Plate Tectonics Alfred Wegener and his theory of Continental Drift along with evidence. Harry Hess and his theory of Seafloor Spreading Continental Drift + Seafloor Spreading = Plate Tectonics Poster/handout and students notes/activity/research page Plate Boundaries Convergent, Divergent, and Trans...
Learn about plate tectonics using an orange. This hands on activity is a great introduction to plat boundaries and tectonics for kids
Plate tectonics is a revolutionary theory on a par with modern genetics. Yet, apart from the frequent use of cliches such as 'tectonic shift' by economists, journalists, and politicians, the science itself is rarely mentioned and poorly understood. This book explains modern plate tectonics in a non-technical manner, showing not only how it accounts for phenomena such as great earthquakes, tsunamis, and volcanic eruptions, but also how it controls conditions at the Earth's surface, including global geography and climate. The book presents the advances that have been made since the establishment of plate tectonics in the 1960s, highlighting, on the 50th anniversary of the theory, the contributions of a small number of scientists who have never been widely recognized for their discoveries. Beginning with the publication of a short article in Nature by Vine and Matthews, the book traces the development of plate tectonics through two generations of the theory. First generation plate tectonics covers the exciting scientific revolution of the 1960s and 1970s, its heroes and its villains. The second generation includes the rapid expansions in sonar, satellite, and seismic technologies during the 1980s and 1990s that provided a truly global view of the plates and their motions, and an appreciation of the role of the plates within the Earth 'system'. The final chapter bring us to the cutting edge of the science, and the latest results from studies using technologies such as seismic tomography and high-pressure mineral physics to probe the deep interior. Ultimately, the book leads to the startling conclusion that, without plate tectonics, the Earth would be as lifeless as Venus. 84 figures/illustrations
Harry Hammond Hess poster print. Crafted from museum-quality, crease-resistant matte paper, this poster is built to last - just like the lasting impact Harry Hammond Hess had on history.It's more than just a decorative piece - it's a compliment magnet that starts conversations like wildfire! Bold and imposing, this print instantly transforms the look of a room. The satisfyingly sturdy paper is equally at home in or out of a frame, and you'll quickly get used to hearing 'where did you get that?'Whether it adorns a classroom wall, personal study, living room or office, it also packs some serious educational value. As a captivating reminder of the story that Harry Hammond Hess represents, it piques curiosity and inspires deeper learning.Like all our home decor, your print is carefully packaged to ensure it arrives in pristine condition, ready to captivate and inspire. And if you have any questions, comments or suggestions? We're a small friendly team, and we're just a message away!
We are in Unit 4-7 of Layers of Learning and today's science lesson was on plate tectonics. We do science once a week, usually on Tuesday or Wednesday . . .
Plate tectonics and continental drift theory Plate tectonics was born in 1968 in the form of a theory of the evolution of ...
Introduce your students to one of the most influential and important geologists of all time! Alfred Wegener named Pangea and provided evidence of continental drift, which became the foundation of the theory of plate tectonics. Both print and Google Slides options to assign are included. In this activity, students will: READ an engaging biography about Wegener, his adventurous spirit, his evidence of continental drift, and how his ideas were initially dismissed. ANSWER text-dependent questions based on the article. No prior knowledge is required! Teacher Notes: This resource is not editable. An answer key is included. A link to the Google Slides version of this activity is included with purchase. ⭐ Let us send you TONS of FREE Grades 7-12 Science activities to try! ⭐
Quiz – Plate Tectonics, Weathering, Erosion, Deposition This quiz reviews the theory of plate tectonics, plate boundaries and the geological events that happen at each, as well as the processes of weathering, erosion, and deposition. Students are expected to know about divergent, convergent, and transform boundaries, chemical and physical weathering, the agents of erosion, and landforms that are caused by deposition. The quiz contains multiple choice, matching, and short-answer questions. This quiz is fully editable and includes an answer key. ***************************************************************************** You May Also Like… Layers of the Earth Lesson Describing Minerals Worksheet Describing Igneous Rocks Worksheet Describing Igneous Rocks PowerPoint (Or get the bundle… Describing Igneous Rocks Bundle) Describing Sedimentary Rocks Worksheet Describing Sedimentary Rocks PowerPoint (Or get the bundle… Describing Sedimentary Rocks Bundle) Describing Metamorphic Rocks Worksheet Describing Metamorphic Rocks PowerPoint (Or get the bundle… Describing Metamorphic Rocks Bundle) If you’re interested in all my rock products, get the complete bundle! Describing Igneous, Sedimentary, and Metamorphic Rocks PowerPoint ***************************************************************************** Customer Tips:How to get TPT credit to use on future purchases: • Please go to your My Purchases page (you may need to login). Beside each purchase you'll see a Provide Feedback button. Simply click it and you will be taken to a page where you can give a quick rating and leave a short comment for the product. Each time you give feedback, TPT gives you feedback credits that you use to lower the cost of your future purchases. I value your feedback greatly as it helps me determine which products are most valuable for your classroom so I can create more for you. ☺ Be the first to know about my new discounts, freebies and product launches: • Look for the green star next to my store logo and click it to become a follower. Voila! You will now receive email updates about this store. ☺ *****************************************************************************
The main difference between plate tectonics and continental drift is that plate tectonics describes the features and movement of Earth’s surface in the past
Tectonic plates have created some of the most astonishing geologic creations on earth. Read more about the History, Theory, and Definition...
Lemuria The continent of Lemuria, though largely discounted by the theory of plate tectonics and the existence of other sunken continents still visible on the silty bottom of many oceans, lives on in people’s dreams. The Native American Indians have been said to be descendants of the Lemurians, as are certain tribes in Turkey, the
Introduce the theory of plate tectonics with evidence from earthquakes and volcanoes! In this quest, your students must help Lady Ada Lovelace from the game world of Aureus Imperium uncover the link that exists with the location of earthquakes, volcanoes and plate boundaries! Students are given the coordinates of a series of major earthquakes and famous volcanoes on planet Earth. They use the latitude and longitude coordinates and plot these locations on a world map. Students then draw the edges of the major tectonic plates on their maps to discover the pattern that exists between earthquakes, volcanoes, and tectonic plates. As an extension, challenge your students with eight scenario cards where they must judge the earthquake and volcano risk based on the location's proximity to the edge of the plates. This activity is a great review of the importance of map skills and provides strong evidence in support of the theory of plate tectonics. It is the perfect lesson to follow-up your Earth layers and seismic wave lessons! Students will be able to demonstrate skills related to these learning targets: -I can compare world maps of earthquakes and volcanoes to a map of plate boundaries. - I can explain that Earth’s crust consists of major and minor tectonic plates. Within this download you will get a suggested lesson plan, the student quest handouts, plotting and plate map reference sheets, eight earthquake and volcano scenario cards, and answer key! This activity can be easily assigned for "distance-learning" or "at-home learning." For more engaging Earth science seismic wave activities, pair this with: Quest- Desert of the Deathworm! Quest- Alert Cindermill Quest- Evacuate Cindermill, A Seismic Wave and Earth Layers Activity Quest- The Evolving Landscape- A Pair of Plate Boundary Graphing Activities Quest- Hunting Earthquakes, A Current-Event Earthquake Plotting Activity Copyright © 2020 Daniel Hellmund, Hellmund Science All rights reserved by author. Permission to copy for classroom use only. Electronic distribution limited to classroom use only. Don't forget to follow us by clicking the little green star under our store name! Leaving feedback grants you TPT credits for future purchases! Hellmund Science offers a variety of gamified science labs, notes, projects and games with Universal Design for Learning (UDL) and Project-Based Learning in mind. Gamification allows for Positive Behavioral Intervention Support as well as differentiation. Using this format, students learn to work together and choose the path of their liking to learn various learning targets. Your students will play to learn!
Tectonic plates, large slabs of rock that divide Earth’s crust, move constantly to reshape the Earth’s landscape. The system of ideas behind plate tectonics theory suggests that Earth's outer shell (lithosphere) is divided into several plates that glide over the Earth’s rocky inner layer above the soft core (mantle). The plates act like a hard and rigid shell compared to Earth's mantle. The mantle sits between Earth's dense, very hot core and its thin outer layer, the crust. Plate tectonics has become the unifying theory of geology. It explains the earth’s surface movement, current and past, which has created the tallest mountain ranges and the deepest oceans.
Earth's first continents may have formed close to the planet's surface, oozing out from the crust instead of boiling up from the mantle as was thought.
At the end of this continental drift theory lesson plan, students will be able to describe the historical developments that support the plate tectonic
Geologic Change Over Time Fossils Florida BEST 6th Grade Science SC.7.E.6.4 is great for teaching about uniformitarianism, Florida fossils, fossil formation, types of fossilization, the principle of fossil succession, the Continental Drift Theory, the Plate Tectonics Theory and so much MORE! This resource includes: Learning Objectives KWL Chart Modern Geology Reading Florida Fossils Reading Types of Fossils and Fossilization (per-mineralization, carbonization, molds and casts, replacement, and amber) Extension Resources The Principle of Fossil Succession Reading Continents on the Move Reading New Vocabulary Activities Show What You Know Post Lesson Questions Post Lesson Quiz & Answer Key This resource is great for: Teaching about fossils Science centers Independent work Distance learning, eLearning At home learning, homework Test prep Assessment Here’s what teachers just like you are saying about this resource: ⭐️⭐️⭐️⭐️⭐️ Marta B. says, "Very helpful resource for hands-on learning. Made the student more interested in learning." ⭐️⭐️⭐️⭐️⭐️ Robin T. says, "Just what I needed!" Similar Resources: Rock Cycle - Science - Pdf & Nearpod Lesson - Google Classroom Ready Renewable and Non-Renewable Energy - Pdf & Nearpod Lesson Weathering and Erosion - Lesson - Pdf & Nearpod Lesson Formats ************************************************************************************* • Be sure to follow my store to be alerted of new products >> click here • Don't forget to leave feedback . You will receive TPT credits to be used towards future purchases! Have Fun Teaching! Mrs. Lena M. Ed.
heat and pressure is applied to the rock and it becomes a metamorphic rock.
This is a 4-page test that assesses students understanding of ALL components of the Next Generation Science Standard (next gen) MS-ESS2-3 which covers the theory of plate tectonics and continental drift. The assessment is designed to allow students to express their understanding of the standard through multiple modalities/learning styles. The assessment is both highly accurate and reliable. The assessment is designed to mirror the performance tasks students will be presented with on the end of year state science test. There are four sections to the test which include: 1. Label the Model - Students label the plate boundaries using the words from the word bank. 2. Short Response - Students explain how the evidence in the provided image supports the theory of continental drift. 3. Fill in the Blanks - Students complete each sentence with the appropriate word. 4. Image Analysis - Students analyze the image of Pangaea and answer comprehension questions.
Plate tectonics and continental drift theory Plate tectonics was born in 1968 in the form of a theory of the evolution of the Earth's surface as a whole, hence the name given to it often global tectonics. Based on geophysical approach, it has since been the subject of numerous checks that have made it a widely accepted theory, making obsolete all other theories orogenic, or at least reducing the explanation of partial processes (for example, the gravitational slip of cover tectonics). Plate tectonics resumes continental drift , as it was designed by Alfred Wegener (1912) and as it was abandoned for nearly fifty years under the blows of momentary geophysical arguments, despite the favor she continued enjoy in some tectoniciens, including Emile Argand (1922) was the leader and Alexander L. Du Toit (1937) one of the representatives. But it goes much further than Wegener's ideas - it is not a mere repetition - by providing them a framework and specific geophysical mechanisms persuasive impact is generally applicable to all Earth Sciences . 1. Continental drift: The first idea that came to mind is that geologists stability of continents and oceans, following the conventional wisdom that gives firmness to the rock eternal. He belonged to Wegener, a book remained famous for the ideas he has planted and the controversy it has raised (Die Entstehung und der Kontinente Ozeane, 1915), to draw attention to the possibility of moving continents, he gave many arguments, especially orders morphological, stratigraphic, tectonic and paleontological. - Arguments morphology. Some continents fit easily into one another, like South America and Africa, in addition, this fitting is done, there is continuity of land and structures across the continental limits current. This allowed Wegener continents gather at the end of Primary, a single Pangea he opposed a Panthalassa. - Arguments stratigraphic. Parts of continents today disjoint sets demonstrate very similar: thus will he for South America, Africa, Madagascar, India and Australia, whose Permo-Triassic series are surprisingly similar, where the idea was born of a Gondwanaland fragmented thereafter. In the same vein, the gathering of Carboniferous glacial deposits on the one hand, and coal deposits of the same period, on the other, is an argument in favor of Pangaea in the late time primary. - Arguments tectonics. The arguments concerning the obvious tectonic shortening corresponding to the formation of mountain ranges, without that there is discontinuity between the buildings. Rather than a general contraction of the crust, you can use a combination of two fragments of it, so was born the concept of the genesis of the Alps by a rapprochement between the European continent and North Africa in South. - Arguments paleontology. Paleontological arguments reside in the observation of similarities in faunas continents now separated: thus, in Gondwana, meet at the Permo-Triassic, the same flora and Gangamopteris Glossopteris and the same faunas Reptiles theromorphs. One can of course imagine "intercontinental bridges" now submerged. Such bridges still exist today, so the Isthmus of Suez, Pliocene connected Africa and Eurasia and has, since that time, numerous fauna passages (eg, camels, Asian, invaded Africa), so the Isthmus of Panama, which was completed in the Pliocene, has also many passages of faunas between North America and South America (even today , armadillo, native to South America, invaded North America). But must still prove the existence of such intercontinental bridges the times when they were needed, and should, in addition, comply with what we now know of the nature of the seabed, many bridges are supposed and sentenced faunas have not made their migration to the oceanic crust ... The hypothesis of fragmentation of a formerly single landmass and the relative displacement of different parts was more convincing. Wegener thought that the continents sialic (of sial, silicon and aluminum, the major constituents of the surface of the continents) as rafts drifting on the underlying sima (silicon and magnesium, major constituents of the ocean floor), due the Earth's rotation. The shape of the Earth is a sphere, the continents were thus derive both westward (to delay the rotation) to the equator (axifuge effect). This explained simply double orientation orogenic belts, latitudinal (or Tethyan belt mésogéenne) or longitudinal (waist circum). At the front of the continents grew by mountain ranges "bow effect" (American Cordillera) and the back had instead of "releases" of island arcs by "Stern effect" (Asian island arcs) realized that a simple asymmetry of the Pacific; reconciliation and collision of continents from the Angara and Gondwana (Eurasia and all African-Arab-Indian) gave birth to the alpine ranges of Eurasia. Wegener's theory was thus a harmonious and coherent. There were some imperfections in detail: for example, the Americas had a bow but not stern, Eurasia had a stern but not bow; while Africa had neither the one nor the other . But it did not affect much the overall pattern, which appeared as the first version of the geology of the overall surface of the Earth and, as such, was a great success. This theory, however, was rejected, probably because it allowed excess: too many continents were moved to the needs of a beetle or cave fauna such ... It was especially set aside for lack of geophysical foundations, at least in the context of knowledge of the time. Thus, Wegener would measure the relative displacement current continents (between Greenland and Scandinavia), but unfortunately the scale of displacement he wanted to highlight - very overrated though - was equal to or less than the magnitude of simple errors calculation, given the methods he used. In addition, geophysicists showed that the continents could move through simple inertia forces associated with the rotation of the Earth. Wegener's theory therefore fell under the blows of geophysics. Yet it is the latter which would revive: paleomagnetism should prove continental drift [cf. GEOMAGNETISM]. Thus we have been able to reconstruct the positions of the continents over time and show that they formed a unique well at the end of the primary, and virtually overlapping pattern Wegener. In the 1950s, continental drift had regained his credit. But it was still unable to describe how to find and the engine. The seafloor spreading and plate tectonics would answer these two questions in turn. 2. The seafloor spreading: The hypothesis of seafloor spreading was issued by Harry H. Hess (1960-1962) from the one hand, the shape of the mid-ocean ridges with their extensive rift median aspect, on the other hand, the existence of plans seismic discovered before World War II by the Japanese geophysicist Kiyoo Wadati, then rediscovered later by the American seismologist Hugo Benioff, whose name they bear (cf. sUBDUCTION, fig. 1). These plans Benioff dive to the outside of the Pacific bordiers continents or island arcs. It was as if, as a result of double convection across the Pacific upper mantle, ascending at the median rift, descending at plans Benioff, gave birth to the oceanic crust in the first case, and "digest" in the second. Such an assumption could not rely on the certainty of a difference in kind between the continental crust and the oceanic crust, which was demonstrated by geophysics. The recording of the first wave of earthquakes relatives, who walk in depth, showed different propagation speeds in the one and the other: respectively 5.6 and 6.5 km / s for longitudinal waves, 3, 3 and 3.7 km / s for transverse waves, speeds were compared with experimental measurements in granites and basalts. Hence, in a first time, the concept of continental crust "granite" and oceanic crust "basaltic". Distinction did confirm that the records of distant earthquakes longwave whose spokes pilgrim way in surface: these waves are "ahead" after crossing an ocean compared to the equivalent of crossing a continent This confirms that the oceanic crust is "faster" than the continental crust. "Granitic" and "basaltic" are obviously references averages. For the continental crust that covers the whole formed by the sedimentary cover, metamorphic rocks (gneiss, mica) and granites themselves. Outcrops and boreholes show, including deep drilling undertaken in the Kola Peninsula (Russia), which reached more than 12,200 meters in the early 1990s. For the oceanic crust that covers a stratified (top to bottom) of basalts, dolerites in veins or dykes complex, gabbros, cumulate peridotites, in a structure similar to that of the ophiolite massifs of the Alpine chains, considered fragments crust and upper mantle ocean swept along on the continents. Dredging in the oceans have raised these types of rock drilling have met, including that of the well 504 B program IPOD (International Program for Ocean Drilling) which, off Costa Rica, in 4000 meters of water and 400 meters of sediment, crossed almost 1,200 meters of ocean crust basalts with dolerite and gabbros (the well remains open for deeper future). Campaigns submersible dives - with American Alvin, the Nautilus Cyana and French - have recognized basalts (campaigns FAMOUS - French-American Mid-Oceanic Undersea Survey - on the Mid-Atlantic Ridge, Cyamex - Cyana of Mexico and - the ride is peaceful) or deeper words, gabbros and peridotites (Cyagor campaigns on the bench Goringe, south-west of Portugal, and Vemanaut Kanaut along the Vema transform faults in the South Atlantic and Kane, in the central Atlantic). The dual nature of continental and oceanic crust is therefore no longer in doubt. The discovery and interpretation of magnetic anomalies at mid-ocean ridges would lead to justify the notion of expansion at the median rifts. This discovery was made by Ronald G. Mason (1958) in the Pacific west coast of North America, it was quickly confirmed and extended to other oceans, including the Atlantic Ocean at the Reykjanes Ridge, south of the Iceland, which is the northern part of the Mid-Atlantic Ridge. These anomalies were interpreted by Frederick J. Vine and Drummond H. Matthews (1963), taking into account palaeomagnetical thermorémanent: bands magnetic anomaly, rift in parallel and symmetrical with respect thereto were interpreted as being due to many successive intrusions from basic material of the mantle, while each the paleomagnetic field was the same direction as the current field (positive anomalies: the thermoremanent magnetic component is added to the current field), while the other paleomagnetic field was opposite to that of the current (negative anomalies: the paleomagnetic thermoremanent component is subtracted from the current field). This being admitted, we can then, depending on the calendar used paleomagnetic, assign an age to each band of magnetic anomalies, thus showing that the deep ocean is more ancient, as one moves away from Median rift. There arise where these cards, along with rifts, identifies key anomalies identified by their serial number in a fixed schedule or even their absolute age from the calendar. At the same time, the calculation of the rate of expansion - indeed half-rate because the phenomenon is valid on both sides of the ride - is made possible by simply dividing the distance a band rift anomalies by age it: values obtained range up to a maximum of 17 to 18 centimeters per year at the East Pacific Ridge in the north-equatorial. The most frequent value, especially in the Atlantic, is about 2 centimeters per year. The analysis of earthquakes occurring at mid-ocean ridges clarified the terms of the hypothesis. This is John Tuzo Wilson (1965) noted that the seismic characteristics of the major accidents to cross mid-ocean ridges. If they were real setbacks, we should expect that households have seismic over the entire length of these accidents. But it is not so: the seismic foci have only the section of the accident between the two offset portions of the rift. If, instead, we consider that these accidents, shift away from a rift preformed are created by the same process as that one, we get a very different result: the rate of seafloor spreading is assumed the same on both sides of the accident, we immediately see that, between the two offset rift, the direction of relative movement of the oceanic crust is opposite to that of the apparent setback, while beyond the rifts, the game equal rate of expansion oceanic crust movement is in the same direction and the same speed of both sides of the accident, which thus can be considered dead. We understand that the only seismic foci are located between the rifts. These accidents were designed and called transform faults by J. T. Wilson, to distinguish them from setbacks. Lynn R. Sykes (1967) was to undertake the verification of this fact by a new analysis of earthquake foci mechanism to mid-ocean. If we accept that an earthquake at the hypocenter is caused by a sudden rupture along a fault, the stress state corresponding to this failure can be divided into four quadrants, two compression and two expansion, these two situations by expressing the meaning of the first movement and the overall result of it. If so, on the occasion of a given earthquake, we took stock of the meaning of the first movements in different seismological stations distributed throughout the world (using P waves arriving early), they must be divided into four quadrants separated by two large circles perpendicular to each other, such that, in pairs, one can observe one. However, this result does not mean, reversing the reasoning to determine the cause of the fault and earthquake motion. If you do not know the fault that causes the earthquake, there is an uncertainty of 900 in the possible direction of this: we can not choose between the two families combined with a network of faults and, by consequently, we can not determine the motion. But if you know the cause of the earthquake fault - so if you know which case 7 b and 7 c is good - we can determine the motion along it. L. R. Sykes applied to earthquakes so this method of mid-ocean ridges, considering that they occurred along transform faults, and thus confirmed that they correspond to a reverse movement of the apparent setback, which was the assumption of J . T. Wilson.
We are in Unit 4-7 of Layers of Learning and today's science lesson was on plate tectonics. We do science once a week, usually on Tuesday or Wednesday . . .
Explore the patterns and relationships among the locations of tectonic plate boundaries, mountain ranges, volcanoes, and earthquakes on the planet. Use this resource to visualize data and provide opportunities to develop and use models.
A plate tectonics unit needs to be engaging! This post features 7 ways to get your students engaged in plate boundaries and continental drift.
⭐ ⭐ ⭐ ⭐ This resource is a compilation of bell ringers or daily quizzes to start off or end each class period for your plate tectonics unit. It includes 20 days worth of assessment questions covering plate boundaries, Pangaea, types of crust, geologic features at plate boundaries, sea-floor spreading, and more! It is my favorite way to engage students at the beginning of each class! ⭐ How can I use this? • As a bell ringer or warm up to get students settled and ready for class to begin • As a daily quiz or formative to assess students each day • As an exit slip or ticket out the door to check for understanding at the end of class • As a gallery walk to get kids up and moving to review material learned in class ⭐ What is included? • 20 PowerPoint slides each with different questions or activities to project on your classroom screen. • 2 20-Page PDF versions (black/white and full color versions) • Student Response Sheet (editable and PDF versions) • Answer Key (PDF and also answers are located in the notes section of each slide in the PowerPoint) •Teacher Guide and Overview • Smaller format of all bell ringers (all 20 activities on 2-page PDF) - perfect for absent students • Editable Card Templates ⭐What topics are covered? • Theory of Plate Tectonics • Plate Boundaries • Interactions at Plate Boundaries • Geologic Features at Plate Boundaries • Sea-Floor Spreading • Pangaea • Continental Drift • Types and Characteristics of Crust ⭐ What is special about this? • These are not numbered. Instead they each are given a letter. That way you don't have to present them in order. This is very important to me because I do not always use all the activities, want to add cards, or different classes are at different points in the unit. The answer key corresponds to letters, not numbers, so you can switch it up without confusing your students. • You can use these in tons of ways! - Bell ringers, exit tickets, gallery walk, test review, task cards, stations, partner work, distance learning, formative assessment, and more! • Beautiful graphics, clear formatting, and lots of science diagrams! • Variety of Activities - Students won't get bored of the same style every day! Multiple choice, T/F, Venn Diagrams, Labeling Diagram, Fill-in-Blanks, Short Answer, etc. •Template Cards and Editable Student Answer Sheets Included Click on the Preview to Learn More! **************************************************************** ❤️CLICK TO FOLLOW SCIENCE IS REAL! ❤️ Get Alerted to New Products, Sales, Discounts, and Freebies! HAPPY SCIENCING! Science Is Real! Terms of Use (TOU): By purchasing this product, you own a license for one teacher only for personal use in their own classroom. Licenses are non-transferable and therefore cannot be passed from one teacher to another. If the teacher who purchased this license leaves the classroom or changes schools, the license and materials leave with that teacher. No part of this resource is to be shared with colleagues or used by an entire team, grade level, school or district without purchasing the correct number of licenses. If you are a coach, principal or district interested in transferable licenses that would accommodate yearly staff changes, please contact me for a transferable license quote at [email protected]. Copyright by Science is Real. Please note - all material included in this resource belongs to Ana Catts. By purchasing, you have a license to use the material, but you do not own the material. You may not upload any portion of this resource to the internet in any format, including school/personal websites or network drives unless the site is password protected and can only be accessed by students, notother teachers or anyone else on the internet. * Graphics by (c) The Painted Crow and (c) Sarah Pecorino ❤️ CHECK OUT MORE GREAT THINGS FROM SCIENCE IS REAL! ❤️ ⭐ Plate Tectonics Graphic Organizer w/ Reference Sheets & Key! ⭐ Plate Tectonics Boom Cards - Digital Task Cards - Distance Learning ⭐ Plate Tectonics Assessment-Test Question Bank & Pre-Made EDITABLE Assessments ⭐ Plate Tectonics Webquest - Digital & Printable ⭐ Plate Tectonics PowerPoint with Student Notes, and Kahoot! - Digital & Printable ⭐ Plate Tectonics with Continental Drift Growing Bundle ⭐ Continental Drift Assessment-Test Question Bank & Pre-Made EDITABLE Assessments ⭐ Continental Drift PowerPoint with Student Notes & Kahoot! Digital & Printable ⭐ Earthquakes Graphic Organizer - Distance Learning ⭐ Earthquakes PowerPoint with Fill-in Notes, Comprehension Checks, and Kahoot ⭐ Earthquakes and Volcanoes Webquest - Google Slides, MS Word, and PDF Versions ⭐ Ring of Fire Mapping Activity and Questions - Earthquakes and Volcanoes
“The evolutionist thesis has become more stringently unthinkable than ever before.” (Wolfgang Smith Ph.D.) One of the dumbest theories linked to Evolution is the popularly held “P…
We are in Unit 4-7 of Layers of Learning and today's science lesson was on plate tectonics. We do science once a week, usually on Tuesday or Wednesday . . .
Our planet's outermost rigid layer, the lithosphere, is fractured into roughly 7 major and several minor tectonic plates that fit together l...
