Transcript: More WordArt to make your Powerpoint Interesting! New Transitions! More Layouts! More Colors and Themes! More Theme Styles! Bigger and Better Fonts! New Powerpoint Animations!! More Animations to choose from! Choose Better Shapes! More Text Styles!
Transcript: How does someone enter the Oracle? Religion Knowing that Unoka was weak helps us to understand why Okonkwo was ashamed and so determined to be better than his father. Being weak is not showing the right characteristics of a man. = The priestess said... "When a man is at peace with his gods and his ancestors, his harvest will be good or bad according to the strength of his arm." "The way into the shrine was a round hole at the side of a hill, just a little bigger than the round opening into a henhouse." Why might this be important to our understanding of Okonkwo's character? Unoka went to the Oracle of Agbala to find out why he always had a miserable harvest. Why did Unoka go to visit the Oracle of Agbala? What message does he receive?
Transcript: We are Egypt's SIFE National Champions ! Right ? Have you unleashed your full potential ? If this was our impact... Make a “date” with yourself .. You deserve to take “time out” to think. Think about your dreams – is there something you always WANTED to do? Get in touch with “yourself” - what are your talents, what fulfils you as a person and search for your passion! Take Actions Take Charge! Be proactive and positive. Face your challenges and fears. Learn everything you can, anytime you can, from anyone you can - there will always come a time when you will be grateful you did. Talk to others about opportunities and ideas. Opportunity seldom knocks twice. And Finally Balance your life aspects. Your Healthy life Your Social life Your Academic life Your Future careeer Development Apply for SIFE Leadership postitons & Unleash the full POTENTIALS SIFE Photo credits: 'horizon' by pierreyves @ flickr It could be much larger! But... 30 Cairo University Let me give you some tips .... This achievement is the result of the combined effort of each one of you. Grab Yours ! Just by Unleashing your full POTENTIAL....
Transcript: Seafloor spreading Sea-floor spreading is the process in which the ocean floor is extended when two plates move apart. As the plates move apart, the rocks break and form a crack between the plates. Earthquakes occur along the plate boundary. Magma rises through the cracks and seeps out onto the ocean floor like a long, thin, undersea volcano. As magma meets the water, it cools and solidifies, adding to the edges of the sideways-moving plates. As magma piles up along the crack, a long chain of mountains forms gradually on the ocean floor. This chain is called an oceanic ridge. The boundaries where the plates move apart are 'constructive' because new crust is being formed and added to the ocean floor. The ocean floor gradually extends and thus the size of these plates increases. As these plates get bigger, others become smaller as they melt back into the Earth in the process called subduction. The new rock at the edge has no sediments like the sand or mud, since it is formed only recently. Farther away from the ridge, sand and mud gradually settle on it, in an ever-thickening blanket. The oldest rocks may have 14,000 feet of sand and other sediments resting on top of it. An example of an oceanic ridge is the Mid-Atlantic Ridge. It is one part of a system of mid-oceanic ridges that stretches for 50,000 miles through the world's oceans. The underwater mountains of the ridge may not be more than two miles higher than the surrounding sea floor. Abundant evidence supports the major contentions of the seafloor-spreading theory. First, samples of the deep ocean floor show that basaltic oceanic crust and overlying sediment become progressively younger as the mid-ocean ridge is approached, and the sediment cover is thinner near the ridge. Second, the rock making up the ocean floor is considerably younger than the continents, with no samples found over 200 million years old, as contrasted with maximum ages of over 3 billion years for the continental rocks. This confirms that older ocean crust has been reabsorbed in ocean trench systems. By the mid-1960s studies of the earth's magnetic field showed a history of periodic reversals in polarity (see paleomagnetism). A timescale for “normal” and “reversed” polarity was established, showing 171 magnetic “flip-flops” in the past 76 million years. Magnetic surveys conducted near the mid-ocean ridge showed elongated patterns of normal and reversed polarity of the ocean floor in bands paralleling the rift and symmetrically distributed as mirror images on either side of it. The magnetic history of the earth is thus recorded in the spreading ocean floors as in a very slow magnetic tape recording, forming a continuous record of the movement of the ocean floors. Other supportive evidence has emerged from study of the fracture zones that offset the sections of the ridge. Sections in this article: Read more: seafloor spreading: Supporting Evidence for Seafloor Spreading — Infoplease.com http://www.infoplease.com/ce6/sci/A0860994.html#ixzz1ecWGFkw3 Plate tectonics (from the Late Latin tectonicus, from the Greek: τεκτονικός "pertaining to building") is a scientific theory that describes the large scale motions of Earth's lithosphere. The theory builds on the concepts of continental drift, developed during the first decades of the 20th century, and accepted by the majority of the geoscientific community when the concepts of seafloor spreading were developed in the late 1950s and early 1960s. The lithosphere is broken up into tectonic plates. In the case of the Earth, there are currently seven or eight major (depending on how they are defined) and many minor plates. The lithospheric plates ride on the asthenosphere. These plates move in relation to one another at one of three types of plate boundaries: convergent, or collisional boundaries; divergent boundaries, also called spreading centers; and conservative transform boundaries. Earthquakes, volcanic activity, mountain-building, and oceanic trench formation occur along these plate boundaries. The lateral relative movement of the plates typically varies from 0–100 mm annually. The tectonic plates are composed of two types of lithosphere: thicker continental and thin oceanic. The upper part is called the crust, again of two types (continental and oceanic). This means that a plate can be of one type, or of both types. One of the main points the theory proposes is that the amount of surface of the (continental and oceanic) plates that disappears in the mantle along the convergent boundaries by subduction is more or less in equilibrium with the new (oceanic) crust that is formed along the divergent margins by seafloor spreading. This is also referred to as the conveyor belt principle. In this way, the total surface of the globe remains the same. This is in contrast with earlier theories advocated before the Plate Tectonics paradigm, as it is sometimes called, became the main scientific model, theories that proposed gradual shrinking
Transcript: Our Project Production and Growth production function Important Details ma meo ola haha mot con vit xoe ra 2 cai canh (cc) photo by Metro Centric on Flickr technological knowlege Budapest omg San Francisco con heo beo Results Notes Stockholm (cc) photo by jimmyharris on Flickr Double click to crop it if necessary (cc) photo by Franco Folini on Flickr Production and growth Place your own picture behind this frame! (cc) photo by Metro Centric on Flickr
Transcript: Example of a Jeopardy Template By: Laken Feeser and Rachel Chapman When creating without a template... http://www.edtechnetwork.com/powerpoint.html https://www.thebalance.com/free-family-feud-powerpoint-templates-1358184 Example of a Deal or No Deal Template PowerPoint Game Templates There are free templates for games such as jeopardy, wheel of fortune, and cash cab that can be downloaded online. However, some templates may cost more money depending on the complexity of the game. Classroom Games that Make Test Review and Memorization Fun! (n.d.). Retrieved February 17, 2017, from http://people.uncw.edu/ertzbergerj/msgames.htm Fisher, S. (n.d.). Customize a PowerPoint Game for Your Class with These Free Templates. Retrieved February 17, 2017, from https://www.thebalance.com/free-powerpoint-games-for-teachers-1358169 1. Users will begin with a lot of slides all with the same basic graphic design. 2. The, decide and create a series of questions that are to be asked during the game. 3. By hyper linking certain answers to different slides, the game jumps from slide to slide while playing the game. 4. This kind of setup is normally seen as a simple quiz show game. Example of a Wheel of Fortune Template https://www.teacherspayteachers.com/Product/Wheel-of-Riches-PowerPoint-Template-Plays-Just-Like-Wheel-of-Fortune-383606 Games can be made in order to make a fun and easy way to learn. Popular game templates include: Family Feud Millionaire Jeopardy and other quiz shows. http://www.free-power-point-templates.com/deal-powerpoint-template/ Quick video on template "Millionaire" PowerPoint Games Some games are easier to make compared to others If users are unsure whether or not downloading certain templates is safe, you can actually make your own game by just simply using PowerPoint. add logo here References Example of a Family Feud Template PowerPoint Games are a great way to introduce new concepts and ideas You can create a fun, competitive atmosphere with the use of different templates You can change and rearrange information to correlate with the topic or idea being discussed. Great with students, workers, family, etc. For example: With games like Jeopardy and Family Feud, players can pick practically any answers. The person who is running the game will have to have all of the answers in order to determine if players are correct or not. However, with a game like Who Wants to be a Millionaire, the players only have a choice between answers, A, B, C, or D. Therefore, when the player decides their answer, the person running the game clicks it, and the game will tell them whether they are right or wrong.
Transcript: Wowing template. Click through in 20 steps. But we can move beyond the present. Why? Here is something small... Photo credits: 'horizon' by pierreyves @ flickr te amo mucho It could be much larger! chaparrita linda es mi amor An Example: So... por que yo -te amo -te adoro -te quiero mucho 30 Let me give you some perspetive.... te quierooooo Well here we go suany Here is some context. Provide some common ground. Or something from the present, that we should look beyond. So....
Transcript: Social learning network for teachers & students Create assignments, files & notices Discussion forum for class groups Retrieve homework Penzu Furl Shanna Wood 10/5/12 Web 2.0 Tools Multiple technology tools increase ability to learn Providing students with technology that they would not normally have Positive effect of student learning Student engagement & hands on with technology Encourage creativity Audio broadcast converted to MP3 or other playback device Listener can choose what they listen to and download Can be used for class presentations, lecture & literacy Anyone, Anytime, Anywhere Web 2.0 is a term coined in 1999 to describe web sites that use technology beyond the static pages of earlier web sites Blogs Emerging Technologies Reflection Edmodo Ways that Penzu can be implemented into the classroom:Warm-Up Activities Daily journaling Writing Essay's Introduction Penzu is a simple service written on rails, that allows you to write and save private notes or posts with images, print the entry, or share it by email or submit as assignment Podcasts Enhance learning, creativity & collaboration Easier to share global wide Web 2.0 tools are today's tomorrow Possibilities & future are endless Social bookmarking site that enables students and teachers to share their favorite sites with each other. This can be helpful for research, projects or sharing tutorial sites, with peers. Teachers can also use this site to share ideas on lesson plans or fun ways to teach while keeping students engaged in learning. Daily post Personal reflections Only owner can make changes Class discussion forum
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