like the Precambrian-Cambrian boundary marking the rise of multicellular life.
Erosion and sedimentation
This chapter discusses two main processes that shape the Earth's surface topography: climatic and vegetative zonation, and geographical cycles. Zonation divides the Earth into climate zones from poles to equator based on factors like latitude and vegetation. Geographical cycles describe the evolution of landscapes through youth, maturity, and old age stages. While zonation and cycles were originally seen as competing theories, they are now viewed as often complementary. Zonation has influenced paleogeography and sedimentation since life became widespread, while cycles better describe some arid landscapes. Both processes, along with tectonics and eustatic sea level changes, have interacted to sculpt the Earth's surface over geological time.
Page 1 1.1 IntroductIonThe average introductory geolog.docx
Page | 1
1.1 IntroductIon
The average introductory geology student’s perception of geology normally in-
volves the memorization of rocks and discussions of natural disasters, but Geology
contains so much more. Geology is the study of our planet, which is vital to our ev-
eryday lives from the energy we use, to the growing of the food we eat, to the foun-
dations of the buildings we live in, to the materials that are used to make everyday
objects (metals and plastics). The ideal place to start this course is discussing the
methods that are used to better understand our planet, the processes that shape it,
and its history.
Science is not a set of facts to remember. Instead it is a method to discover
the world around us. You are likely already familiar with the Scientific Method,
but it is worthwhile to review the process. The first step of the scientific method
is making an observation or learning the background surrounding the question in
which you are interested. This can be done by taking classes on a subject matter
as you are doing presently in geology or by simply taking careful notes about your
surroundings. Based on your knowledge and observations, you can then make a
hypothesis, which is a testable prediction on how something works. A hypothesis
should be framed in a way that is easy to test and prove wrong. This might sound
odd, but science works to rigorously disprove a hypothesis and only those that
withstand the tests become accepted. The wonderful aspect of this definition of a
hypothesis is that the testing results in a brand new observation that can then be
used to formulate a new hypothesis. Therefore, whether the hypothesis is verified
or rejected it will lead to new information. The next step is communication to other
scientists. This allows other scientists to repeat the experiment as well as alter it in
new and unthought-of ways that can then expand on the original idea. These few
steps encompass the vast majority of the scientific method and the career of any
individual scientist. As hundreds of related observations and tested hypotheses
accumulate scientists can formulate a theory. The scientific meaning of a theory is
an explanation for a natural phenomenon that is supported by a wealth of scientific
1 Introduction to Physical GeologyBradley Deline
Page | 2
Introductory GeoloGy IntroductIon to physIcal GeoloGy
data. A theory is not yet a law because there still may be some debate on the exact
workings of the theory or the reasons why a phenomenon occurs, but there is little
debate on the existence of what is being described.
This leads us back to Geology, the scientific study of the Earth. There are as-
pects in geology that are directly testable, but others are not and geologists must
become imaginative in discovering aspects about the earth and its history that we
will never be able to directly observe. In this laboratory manual we will discuss the
materials that make up the ear.
Intraplate magmatism intraplate volcanism
This summary provides the key points from the document in 3 sentences:
The document discusses a study that proposes a new hypothesis for the origin of intraplate volcanism. The study suggests that some intraplate volcanic activity, like the Steens-Columbia River flood basalt, can be explained by tearing of subducting tectonic plates as they slow down, which allows rapid mantle upwelling. While this model may explain some cases of intraplate magmatism, it does not fully account for all aspects of some systems like Yellowstone, so the relationship between plate tectonics and intraplate volcanism remains an area of ongoing research.
Required Resources httpswww.cdc.govphlpnewscurrent.htmlh.docx
Required Resources
https://www.cdc.gov/phlp/news/current.html
https://www.congress.gov/
https://www.congress.gov/legislative-process
Geobiology is the study of the interactions that occur between the biosphere and the geosphere. It must include elements of the atmosphere, the hydrosphere and the lithosphere. When I looked up geobiology a lot of the articles came up about climate change.
Geologists think of the last 50 million years as the recent past, both because they represents only about one percent of the age of the earth. As well as because plate tectonics, the geologic process that controls conditions within the solid part of the earth, has operated without major change during that time period. This is the time period that is most relevant to gaining insights about earth’s climate. Which can be applied to the present-day global warming. Geological record of ancient climate is good. Ancient temperatures can be determined very precisely, because the composition of the shells of corals and other marine organisms varies measurably with it. The plants and animals that lived during a given time and are now preserved as fossils indicate whether the climate was wet or dry. Overall climatic trend has been cooling, from an unusually warm period. This is called the Eocene Optimum. Before like 55-45 million years ago, there was a cool period, colloquially called the Ice Age. It ended just 20,000 years ago. The overall range in temperature was huge it was about 35°F. During the Eocene Optimum it was warm that Antarctica was ice-free. The ice caps did not start to form there until about 35 million years ago. Palm trees grew at high latitudes. As well cold-blooded animals, such as crocodiles, lived in the Arctic. The earth’s climate is highly variable. During the Eocene Optimum and the Ice Age, though in both cases life was more abundant in some parts of the world than in others. The fossil record indicates that forests were common during the Eocence Optimum. But in some areas were vegetated steppes and deserts. While the great glaciers of the Ice Age were lifeless, extremely large mammals inhabited lower latitudes. Some species adapted and others went extinct. Climate during the Ice Age was unstable. Many swings of more than 10°F. The Milankovitch cycles, which is a cycle due to the gravitational influence of the moon and planets. The timing of these swings closely follows regular fluctuations in the tilt of the earth’s axis and the shape of its orbit around the sun. The magnitude can be reliably calculated.
Another article stated that the a changing climate has been the norm throughout the 4.6 billion year history of the Earth. Recent geological past, climate swings have given us repeated glaciations separated by warmer intervals. Climate is intimately connected to the evolution of life, to the erosion and formation of rocks, and even to the generation of mountains. The connections is the transfer of carbon from one place is a process known as.
Role of the disturbance in shaping bio geography
It will help to students who study bio geography and relevant subjects , this is a project what we have done in our university and now i m publishing this for your references. in this presentation we describe of disturbance types and how it was worked , unfortunately we are not able to upload the containing video to this presentation if you need it just you will able to get it from you tube by searching plate tectonics mechanism , study well and best of luck !!!!!!!
Recommended
The Final exam primarily covers the areas of the hydrosphere, the bi.docx
The Final exam primarily covers the areas of the hydrosphere, the biosphere and the lithosphere. As in the Midterm, special attention should be paid to the lecture notes and the PowerPoint files, as well as the Discussion Boards. These sections are dependent on the text and the laboratory exercises, but the discussions and the lecture notes are more conducive to explanation and understanding with a essay-driven format. Additionally, the animated PowerPoints are good at achieving an understanding of processes that are in motion, especially when looking at the lithosphere, giving them more of a 3-dimensional quality.
For this final essay exam you are required to answer all five (5) of the questions. Although there is no set word limit for these essay questions, you will be graded on your knowledge of the material and the detail with which you write your answers. You should take care to cite your sources in APA format and provide full references in a Works Cited list.
Describe the paths of water through the hydrologic cycle. Explain the processes and the energy gains and losses involved in the changes of water between its 3 states. Operationally, we often most concerned with water does when it reaches the solid earth, both on the surface and in the sub-surface. Explain the relationship between the saturated zone, the water table, a ground water well and the cone of depression, all within the sub-surface.
The food chain is a valuable concept in biogeography. Give an example of a specific food chain, labeling the various levels of the food chain. After looking at characteristics of food chains, explain how a geographer’s approach to the study of organisms might be different than biologist’s study of organisms; what would each try to emphasize more than the other? What exactly is a biome? Compare/contrast the concept of the biome with that of the zoogeographic region. Compare/contrast the floral characteristics of 2 of the following biomes: Desert, Tundra, Midlatitude Grassland and Boreal Forest.
Theorize the difference in soil development in adjoining soils developed on forested, sloped area versus a grassed flat area. What are the soil-forming factors? Explain the importance of the nature of the parent material to soil formation and type. Then, cite at least 2 examples in which the influence of parent materials might be outweighed by other soil-forming factors. Explain the “struggle” between the internal and external processes in shaping the Earth’s surface. What are the different ways that the surface of the Earth is changed over time?
Describe the general sequence of events in continental drift since the time of 5 separate continents 450 million years ago. What is the difference between the older continental drift theory by Wegener and the more recent plate tectonic theory? Plate tectonics theory explains many seemingly unrelated phenomena. Explain how the patterns of volcanoes and earthquakes related to plate tectonics..
The importance of continents, oceans and plate tectonics for the evolution of...
Within the uncertainties of involved astronomical and biological parameters, the Drake Equation
typically predicts that there should be many exoplanets in our galaxy hosting active, communicative
civilizations (ACCs). These optimistic calculations are however not supported by evidence, which is
often referred to as the Fermi Paradox. Here, we elaborate on this long-standing enigma by showing
the importance of planetary tectonic style for biological evolution. We summarize growing evidence
that a prolonged transition from Mesoproterozoic active single lid tectonics (1.6 to 1.0 Ga) to modern
plate tectonics occurred in the Neoproterozoic Era (1.0 to 0.541 Ga), which dramatically accelerated
emergence and evolution of complex species. We further suggest that both continents and oceans
are required for ACCs because early evolution of simple life must happen in water but late evolution
of advanced life capable of creating technology must happen on land. We resolve the Fermi Paradox
(1) by adding two additional terms to the Drake Equation: foc
(the fraction of habitable exoplanets
with significant continents and oceans) and fpt
(the fraction of habitable exoplanets with significant
continents and oceans that have had plate tectonics operating for at least 0.5 Ga); and (2) by
demonstrating that the product of foc
and fpt
is very small (< 0.00003–0.002). We propose that the lack
of evidence for ACCs reflects the scarcity of long-lived plate tectonics and/or continents and oceans on
exoplanets with primitive life.
Geological time scale & Dating methods
The document provides an introduction to the geological time scale and methods for dating rocks and events in Earth's history. It discusses that the geological time scale is a system that relates geological strata and events to periods of time in Earth's past. Relative dating methods look at principles like superposition to determine the sequence of rock layers, while absolute dating provides numerical ages using radiometric dating techniques like uranium-lead dating. The document outlines important divisions of the geological time scale including eons, eras, periods, and epochs, and summarizes some key boundaries that indicate changes in life forms, like the Precambrian-Cambrian boundary marking the rise of multicellular life.
Erosion and sedimentation
This chapter discusses two main processes that shape the Earth's surface topography: climatic and vegetative zonation, and geographical cycles. Zonation divides the Earth into climate zones from poles to equator based on factors like latitude and vegetation. Geographical cycles describe the evolution of landscapes through youth, maturity, and old age stages. While zonation and cycles were originally seen as competing theories, they are now viewed as often complementary. Zonation has influenced paleogeography and sedimentation since life became widespread, while cycles better describe some arid landscapes. Both processes, along with tectonics and eustatic sea level changes, have interacted to sculpt the Earth's surface over geological time.
Page 1 1.1 IntroductIonThe average introductory geolog.docx
Page | 1
1.1 IntroductIon
The average introductory geology student’s perception of geology normally in-
volves the memorization of rocks and discussions of natural disasters, but Geology
contains so much more. Geology is the study of our planet, which is vital to our ev-
eryday lives from the energy we use, to the growing of the food we eat, to the foun-
dations of the buildings we live in, to the materials that are used to make everyday
objects (metals and plastics). The ideal place to start this course is discussing the
methods that are used to better understand our planet, the processes that shape it,
and its history.
Science is not a set of facts to remember. Instead it is a method to discover
the world around us. You are likely already familiar with the Scientific Method,
but it is worthwhile to review the process. The first step of the scientific method
is making an observation or learning the background surrounding the question in
which you are interested. This can be done by taking classes on a subject matter
as you are doing presently in geology or by simply taking careful notes about your
surroundings. Based on your knowledge and observations, you can then make a
hypothesis, which is a testable prediction on how something works. A hypothesis
should be framed in a way that is easy to test and prove wrong. This might sound
odd, but science works to rigorously disprove a hypothesis and only those that
withstand the tests become accepted. The wonderful aspect of this definition of a
hypothesis is that the testing results in a brand new observation that can then be
used to formulate a new hypothesis. Therefore, whether the hypothesis is verified
or rejected it will lead to new information. The next step is communication to other
scientists. This allows other scientists to repeat the experiment as well as alter it in
new and unthought-of ways that can then expand on the original idea. These few
steps encompass the vast majority of the scientific method and the career of any
individual scientist. As hundreds of related observations and tested hypotheses
accumulate scientists can formulate a theory. The scientific meaning of a theory is
an explanation for a natural phenomenon that is supported by a wealth of scientific
1 Introduction to Physical GeologyBradley Deline
Page | 2
Introductory GeoloGy IntroductIon to physIcal GeoloGy
data. A theory is not yet a law because there still may be some debate on the exact
workings of the theory or the reasons why a phenomenon occurs, but there is little
debate on the existence of what is being described.
This leads us back to Geology, the scientific study of the Earth. There are as-
pects in geology that are directly testable, but others are not and geologists must
become imaginative in discovering aspects about the earth and its history that we
will never be able to directly observe. In this laboratory manual we will discuss the
materials that make up the ear.
Intraplate magmatism intraplate volcanism
This summary provides the key points from the document in 3 sentences:
The document discusses a study that proposes a new hypothesis for the origin of intraplate volcanism. The study suggests that some intraplate volcanic activity, like the Steens-Columbia River flood basalt, can be explained by tearing of subducting tectonic plates as they slow down, which allows rapid mantle upwelling. While this model may explain some cases of intraplate magmatism, it does not fully account for all aspects of some systems like Yellowstone, so the relationship between plate tectonics and intraplate volcanism remains an area of ongoing research.
Required Resources httpswww.cdc.govphlpnewscurrent.htmlh.docx
Required Resources
https://www.cdc.gov/phlp/news/current.html
https://www.congress.gov/
https://www.congress.gov/legislative-process
Geobiology is the study of the interactions that occur between the biosphere and the geosphere. It must include elements of the atmosphere, the hydrosphere and the lithosphere. When I looked up geobiology a lot of the articles came up about climate change.
Geologists think of the last 50 million years as the recent past, both because they represents only about one percent of the age of the earth. As well as because plate tectonics, the geologic process that controls conditions within the solid part of the earth, has operated without major change during that time period. This is the time period that is most relevant to gaining insights about earth’s climate. Which can be applied to the present-day global warming. Geological record of ancient climate is good. Ancient temperatures can be determined very precisely, because the composition of the shells of corals and other marine organisms varies measurably with it. The plants and animals that lived during a given time and are now preserved as fossils indicate whether the climate was wet or dry. Overall climatic trend has been cooling, from an unusually warm period. This is called the Eocene Optimum. Before like 55-45 million years ago, there was a cool period, colloquially called the Ice Age. It ended just 20,000 years ago. The overall range in temperature was huge it was about 35°F. During the Eocene Optimum it was warm that Antarctica was ice-free. The ice caps did not start to form there until about 35 million years ago. Palm trees grew at high latitudes. As well cold-blooded animals, such as crocodiles, lived in the Arctic. The earth’s climate is highly variable. During the Eocene Optimum and the Ice Age, though in both cases life was more abundant in some parts of the world than in others. The fossil record indicates that forests were common during the Eocence Optimum. But in some areas were vegetated steppes and deserts. While the great glaciers of the Ice Age were lifeless, extremely large mammals inhabited lower latitudes. Some species adapted and others went extinct. Climate during the Ice Age was unstable. Many swings of more than 10°F. The Milankovitch cycles, which is a cycle due to the gravitational influence of the moon and planets. The timing of these swings closely follows regular fluctuations in the tilt of the earth’s axis and the shape of its orbit around the sun. The magnitude can be reliably calculated.
Another article stated that the a changing climate has been the norm throughout the 4.6 billion year history of the Earth. Recent geological past, climate swings have given us repeated glaciations separated by warmer intervals. Climate is intimately connected to the evolution of life, to the erosion and formation of rocks, and even to the generation of mountains. The connections is the transfer of carbon from one place is a process known as.
Role of the disturbance in shaping bio geography
It will help to students who study bio geography and relevant subjects , this is a project what we have done in our university and now i m publishing this for your references. in this presentation we describe of disturbance types and how it was worked , unfortunately we are not able to upload the containing video to this presentation if you need it just you will able to get it from you tube by searching plate tectonics mechanism , study well and best of luck !!!!!!!
ES 1010, Earth Science 1 Course Learning Outcomes for.docx
ES 1010, Earth Science 1
Course Learning Outcomes for Unit V
Upon completion of this unit, students should be able to:
7. Compare the geography, composition, circulation, and temporal cycles of the oceans.
Reading Assignment
Chapter 9:
Oceans: The Last Frontier
Chapter 10:
The Restless Ocean
Watch the following video:
Williams, C. [IDT-CSU]. (2015, August 7). Coastal processes [Video file]. Retrieved from
https://youtu.be/ZO07SgCFKWs
Click here to access a transcript of the video.
NASA Goddard. (2008, October 24). In the zone. Retrieved from https://youtu.be/lB1FADETAyg
Unit Lesson
It is easy to see why Earth is referred to as the “Blue
Planet”—71% of the Earth’s surface is covered by
oceans and seas. However, less than 5% of our
oceans have been explored (National Oceanic and
Atmospheric Administration [NOAA] 2014). So
essentially, most of our Earth is still unexplored and
largely unknown. We do know that oceans contain the
highest mountains, the deepest trenches, and the
longest mountain ranges. On average, the ocean
depth is about four times the average elevation of
continents. In fact, Lutgens & Tarbuck (2014) state that
if the Earth’s continents were perfectly flat, they would
be completely submerged under more than 2,000
meters of seawater!
Oceanography is the branch of science that studies
the world’s oceans. It includes geology, chemistry,
physics, and biology (Lutgens & Tarbuck, 2014).
Oceanographers started mapping the oceans floors as
early as 1872 by dropping weighted lines down to the
ocean bottom at random points. The use of sound navigation and ranging (sonar) began during World War I
to detect enemy submarines, and was later improved during World War II. Sonar uses the echo of sound
waves to plot the profile of the ocean floor. Satellite radar technology has also contributed to mapping the
ocean floor. Today, we have a fairly good picture of the ocean floor topography.
As we study the ocean floor, we notice three major features: continental margins, basin floors, and mid-
oceanic ridge. The continental margins can be classified as active or passive. Active margins are where the
UNIT V STUDY GUIDE
Oceans
An iceberg captured on camera during a 30-day mission in
2012 to map areas of the Arctic aboard the NOAA Ship
Fairweather (NOAA, 2013).
https://online.columbiasouthern.edu/CSU_Content/courses/General_Studies/ES/ES1010/15N/UnitV_CoastalProcesses.pdf
ES 1010, Earth Science
UNIT x STUDY GUIDE
Title
ocean lithosphere is subducted beneath the continental crust (recall what you learned in Units III and IV).
These are mainly found around the Pacific Ocean. Passive margins are those that are not experiencing plate
tectonic activity and have more stable topography. Basin floors make up about 30% of the Earth’s surface
(Lutgens & Tarbuck, 2014). These areas are between the margins and the mid-ocean ridges and include
deep trenches, under ...
Historyoftheearth
The document summarizes key concepts in geology, including:
1) The formation of the solar system from a nebula of dust and gas around 4.5 billion years ago, which led to the formation of the Sun and planets through gravitational attraction and other processes.
2) Methods for determining the age of the Earth including absolute radiometric dating techniques that measure radioactive decay and relative dating principles like superposition and cross-cutting relationships.
3) The use of fossils to provide temporal and paleoecological information about Earth's history and environmental conditions of different periods. Index fossils in particular help date and classify rock layers.
Overview of evolution
The document discusses three types of evolution: geologic, biologic, and technologic. It focuses on geologic evolution, explaining how rocks, fossils, and ice cores provide evidence of changes to the Earth's surface and climate over time, as well as changes to life forms. The law of superposition and use of index fossils allow scientists to determine the relative ages of rock layers. Studying this geologic evidence has helped scientists develop an understanding of how the Earth and life have evolved over millions of years.
Science: Earth beyond six of nine planetary boundaries
This planetary boundaries framework update finds that six of the nine boundaries are transgressed, suggesting that Earth is now well outside of the safe operating space for humanity. Ocean acidification is close to being breached, while aerosol loading regionally exceeds the boundary. Stratospheric ozone levels have slightly recovered. The transgression level has increased for all boundaries earlier identified as overstepped. As primary production drives Earth system biosphere functions, human appropriation of net primary production is proposed as a control variable for functional biosphere integrity. This boundary is also transgressed. Earth system modeling of different levels of the transgression of the climate and land system change boundaries illustrates that these anthropogenic impacts on Earth system must be considered in a systemic context.
Publication date: 13th September 2023
Zoogeography
There are few places left on the planet where the impact of people has not been felt. We have explored and left our footprint on nearly every corner of the globe. As our population and needs grow, we are leaving less and less room for wildlife.
Wildlife are under threat from many different kinds of human activities, from directly destroying habitat to spreading invasive species and disease. Most ecosystems are facing multiple threats. Each new threat puts additional stress on already weakened ecosystems and their wildlife.
The earth system
The document discusses the interconnected nature of Earth's four main spheres: the geosphere, atmosphere, hydrosphere, and biosphere. It explains that the geosphere, made up of Earth's solid interior and surface, interacts with the other spheres through volcanism, rock weathering, and nutrient cycling. The atmosphere exchanges gases with the hydrosphere and biosphere and affects climate. The hydrosphere connects the other spheres via the water cycle and influences rock weathering. The biosphere interacts with all spheres through life processes like photosynthesis and nutrient transport. Appreciating these interconnected systems is important for understanding fields like medical geology and forensic geology.
Earth Science 3.5 : Time Marches On
The document summarizes key aspects of geologic timescales including:
1) Rock layers at places like the Grand Canyon provide evidence of nearly 2 billion years of Earth's history. Fossils preserved in sedimentary rocks also provide information about geologic eras.
2) Geologists have divided Earth's history into a geologic timescale including eons, eras, periods, and epochs to better study the planet's natural history.
3) Mass extinction events have occurred where a large percentage of species suddenly die off, such as the extinction that ended the Paleozoic era killing nearly 90% of marine species. Climate changes are believed to be a cause of some extinctions.
11. fossils and creation
This document discusses two contrasting views of the fossil record - the biblical view that life was created recently and most fossils are the result of a global flood, versus the evolutionary view that life evolved gradually over billions of years. It examines how the fossil record appears to show a progression from simple to complex organisms and explores creationist explanations for this pattern, including ecological zonation theory. This theory proposes that the order of fossils reflects the pre-Flood distribution of life across different ecological zones, which were destroyed sequentially by a rising flood.
Plate Tectonics and environment geology, minerals and rock, ecology and geology
This document summarizes key aspects of plate tectonics and how it relates to the environment, minerals, rocks, and ecology. It describes how plate tectonics theory explains the movement of tectonic plates in the earth's lithosphere. There are three main types of plate boundaries: divergent where plates move apart, convergent where they collide, and transform faults where motion is horizontal. Plate tectonics causes volcanism and mountain building which can influence climate patterns. Weathering and mining impact the environment and change rocks and minerals over time. Environmental factors like temperature and rainfall also control the rate of rock weathering. Ecology differs from geology in that ecology studies the relationships between living organisms and their habitat,
Intro to Earth System Science
The document introduces Earth system science, which views Earth as an interconnected system rather than separate parts. It describes Earth's four spheres - the atmosphere, geosphere, hydrosphere, and biosphere - and how they interact. It also outlines the scientific method and key terms used in Earth system science.
Prentice Hall ch12 geologic time part 1 edited
This document discusses methods that geologists use to determine the age of rocks and events in Earth's history. It introduces the concepts of relative dating, which determines the sequence of events but not their absolute age. Radiometric dating allows determining absolute ages by measuring the decay of radioactive isotopes. The geologic time scale divides Earth's history into standardized units like eons, eras, periods and epochs based on changes in life forms and rock formations. Radiometric dating has supported the immense timescale of geologic history.
Earth_Science_&_Climate_Change_Somenath_Ganguly
This document summarizes the relationship between global warming, sea level rise, and the melting of sea ice and continental ice sheets. It first discusses how increasing greenhouse gas emissions are causing global warming, which is melting both sea ice and continental ice reserves. However, it notes there is ambiguity about the rate of ice melting compared to the rate of sea level rise. The document then presents a conceptual model that differentiates the roles of sea ice, continental glaciers, and ice sheets in causing global or eustatic sea level rise. It concludes that while melting of continental ice sheets and glaciers, along with thermal expansion of the oceans, are responsible for recent sea level increases, melting of sea ice alone does not contribute to changes in global
Middle Range Theory Essay
The document discusses middle range theory in archaeology. Middle range theory aims to connect raw archaeological data to broader conclusions about human behavior in the past. It seeks to develop testable theories that are abstract enough for generalization but grounded in empirical evidence. While archaeologists initially applied middle range theory haphazardly, it has the potential to play an important role in the future by refocusing research on theoretical issues and human behavior rather than just interpretation. However, more work needs to be done to further define middle range theory in archaeology.
Unit 2 relief and water on earth wiki
The document provides an overview of relief and water on Earth. It discusses the structure of the Earth and how tectonic plate movements have shaped the continents over hundreds of millions of years. It also describes the main types of continental and oceanic relief that have been formed through internal forces like earthquakes and volcanoes, as well as external forces like erosion. Finally, it examines the distribution of water on Earth, including the characteristics and movements of oceans, seas, and continental freshwater sources.
Thompson Turk - Introduction to Physical Geology.pdf
This document provides an overview of the key concepts in geology. It discusses how the Earth appears static but is actually dynamic with slow continental drift and occasional rapid changes from earthquakes and volcanic eruptions. It introduces the concepts of uniformitarianism, where present geological processes can explain past events, and catastrophism, where rare catastrophic events cause rapid changes. It outlines the components of the Earth, including the solid Earth, hydrosphere, atmosphere and biosphere. It also presents the geological time scale which divides Earth's history into standardized eons, eras, periods and epochs based on the evolution of life.
SCI101-1501A-08 Introduction to the SciencesTask NamePhase 5 I.docx
SCI101-1501A-08 Introduction to the Sciences
Task Name: Phase 5 Individual Project
Deliverable Length: 4–5 pages (not including Title and Reference pages)
Details:
Weekly tasks or assignments (Individual or Group Projects) will be due by Monday and late submissions will be assigned a late penalty in accordance with the late penalty policy found in the syllabus. NOTE: All submission posting times are based on midnight Central Time.
The final paper for this course has multiple sections. Please read the following carefully.
Review the comments from your instructor, and make revisions to your Phase 4 Individual Project. Fix/add to Phase 4 IP assignment from the comments I gave you. Remember all changes need to be in red. After you have re-accomplished the phase 4 IP, add the 200-300 word essay on non-renewable fuel to the bottom?
Add 1 additional reference. Be sure to include the reference as both an in-text citation and an entry on your Reference list.
(Here are the comments from the instructor)
"Hi Ricky: Total points earned (rounded): 110 out of 150 (73%). Task Requirements points earned: 26.25 out of 37.5 (70%). Demonstration and application of knowledge points earned: 57.75 out of 82.5 (70%). Academic writing and format points earned: 25.5 out of 30 (85%). Late Penalty: 15% Strengths: Good paper, well written. Opportunities for improvement: You didn't once mention Wegner anywhere in your paper. Also I would have like to have seen you cover the fossils in the Reasons scientists now agree to continental drift paragraph. I would like to see a little more on the ring of fire... Additional Comments: A good paper but late. You cited your references well
Geographic evidence supporting the theory of continental drift
There is so much evidence today that supports the theory of continental drift. Through scientific research, many scientists have looked into different facts which support the continental drift theory. Some of the pieces of evidence available include the ocean floor which demonstrates ruggedness. Some scientists have confirmed the repeated reversal of the magnetic field of the earth which confirms that the continents are drifting away from each other (University of Columbia, n.d.). A hypothesis of the spreading of seafloor and the oceanic crust recycling associated with it. In addition to this, the pattern of earthquakes and volcanic activity are concentrated along the oceanic trenches and submarine mountain ranges. These are located at the edges of the tectonic plates.
Reasons scientists now agree to continental drift but did not agree to it in the past
There are various reasons why scientists agree to the continental drift theory. Although scientist at first did not accept the theory about continental drifting, there is some evidence which confirm that the theory has a lot of sense in it. First, there is so much evidence which proves that the continents lie on very big slabs called the tectonic plates. The activity.
Geomorphological indicators of climate change zewde alemayehu tilahun
The document discusses various geomorphological indicators of climate change. It begins by introducing geomorphology and its subfields including climatic geomorphology, fluvial geomorphology, tropical geomorphology, periglacial geomorphology, tectonic geomorphology, and coastal geomorphology. It then discusses specific geomorphological indicators of climate change such as lake growth at glacier margins as glaciers recede, increases in debris flows due to heavier rainfall, paraglacial adjustment of moraines as ice melts, increases in high altitude rock falls and avalanches, and ice falls and avalanches as glacial cover decreases. The document concludes by discussing indicators related to glacier change such as
Integrated Science M4 terrestrial environment
This document provides an introduction to a unit on the terrestrial environment and the biosphere. It begins by outlining the objectives and overview of the unit. The unit will introduce the components of the biosphere, ecosystems and biomes, and interactions among the spheres. It then defines key terms like biosphere, environment, and discusses the three main spheres of the biosphere - the atmosphere, hydrosphere, and lithosphere. The document provides examples of terrestrial and aquatic biomes and discusses abiotic and biotic factors within ecosystems. It also explores interactions between the spheres through examples like the water cycle and food chains/webs.
2_Intro_Oceanography.pptx
This document provides an introduction to oceanography. It discusses the four main branches of earth sciences - geology, meteorology, oceanography, and astronomy. Oceanography is defined as the study and description of the marine environment, involving disciplines like physics, biology, chemistry and geology. The document outlines several verticals within oceanography, including chemical, physical, geological, and biological oceanography. It also discusses marine biogeochemical cycles and plate tectonics. Plate tectonics involves the movement of tectonic plates at divergent boundaries where new crust is formed, and convergent boundaries where plates collide in different ways, such as continent-continent, continent-ocean, or ocean-ocean collisions.
Minding this Water Planet
Presentation using a pair of books to expand possibilities inherent in chemical and electromagnetic interaction leading to some wider speculation about the role the rich structure of H₂O has had and continues to have in shaping Life of this planet. Consequent linkage to persistent themes within our Supervenience project and wider orbit.
Describe what the Internet of Things means and how this interconnect.docx
Describe what the Internet of Things means and how this interconnectedness of smart devices will affect how we live and work. Do you foresee any positive and/or negative effects from this infrastructure based on billions of devices that will be collecting and exchanging data daily? Provide at least one example of a smart device and how it can be applied to the Internet of Things. A minimum of 3 to 5 paragraphs. Must include at least one source (a journal, periodical, article, etc.) from a Broward College Library database (Library Resources). Must include a Work Cited page for the source material. Must be submitted as a .docx (Microsoft Word) file and in APA format
.
Describe what the issue or decision of consideration is. Identify .docx
Describe what the issue or decision of consideration is. Identify who is involved in making the decision and who is affected by the decision(s),who are the stakeholders. Identify any and all alternatives in choice. Offer your opinion relative to decision making and choice.
Bioethical Analysis Worksheet Scenario
Chang and Fang Yin are a married couple living in China. They have decided to have a child and Fang Yin is at a stage in her pregnancy where the sex of the child can be determined. China is one of the most heavily populated countries in the world, and as a result the “One Child Policy” was put in place by the Chinese government. The policy was to ensure that China, a country that has historically been prone to severe famine and flooding, would be able to feed it’s people. The rapid population growth that occurred after the Communist Party came to power had put a strain on the government’s efforts to help it’s people. So in an attempt to combat the widespread poverty and improve the overall quality of life, the “One Child Policy” was gradually adopted. Chinese families overwhelmingly prefer male children to female children and as a result, female infanticide has increased. Also many people criticize the fact that abortions are often forced on women who are visibly pregnant with their second child. This often includes very late term abortions and there have been reports of mass sterilizations in rural areas as well. Fang Yin is under a lot of pressure from her husband and his family to have a boy to carry on the family name. They have told her that if she finds out the sex of her baby and it is a female, then she should take the proper steps to terminate the pregnancy and the family will even pay the cost of this. Fang Yin doesn’t care what sex the child is, she just wants a healthy baby. The issue is whether or not to determine the sex of the child while in the womb.
Hindu Gods and Goddesses
September 24, 2018
I. These are names of the Gods and Goddesses on the following page:
A. Trimuti (3 distinct gods are here)
B. Ganesha
C. Lakshmi
D. Kali
E. Hanuman
II. Do a little research on each god. Find and learn their names. What are the symbols usually associated with these gods? What are their powers? What is their popularity among Hindu people today?
III. Develop your findings into a nice paragraph or two for each God.
25 points/Friday 28 September, 2018
Study points or things you ought to know……..
• Hinduism is one of the oldest known organized religions—its sacred writings date as far back as 1400 to 1500 B.C. It is also one of the most diverse and complex, having millions of gods. Hindus have a wide variety of core beliefs and exist in many different sects. Although it is the third largest religion in the world, Hinduism exists primarily in India and Nepal.
• The main texts of Hinduism are the Vedas (considered most important), Upanishadas, the Mahabharata, and the Ramayana. These writings contain hymns, incantat.
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ES 1010, Earth Science 1
Course Learning Outcomes for Unit V
Upon completion of this unit, students should be able to:
7. Compare the geography, composition, circulation, and temporal cycles of the oceans.
Reading Assignment
Chapter 9:
Oceans: The Last Frontier
Chapter 10:
The Restless Ocean
Watch the following video:
Williams, C. [IDT-CSU]. (2015, August 7). Coastal processes [Video file]. Retrieved from
https://youtu.be/ZO07SgCFKWs
Click here to access a transcript of the video.
NASA Goddard. (2008, October 24). In the zone. Retrieved from https://youtu.be/lB1FADETAyg
Unit Lesson
It is easy to see why Earth is referred to as the “Blue
Planet”—71% of the Earth’s surface is covered by
oceans and seas. However, less than 5% of our
oceans have been explored (National Oceanic and
Atmospheric Administration [NOAA] 2014). So
essentially, most of our Earth is still unexplored and
largely unknown. We do know that oceans contain the
highest mountains, the deepest trenches, and the
longest mountain ranges. On average, the ocean
depth is about four times the average elevation of
continents. In fact, Lutgens & Tarbuck (2014) state that
if the Earth’s continents were perfectly flat, they would
be completely submerged under more than 2,000
meters of seawater!
Oceanography is the branch of science that studies
the world’s oceans. It includes geology, chemistry,
physics, and biology (Lutgens & Tarbuck, 2014).
Oceanographers started mapping the oceans floors as
early as 1872 by dropping weighted lines down to the
ocean bottom at random points. The use of sound navigation and ranging (sonar) began during World War I
to detect enemy submarines, and was later improved during World War II. Sonar uses the echo of sound
waves to plot the profile of the ocean floor. Satellite radar technology has also contributed to mapping the
ocean floor. Today, we have a fairly good picture of the ocean floor topography.
As we study the ocean floor, we notice three major features: continental margins, basin floors, and mid-
oceanic ridge. The continental margins can be classified as active or passive. Active margins are where the
UNIT V STUDY GUIDE
Oceans
An iceberg captured on camera during a 30-day mission in
2012 to map areas of the Arctic aboard the NOAA Ship
Fairweather (NOAA, 2013).
https://online.columbiasouthern.edu/CSU_Content/courses/General_Studies/ES/ES1010/15N/UnitV_CoastalProcesses.pdf
ES 1010, Earth Science
UNIT x STUDY GUIDE
Title
ocean lithosphere is subducted beneath the continental crust (recall what you learned in Units III and IV).
These are mainly found around the Pacific Ocean. Passive margins are those that are not experiencing plate
tectonic activity and have more stable topography. Basin floors make up about 30% of the Earth’s surface
(Lutgens & Tarbuck, 2014). These areas are between the margins and the mid-ocean ridges and include
deep trenches, under ...
Historyoftheearth
The document summarizes key concepts in geology, including:
1) The formation of the solar system from a nebula of dust and gas around 4.5 billion years ago, which led to the formation of the Sun and planets through gravitational attraction and other processes.
2) Methods for determining the age of the Earth including absolute radiometric dating techniques that measure radioactive decay and relative dating principles like superposition and cross-cutting relationships.
3) The use of fossils to provide temporal and paleoecological information about Earth's history and environmental conditions of different periods. Index fossils in particular help date and classify rock layers.
Overview of evolution
The document discusses three types of evolution: geologic, biologic, and technologic. It focuses on geologic evolution, explaining how rocks, fossils, and ice cores provide evidence of changes to the Earth's surface and climate over time, as well as changes to life forms. The law of superposition and use of index fossils allow scientists to determine the relative ages of rock layers. Studying this geologic evidence has helped scientists develop an understanding of how the Earth and life have evolved over millions of years.
Science: Earth beyond six of nine planetary boundaries
This planetary boundaries framework update finds that six of the nine boundaries are transgressed, suggesting that Earth is now well outside of the safe operating space for humanity. Ocean acidification is close to being breached, while aerosol loading regionally exceeds the boundary. Stratospheric ozone levels have slightly recovered. The transgression level has increased for all boundaries earlier identified as overstepped. As primary production drives Earth system biosphere functions, human appropriation of net primary production is proposed as a control variable for functional biosphere integrity. This boundary is also transgressed. Earth system modeling of different levels of the transgression of the climate and land system change boundaries illustrates that these anthropogenic impacts on Earth system must be considered in a systemic context.
Publication date: 13th September 2023
Zoogeography
There are few places left on the planet where the impact of people has not been felt. We have explored and left our footprint on nearly every corner of the globe. As our population and needs grow, we are leaving less and less room for wildlife.
Wildlife are under threat from many different kinds of human activities, from directly destroying habitat to spreading invasive species and disease. Most ecosystems are facing multiple threats. Each new threat puts additional stress on already weakened ecosystems and their wildlife.
The earth system
The document discusses the interconnected nature of Earth's four main spheres: the geosphere, atmosphere, hydrosphere, and biosphere. It explains that the geosphere, made up of Earth's solid interior and surface, interacts with the other spheres through volcanism, rock weathering, and nutrient cycling. The atmosphere exchanges gases with the hydrosphere and biosphere and affects climate. The hydrosphere connects the other spheres via the water cycle and influences rock weathering. The biosphere interacts with all spheres through life processes like photosynthesis and nutrient transport. Appreciating these interconnected systems is important for understanding fields like medical geology and forensic geology.
Earth Science 3.5 : Time Marches On
The document summarizes key aspects of geologic timescales including:
1) Rock layers at places like the Grand Canyon provide evidence of nearly 2 billion years of Earth's history. Fossils preserved in sedimentary rocks also provide information about geologic eras.
2) Geologists have divided Earth's history into a geologic timescale including eons, eras, periods, and epochs to better study the planet's natural history.
3) Mass extinction events have occurred where a large percentage of species suddenly die off, such as the extinction that ended the Paleozoic era killing nearly 90% of marine species. Climate changes are believed to be a cause of some extinctions.
11. fossils and creation
This document discusses two contrasting views of the fossil record - the biblical view that life was created recently and most fossils are the result of a global flood, versus the evolutionary view that life evolved gradually over billions of years. It examines how the fossil record appears to show a progression from simple to complex organisms and explores creationist explanations for this pattern, including ecological zonation theory. This theory proposes that the order of fossils reflects the pre-Flood distribution of life across different ecological zones, which were destroyed sequentially by a rising flood.
Plate Tectonics and environment geology, minerals and rock, ecology and geology
This document summarizes key aspects of plate tectonics and how it relates to the environment, minerals, rocks, and ecology. It describes how plate tectonics theory explains the movement of tectonic plates in the earth's lithosphere. There are three main types of plate boundaries: divergent where plates move apart, convergent where they collide, and transform faults where motion is horizontal. Plate tectonics causes volcanism and mountain building which can influence climate patterns. Weathering and mining impact the environment and change rocks and minerals over time. Environmental factors like temperature and rainfall also control the rate of rock weathering. Ecology differs from geology in that ecology studies the relationships between living organisms and their habitat,
Intro to Earth System Science
The document introduces Earth system science, which views Earth as an interconnected system rather than separate parts. It describes Earth's four spheres - the atmosphere, geosphere, hydrosphere, and biosphere - and how they interact. It also outlines the scientific method and key terms used in Earth system science.
Prentice Hall ch12 geologic time part 1 edited
This document discusses methods that geologists use to determine the age of rocks and events in Earth's history. It introduces the concepts of relative dating, which determines the sequence of events but not their absolute age. Radiometric dating allows determining absolute ages by measuring the decay of radioactive isotopes. The geologic time scale divides Earth's history into standardized units like eons, eras, periods and epochs based on changes in life forms and rock formations. Radiometric dating has supported the immense timescale of geologic history.
Earth_Science_&_Climate_Change_Somenath_Ganguly
This document summarizes the relationship between global warming, sea level rise, and the melting of sea ice and continental ice sheets. It first discusses how increasing greenhouse gas emissions are causing global warming, which is melting both sea ice and continental ice reserves. However, it notes there is ambiguity about the rate of ice melting compared to the rate of sea level rise. The document then presents a conceptual model that differentiates the roles of sea ice, continental glaciers, and ice sheets in causing global or eustatic sea level rise. It concludes that while melting of continental ice sheets and glaciers, along with thermal expansion of the oceans, are responsible for recent sea level increases, melting of sea ice alone does not contribute to changes in global
Middle Range Theory Essay
The document discusses middle range theory in archaeology. Middle range theory aims to connect raw archaeological data to broader conclusions about human behavior in the past. It seeks to develop testable theories that are abstract enough for generalization but grounded in empirical evidence. While archaeologists initially applied middle range theory haphazardly, it has the potential to play an important role in the future by refocusing research on theoretical issues and human behavior rather than just interpretation. However, more work needs to be done to further define middle range theory in archaeology.
Unit 2 relief and water on earth wiki
The document provides an overview of relief and water on Earth. It discusses the structure of the Earth and how tectonic plate movements have shaped the continents over hundreds of millions of years. It also describes the main types of continental and oceanic relief that have been formed through internal forces like earthquakes and volcanoes, as well as external forces like erosion. Finally, it examines the distribution of water on Earth, including the characteristics and movements of oceans, seas, and continental freshwater sources.
Thompson Turk - Introduction to Physical Geology.pdf
This document provides an overview of the key concepts in geology. It discusses how the Earth appears static but is actually dynamic with slow continental drift and occasional rapid changes from earthquakes and volcanic eruptions. It introduces the concepts of uniformitarianism, where present geological processes can explain past events, and catastrophism, where rare catastrophic events cause rapid changes. It outlines the components of the Earth, including the solid Earth, hydrosphere, atmosphere and biosphere. It also presents the geological time scale which divides Earth's history into standardized eons, eras, periods and epochs based on the evolution of life.
SCI101-1501A-08 Introduction to the SciencesTask NamePhase 5 I.docx
SCI101-1501A-08 Introduction to the Sciences
Task Name: Phase 5 Individual Project
Deliverable Length: 4–5 pages (not including Title and Reference pages)
Details:
Weekly tasks or assignments (Individual or Group Projects) will be due by Monday and late submissions will be assigned a late penalty in accordance with the late penalty policy found in the syllabus. NOTE: All submission posting times are based on midnight Central Time.
The final paper for this course has multiple sections. Please read the following carefully.
Review the comments from your instructor, and make revisions to your Phase 4 Individual Project. Fix/add to Phase 4 IP assignment from the comments I gave you. Remember all changes need to be in red. After you have re-accomplished the phase 4 IP, add the 200-300 word essay on non-renewable fuel to the bottom?
Add 1 additional reference. Be sure to include the reference as both an in-text citation and an entry on your Reference list.
(Here are the comments from the instructor)
"Hi Ricky: Total points earned (rounded): 110 out of 150 (73%). Task Requirements points earned: 26.25 out of 37.5 (70%). Demonstration and application of knowledge points earned: 57.75 out of 82.5 (70%). Academic writing and format points earned: 25.5 out of 30 (85%). Late Penalty: 15% Strengths: Good paper, well written. Opportunities for improvement: You didn't once mention Wegner anywhere in your paper. Also I would have like to have seen you cover the fossils in the Reasons scientists now agree to continental drift paragraph. I would like to see a little more on the ring of fire... Additional Comments: A good paper but late. You cited your references well
Geographic evidence supporting the theory of continental drift
There is so much evidence today that supports the theory of continental drift. Through scientific research, many scientists have looked into different facts which support the continental drift theory. Some of the pieces of evidence available include the ocean floor which demonstrates ruggedness. Some scientists have confirmed the repeated reversal of the magnetic field of the earth which confirms that the continents are drifting away from each other (University of Columbia, n.d.). A hypothesis of the spreading of seafloor and the oceanic crust recycling associated with it. In addition to this, the pattern of earthquakes and volcanic activity are concentrated along the oceanic trenches and submarine mountain ranges. These are located at the edges of the tectonic plates.
Reasons scientists now agree to continental drift but did not agree to it in the past
There are various reasons why scientists agree to the continental drift theory. Although scientist at first did not accept the theory about continental drifting, there is some evidence which confirm that the theory has a lot of sense in it. First, there is so much evidence which proves that the continents lie on very big slabs called the tectonic plates. The activity.
Geomorphological indicators of climate change zewde alemayehu tilahun
The document discusses various geomorphological indicators of climate change. It begins by introducing geomorphology and its subfields including climatic geomorphology, fluvial geomorphology, tropical geomorphology, periglacial geomorphology, tectonic geomorphology, and coastal geomorphology. It then discusses specific geomorphological indicators of climate change such as lake growth at glacier margins as glaciers recede, increases in debris flows due to heavier rainfall, paraglacial adjustment of moraines as ice melts, increases in high altitude rock falls and avalanches, and ice falls and avalanches as glacial cover decreases. The document concludes by discussing indicators related to glacier change such as
Integrated Science M4 terrestrial environment
This document provides an introduction to a unit on the terrestrial environment and the biosphere. It begins by outlining the objectives and overview of the unit. The unit will introduce the components of the biosphere, ecosystems and biomes, and interactions among the spheres. It then defines key terms like biosphere, environment, and discusses the three main spheres of the biosphere - the atmosphere, hydrosphere, and lithosphere. The document provides examples of terrestrial and aquatic biomes and discusses abiotic and biotic factors within ecosystems. It also explores interactions between the spheres through examples like the water cycle and food chains/webs.
2_Intro_Oceanography.pptx
This document provides an introduction to oceanography. It discusses the four main branches of earth sciences - geology, meteorology, oceanography, and astronomy. Oceanography is defined as the study and description of the marine environment, involving disciplines like physics, biology, chemistry and geology. The document outlines several verticals within oceanography, including chemical, physical, geological, and biological oceanography. It also discusses marine biogeochemical cycles and plate tectonics. Plate tectonics involves the movement of tectonic plates at divergent boundaries where new crust is formed, and convergent boundaries where plates collide in different ways, such as continent-continent, continent-ocean, or ocean-ocean collisions.
Minding this Water Planet
Presentation using a pair of books to expand possibilities inherent in chemical and electromagnetic interaction leading to some wider speculation about the role the rich structure of H₂O has had and continues to have in shaping Life of this planet. Consequent linkage to persistent themes within our Supervenience project and wider orbit.
Similar to Describe the paths of water through the hydrologic cycle. Explain.docx (20)
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Thompson Turk - Introduction to Physical Geology.pdf
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Describe what the Internet of Things means and how this interconnectedness of smart devices will affect how we live and work. Do you foresee any positive and/or negative effects from this infrastructure based on billions of devices that will be collecting and exchanging data daily? Provide at least one example of a smart device and how it can be applied to the Internet of Things. A minimum of 3 to 5 paragraphs. Must include at least one source (a journal, periodical, article, etc.) from a Broward College Library database (Library Resources). Must include a Work Cited page for the source material. Must be submitted as a .docx (Microsoft Word) file and in APA format
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Bioethical Analysis Worksheet Scenario
Chang and Fang Yin are a married couple living in China. They have decided to have a child and Fang Yin is at a stage in her pregnancy where the sex of the child can be determined. China is one of the most heavily populated countries in the world, and as a result the “One Child Policy” was put in place by the Chinese government. The policy was to ensure that China, a country that has historically been prone to severe famine and flooding, would be able to feed it’s people. The rapid population growth that occurred after the Communist Party came to power had put a strain on the government’s efforts to help it’s people. So in an attempt to combat the widespread poverty and improve the overall quality of life, the “One Child Policy” was gradually adopted. Chinese families overwhelmingly prefer male children to female children and as a result, female infanticide has increased. Also many people criticize the fact that abortions are often forced on women who are visibly pregnant with their second child. This often includes very late term abortions and there have been reports of mass sterilizations in rural areas as well. Fang Yin is under a lot of pressure from her husband and his family to have a boy to carry on the family name. They have told her that if she finds out the sex of her baby and it is a female, then she should take the proper steps to terminate the pregnancy and the family will even pay the cost of this. Fang Yin doesn’t care what sex the child is, she just wants a healthy baby. The issue is whether or not to determine the sex of the child while in the womb.
Hindu Gods and Goddesses
September 24, 2018
I. These are names of the Gods and Goddesses on the following page:
A. Trimuti (3 distinct gods are here)
B. Ganesha
C. Lakshmi
D. Kali
E. Hanuman
II. Do a little research on each god. Find and learn their names. What are the symbols usually associated with these gods? What are their powers? What is their popularity among Hindu people today?
III. Develop your findings into a nice paragraph or two for each God.
25 points/Friday 28 September, 2018
Study points or things you ought to know……..
• Hinduism is one of the oldest known organized religions—its sacred writings date as far back as 1400 to 1500 B.C. It is also one of the most diverse and complex, having millions of gods. Hindus have a wide variety of core beliefs and exist in many different sects. Although it is the third largest religion in the world, Hinduism exists primarily in India and Nepal.
• The main texts of Hinduism are the Vedas (considered most important), Upanishadas, the Mahabharata, and the Ramayana. These writings contain hymns, incantat.
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A minimum of 3 to 5 paragraphs.
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The paper must be written in APA format.
The minimum length of the discussion is 3 pages.
The minimum number of references is 2.
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H_0:
Most environmental crises in this decade were man-made.
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I need this written in APA Format, with at least one-in text citation from the following resource:
Daft, R. L. (2011).
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***200 words response with scholarly reference and in text citation***
Speaking of image, do you feel that no longer wearing traditional white uniforms has had an impact on how nurses are perceived? How is your clothing an important part of your public image?
***200 words response with scholarly reference and in text citation***
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***200 words response with scholarly reference and in text citation
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Your response should be a minimum of 300 word
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2. Name of the composer (if known).
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