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Climate Change Learning Cycle 1
Quiz by Russ Drylie
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​Which of these best explains how changes in the shape of Earth’s orbit and changes in the tilt o fEarth’s axis of rotation cause changes in climate?
These factors affect the sun’s energy output
These factors affect plate tectonic activity and the locations of continents
These factors affect the rate of carbon exchange between the biosphere and atmosphere.
 These factors affect the intensity and distribution of sunlight hitting the Earth.
​A planet’s distance from the sun affects its
input of energy
output of energy
storage and redistribution of energy
Which of these best explains how changes in the shape of Earth’s orbit and changes in the tilt o fEarth’s axis of rotation cause changes in climate?
A planet’s distance from the sun affects its
Which energy flows are impacted by a planet’s atmospheric characteristics?
Which energy flows are impacted by a planet’s atmospheric characteristics?
Once ice sheets start to form at the beginning of a glacial period, more energy is
Which of the following is a change the biosphere will have on one of Earth's other spheres during the glacial period?
How would a volcanic eruption change Earth's energy budget?
Geologists refer to the mineral formations in caves as“speleothems.” While the water flows, the speleothems grow in thin, shiny layers. The amount of growth is an indicator of how much ground water dripped into the cave. When the speleothems stop growing, the outside becomes dirty and eroded in places, giving it a dull appearance. A growing speleothem looks smooth and wet.”
“The cross section of a stalagmite reveals a sequence of layers, similar to the growth rings of trees, laid down over time. Researchers determine the ages of the layers using Uranium-Thorium radiometric dating, andexamine layer thickness and oxygen isotopes to determine past climate.”
Based on the information provided, what do scientists measure in order to study the relationship between speleothems and past climate?
Geologists refer to the mineral formations in caves as“speleothems.” While the water flows, the speleothems grow in thin, shiny layers. The amount of growth is an indicator of how much ground water dripped into the cave. When the speleothems stop growing, the outside becomes dirty and eroded in places, giving it a dull appearance. A growing speleothem looks smooth and wet.”
“The cross section of a stalagmite reveals a sequence of layers, similar to the growth rings of trees, laid down over time. Researchers determine the ages of the layers using Uranium-Thorium radiometric dating, andexamine layer thickness and oxygen isotopes to determine past climate.”
Based on the information provided, what do scientists measure in order to study the relationship between speleothems and past climate?
Based on the information provided the graph, which of these best identifies the purpose of the data analysis displayed?
Geologists refer to the mineral formations in caves as“speleothems.” While the water flows, the speleothems grow in thin, shiny layers. The amount of growth is an indicator of how much ground water dripped into the cave. When the speleothems stop growing, the outside becomes dirty and eroded in places, giving it a dull appearance. A growing speleothem looks smooth and wet.”
“The cross section of a stalagmite reveals a sequence of layers, similar to the growth rings of trees, laid down over time. Researchers determine the ages of the layers using Uranium-Thorium radiometric dating, andexamine layer thickness and oxygen isotopes to determine past climate.”
Continental Drift Theory. From the discussion of the rock cycle, it has been pointed out that through Earth's external and internal processes. Earth's surface is constantly changing. However, this idea of a changing environment did not conform with the belief of earlier scientists. Rather, they thought that the geographic positions of ocean basins and continents have been static since the beginning of time. It was around the 1500s when Leonardo da Vinci, upon his discovery of fossil seashells found at the high mountains of Italy, first thought of the idea that the areas where mountains are located may have been oceans in the past. Through time, other fossils of marine organisms found far above the current sea level further supported the idea that mountains were uplifted and weathering wore them down. At around the 1800s, most scientists have accepted the idea that Earth's crust is undergoing large vertical movements or uplifting. There was also evidence of possible horizontal movements, but the scientists then were not convinced about it. Alfred Wegener showed evidence of horizontal or lateral movement of the continents in his continental drift theory. According to him, the continents have drifted around the world and have once formed a giant landmass or supercontinent called Pangaea. To support his theory, Alfred Wegener presented a set of geographical, biological, and climatic evidence.Wegener's geographical evidence included the jigsaw puzzle fit of the current continents. He pointed out that the coastlines of South America and Africa seem to fit together. He also pointed the presence of mountain ranges having similar rock types and age but separated by vast oceans, like that of the folded rocks of the Caledonian mountains. The same folded rocks run through West Africa, North America, Newfoundland, Ireland, Wales, Scotland, Greenland, and Norway, all of which are now separated by the Atlantic Ocean. A geographical evidence on the similar rock types in West Africa, North America, Greenland, and Europe is found. The biological evidence came in the discovery of similar plant and animal fossils in different continents separated by oceans. The animal fossils of Mesosaurus and Lystrosaurus indicate that they were not capable of crossing the oceans to reach the other continents. If they were, the fossils should have been more widely distributed Africa, Australia, India, and South America were too large to be carried by wind. This indicates that the areas where the fossils were found were closely linked. It has also been found out that the plant only grew in areas with subpolar climate, which would indicate that the landmasses were located near the South Pole.Lastly, for his climatic evidence, Wegener discovered that a glacial period occurred during the late Paleozoic era in Southern Africa, South America, Australia, and India. The initial explanation for this event was global cooling, but it was rejected because large tropical swamps with so much vegetation were found at the same time in the Northern Hemisphere. This further supported the idea that the supercontinent was indeed near the South Pole, and the continents in Northern Hemisphere were once near the equator. The glacial period also left glacial striations, or the scratches glaciers make as they move across on the underlying bedrock, on the aforementioned continents. For such an event to happen, the continents would have to be connected. SCIENCE PIONEER. Alfred Wegener (1880-1930). Alfred Wegener was a German polar researcher, geophysicist, and meteorologist. He was known for his work on the continental drift theory. In his effort to defend his work, he went to the Greenland ice sheet where he died.Even with all the compelling evidence, the continental drift theory hardly convinced the scientific community at that time because Wegener was unable to identify a credible mechanism that drives the continental drift. He was unable to clearly explain how the continents moved and how the larger continents broke through the ocean floor. Eventually, critics of the continental drift began to accept the theory when new evidence supporting the theory was discovered. The new evidence led to a more encompassing theory the theory of plate tectonics. This theory provided a more convincing explanation as to how the continents moved. The evidence that paved the way for the theory of plate tectonics was the idea of wandering poles. Scientists began studying volcanic rocks to determine the location of the magnetic poles. When volcanic rocks crystallize, the minerals with magnetic properties align themselves parallel to Earth's magnetic field at the time the minerals were formed. This finding allowed scientists to determine the polarity of Earth's magnetic field and the magnetic inclination that showed the location of the poles. Upon studying the paleomagnetism of the rocks, geophysicists found out that rocks from various locations point to different magnetic north poles, suggesting that the poles have wandered. Since movement of magnetic poles is very unlikely, scientists have accepted the idea that the continents are indeed moving. And if the continents are moving, scientists thought that maybe the ocean basins are moving too. They also discovered that some rocks showed magnetic reversals, which led them to believe that the magnetic north pole now was not always the magnetic north pole. Seafloor Spreading. After World War II, exploration on the ocean floor became the focus of many geologic studies. It was only then that the ocean ridge system was discovered. A geologist in Princeton University named Harry Hess, along with other scientists, studied this ocean ridge system and hypothesized that the oceanic crust was moving away from the ridge. His hypothesis, known as seafloor spreading, showed that the ocean floor is split along the ridge where the magma rises to form the new ocean floor.Because of this, rocks located near the ridge are younger than those that are located magnetic polarity of Earth is also preserved in those rocks. Withe ridge scientists were able to see the magnetic reversals in the ocean floor, and they were able to make use of information to determine that the ocean floor is moving at a rate of about 10 cm per year. Plate Tectonics. Confirmation of the seafloor spreading hypothesis proved that continents are not moving above the ocean floor. Rather, it is the fragments of the lithosphere. The lithosphere is the rigid layer that is composed of the uppermost mantle and the crust that carry the continents and the ocean basins along. These fragments of the lithosphere are called plates. Underneath the lithosphere is a weaker region in the mantle known as asthenosphere that behaves like a fluid. Thus, the lithosphere floats above the asthenosphere, making it detached and free to move. This became the basis of the theory of plate tectonics. Now that it has been made clear that it is the plates which are moving, the question as to how they move remained. Sir Arthur Holmes proposed the driving force for this plate movement in 1919. He suggested that the movement in the mantle carries the plates along. It was previously discussed that Earth's interior is very hot due to the heat produced by radioactive decay. Convection takes place in the mantle, keeping the asthenosphere hot and weak. The convection currents produced in the asthenosphere are the ones carrying the lithospheric plates and making them move. However, convection currents are not enough. Mechanisms such as ridge push and slab pull aid the convection currents to slowly move the lithospheric plates. Ridge push occurs at mid ocean ridges which are higher in elevation than the surrounding trenches and abyssal plains. The new ocean floor from the ridge is hot and relatively thin. As it moves away from the ridge, it cools down and gets denser, heavier, and thicker. Below this cooling ocean floor is the asthenosphere, which is less dense. This area becomes a massive shear zone and the new ocean floor will effectively slide down the slope of the asthenosphere. When the plate collides with another plate with lesser density, the denser plate sinks and a subduction zone is formed. When the subducting plate sinks, it pulls on the rest of the plate behind it. These mechanisms explain the movement of the plates.Earth has seven major lithospheric plates that account for 94% of Earth's surface. These are the North American Plate, South American Plate, Pacific Plate, African Plate, Eurasian Plate, Indo-Australian Plate, and Antarctic Plate. These plates are constantly moving relative to the other plates. Thus, the interaction of plates occurs mostly along the boundaries. These movements are plotted using information from earthquakes and volcanic activities. There are three main types of plate boundaries: convergent, divergent, and transform boundaries Convergent boundaries are boundaries where two plates move towards each other A convergent boundary is also known as destructive margin since this is where the collision between two plates occhins. There are three types of convergence-oceanic oceanic, oceanic-continental, and continental-continental. Trenches are features of the ocean floor that are present in both oceanic-oceanic boundary and oceanic-continental boundary. Subduction occurs at the trenches, therefore, these are characterized as the deepest parts of Earth. A divergent boundary is the opposite of convergent boundary: two plates move away from each other. Divergent boundaries create new crust; thus, they are also known as constructive margins. The ocean ridge system is a divergent boundary where new ocean floor is produced as magma rises, pushing the older rocks aside.Transform boundary is also known as conservative plate margin since two plates just move past one another, neither creating nor destroying land. Earthquake epicenters are usually detected at transform boundaries because the rocks tend to break and not fold or sink, like in convergent boundaries. Evolution of the Ocean Basins. Both the movement of the plates and seafloor are responsible for the evolution of ocean basins. Along the divergent boundary where ocean ridge systems are found, magma is released and new ocean floor is created. Along convergent boundaries, the ocean floor is being destroyed. The evolution of the ocean basins started during the time when Pangaea was still present and was surrounded by the vast ocean or superocean known as Panthalassa, also called Paleo-Pacific or "old Pacific." Upon the initial break up of Pangaea into Laurasia and Gondwanaland, the Tethys Sea began to form. Then, the Eurasian and North about, forming the North Atlantic. The South Atlantic only started to form when the African Plate and South American Plate separated. The continued movement of the plates created the Himalayas at one side and separated the Pacific Ocean and Atlantic Ocean at the other side, which consequently formed the current ocean basins. Both the movement of the plates and seafloor are responsible for the evolution of ocean basins. Along the divergent boundary where ocean ridge systems are found, magma is released and new ocean floor is created. Along convergent boundaries, the ocean floor is being destroyed. The evolution of the ocean basins started during the time when Pangaea was still present and was surrounded by the vast ocean or superocean known as Panthalassa, also called Paleo-Pacific or "old Pacific." Upon the initial break up of Pangaea into Laurasia and Gondwanaland, the Tethys Sea began to form. Then, the Eurasian and North about, forming the North Atlantic. The South Atlantic only started to form when the African Plate and South American Plate separated. The continued movement of the plates created the Himalayas at one side and separated the Pacific Ocean and Atlantic Ocean at the other side, which consequently formed the current ocean basins.Continents do not immediately end at the point where the ocean meets the land. They may extend slightly into the oceans. The portion of the continent that is submerged is called continental margin. There are two types of continental margin: passive margin and active margin. A passive continental margin consists of a continental shelf, continental slope, and continental rise. It is not associated with plate boundaries; thus, there are very little tectonic activities. An active continental margin only has a continental shelf and a continental slope. It is associated with plate boundaries; thus, a main feature of this boundary is a trench. The different features of a continental margin are the following: 1. The continental shelf is the gently-sloping submerged portion of the continent. 2. The continental slope is the steep slope after the continental shelf. It is still part of the continent. 3. The continental rise is the gently-sloping area after the continental slope and before the ocean floor. 4. The trenches are the deepest parts of the ocean. These are narrow depressions caused by the subduction of the ocean floor along the convergent boundaries. 5. The mid-oceanic ridge is the mountain range system in the ocean. It is responsible for the production of new ocean floor. This is the region where new magma constantly emerges from. SCIENCE CAREER. A scientific illustrator uses art to inform and communicate complex details and concepts of science. He/She makes use of scientifically informed observations and research along with his/her technical art and aesthetic skills to make accurate representations. In Natural History, the scientific illustrators recreate how the extinct species look like by working with scientists and fossil records. Moreover, with the advances in technology, illustrators are now into 3D modelling, animation, and video making. Earth's History. All the processes that have been discussed require long periods of time to create a noticeable change on Earth's surface. You can just imagine how long it would take to create an oceanas vast as the Pacific Ocean if the ocean floor moves only at about 10 cm/year. It is then important to know the history of Earth to learn the complexities of its past and be able to use it to understand the present. Just like learning the history of a country that requires one to read a lot of books, learning the history of Earth involves studying a lot of rocks. Rocks, especially sedimentary rocks, contain a lot of information about Earth's past. It holds the key to most of the geologic processes that happened on Earth and the key to uncovering how life on Earth evolved. But these discoveries are worthless if there is no time perspective. Thus, one of the most important contributions of geologists to mankind is the geologic time scale, which holds a history that is exceedingly long.There are two numbers you need to know about climate change. The first is 51 billion. The other is zero. Fifty-one billion is how many tons of greenhouse gases the world typically adds to the atmosphere every year. This is where we are today. Zero is what we need to aim for. To stop the warming and avoid the worst effects of climate change, humans need to stop adding greenhouse gases to the atmosphere. This sounds difficult, because it will be. Every country will need to change its ways. Virtually every activity in modern life – growing things, making things, getting around from place to place – involves releasing greenhouse gases, and as time goes on, more people will be living this modern lifestyle. That’s good, because it means their lives are getting better. Yet if nothing else changes, the world will keep producing greenhouse gases, climate change will keep getting worse, and the impact on humans will be catastrophic. But “if nothing else changes” is a big If. I believe that things can change. We already have some of the tools we need, and as for those we don’t yet have, we can not only invent, but also deploy them, and, if we act fast enough, avoid a climate catastrophe. Two decades ago, I would never have predicted that one day I would be talking in public about climate change. My background is in software, not climate science. Things changed for me when I met with two former Microsoft colleagues who were starting non-profits focused on energy and climate. They brought along two climate experts who were well versed in the issues, and the four of them showed me the data connecting greenhouse gas emissions to climate change. I kept learning everything I could about climate and energy, agriculture, oceans, sea levels, glaciers, power lines, and more. One thing that became clear to me was that our current sources of renewable energy – wind and solar, mostly – could make a big dent in the problem, but we weren’t doing enough to deploy them. It also became clear why, on their own, they aren’t enough to get us all the way to zero. The wind doesn’t always blow and the sun doesn’t always shine. Within a few years, I had become convinced of three things: 1. To avoid a climate disaster, we have to get to zero. 2. We need to deploy the tools we already have, like solar and wind, faster and smarter. 3. We need to create breakthrough technologies that can take us the rest of the way.The price of electricity has risen (1) ______ over the last year. A) specially | B) obviously | C) significantly | D) remarkably The heavy rain led to floods, (2) ______ a lot of trouble for local farmers. A) causing | B) making | C) resulting | D) affecting I have never seen (3) ______ a beautiful sunset in my entire life! A) as | B) like | C) so | D) such It is very (4) ______ that some people still don't believe in climate change. A) doubtful | B) suspicious | C) worrying | D) uncertain My brother is learning how to (5) ______ a small business. A) adjust | B) run | C) manage | D) direct Can you (6) ______ the person who took your bag? A) inform | B) identify | C) tell | D) know On a daily (7) ______, we should try to use less plastic. A) basis | B) motive | C) cause | D) method Regular exercise and a healthy diet are very (8) ______ for your heart. A) rewarding | B) valuable | C) beneficial | D) productive She was (9) ______ to win the race, so she practiced every single day. A) fixed | B) decided | C) committed | D) determined An (10) ______ student spends about three hours on homework every evening. A) everyday | B) average | C) normal | D) regularSlide 1 Growing Up in the 21st Century: Challenges and Opportunities Slide 2 Introduction: What Does It Mean to Grow Up? • Growing up: The process of maturing physically, mentally, and emotionally • Transition from childhood to adulthood • Unique challenges and opportunities in the 21st century • Importance of mental growth alongside physical development Slide 3 The Journey of Self-Discovery • Exploring personal identity • Understanding values and beliefs • Developing a sense of purpose • Embracing individuality while finding community Slide 4 Mental Growth: A Key Aspect of Maturity • Emotional intelligence and self-awareness • Critical thinking and problem-solving skills • Adaptability and resilience • Importance of continuous learning and personal development Slide 5 Challenges of Growing Up in the Digital Age • Information overload and digital literacy • Social media pressure and online identity • Cyberbullying and online safety • Balancing screen time with real-life experiences Slide 6 21st Century Skills for Success • Technological proficiency • Communication and collaboration • Creativity and innovation • Global awareness and cultural competence Slide 7 Navigating Relationships in a Connected World • Building and maintaining friendships • Romantic relationships in the digital era • Family dynamics and independence • Professional networking and mentorship Slide 8 Education and Career Pathways • Evolving job market and emerging industries • Importance of lifelong learning • Balancing academic success with practical skills • Exploring unconventional career paths Slide 9 Financial Literacy and Independence • Understanding personal finance • Budgeting and saving strategies • Student loans and debt management • Investing for the future Slide 10 Mental Health and Well-being • Recognizing and managing stress • Importance of self-care and work-life balance • Seeking help and support when needed • Destigmatizing mental health issues Slide 11 Physical Health in a Changing World • Importance of regular exercise • Nutrition and healthy eating habits • Sleep hygiene and its impact on well-being • Avoiding harmful substances and addictive behaviors Slide 12 Environmental Awareness and Sustainability • Understanding climate change and its impacts • Developing eco-friendly habits • Participating in community environmental initiatives • Sustainable career opportunities Slide 13 Civic Engagement and Social Responsibility • Understanding political systems and processes • Importance of voting and civic participation • Volunteering and community service • Advocating for social justice and equality Slide 14 Cultural Competence in a Global Society • Appreciating diversity and inclusion • Developing intercultural communication skills • Opportunities for travel and cultural exchange • Embracing multilingualism Slide 15 Time Management and Productivity • Setting goals and priorities • Effective study and work habits • Balancing academics, extracurriculars, and personal life • Avoiding procrastination and developing discipline Slide 16 Dealing with Failure and Setbacks • Reframing failure as a learning opportunity • Building resilience and grit • Developing a growth mindset • Seeking feedback and continuous improvement Slide 17 Technology and Ethics • Understanding digital footprint and online reputation • Responsible use of social media and technology • Privacy concerns and data protection • Ethical considerations in a tech-driven worldclimate change110.31.b.17.C Topic: Reading/Vocabulary DevelopmentSTAAR English II High School 2014 - Past Paper