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Geology Powerpoint Template

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Geology

Transcript: Rocks The Rock Cycle Volcanic Eruption Igneous Rock Sediment Magma Metamorphic rock Types of rocks Sedimentary Rock

geology

Transcript: Fissure Eruptions Continental drift- the theory that continents an drift apart form one another and have done so in the past Plate tectonics- the theory that the earth lithosphere is divided onto tectonics paltes that move around on top of the asthenosphere tectonic plate- a piece of the lithosphere that moves around on top of the asthenosphere Earth Cross section of Earth Transform Boundary Inner core Solid-nickel & iron Outer core liquid- nickel & iron Mantel- Molten rock Crust- rock Earthquakes - often violent shaking of the earth as plates move - most often on plate boundaries Tsunami - (harbor wave) massive volume of water that is displaced by movement of plates boundaries can cause widespread damage and loss of life Folding Volcanic eruptions form in areas where the plates are colliding. The oceanic plate is forced under the continental plate where it melts and forms magma. Volcanic eruptions occur where there is a build up of magma, gases. The pressure builds up over time and the eruptions are violent and destructive. Pyroclastic material can move at over 500 kph and will vaporise all living things in their path. Convergent/consuming boundary-the boundary between two colliding tectonic paltes where one rides up over the other-usually have volcanoes and many erth quakes Subguction zone- hte region where an oceanic plate sinks down into the astheosphere at a conveergent boundary usually between continental and oceanic plates Volcanoes Fault-a break in the earth crust along which two blocks of the crust slide relative to one another due to tectonic forces there are three types of faults Normal faults- where the plates are pulling away from each other and the surface is lengthened - lead to horsts and rift valleys eg the rift valley of east Africa Reverse faults - where the plates are pushing together and the surface is shortened eg fold mountains such as the Himalaya Slip faults - the plates moves sideways eg San Andreas fault Faults Panagea Consuming Boundaries Transform boundary - the boundary between two tectonic plates that are sliding past each other horizontally - san Andrea's fault Earthquakes and Tsunami Formation of the Earth Folding- the bending of rock layers due to stress in the earths crust Fold mountains - mountains that form where two plates collide and copress layers of rock into folds Anticline - a upward fold in rock formed by compression and earths crust Syncline - a downward fold in rock formed by compression in earths crust Recumbent fold - rock layers that are bent so much that a rock appears to be folded on top of one another - vertically Layers of earth The Earth is approximately 4.5 billion years old Its has a crust (the continents and sea beds) on the outside that floats like the skin on custard The mantle has a core are generally molten metals that are extremely hot The continents move very slowly. The magnetic poles can change- as it is possible for the inner core to move relative to the rest of the planet Divergent/accreting boundary - the boundary between two tectonic plates that are moving away from each other - rift valley in North Eastern Africa Sea-floor spreading - the process by which new oceanic lithosphere is created at mid-ocean ridges as older materials are puller away from the ridge. The lithosphere (crust and upper mantle ) rest on the molten asthenosphere (lower mantle). Molten Rock beneath the surface is called "magma". Volcanoes are formed when magma is forced through a weakness in the earths crust, either on land or under the sea. These events are called eruptions. There are two basic types of eruption, fissure eruptions and volcanic eruption Crust- the thin, outermost layer of the earth, or the uppermost part of the lithosphere Continental crust- the portion of the earths crust that primarily contains granite, is less dense than ocenanic crust, and is 20-50km thick Oceanic crust- the portion of earths crust that is usally below the oceans and not associated with continental areas, thinner and higher in destiny that continental crust and basaltic rather than granitic in composition Mountain Building Mantle- layer of the earth between the crust and the core Core- the central, spherical part of the earth below the mantle Lithosphere- the outermost, rigid layer of the Asthenosphere- the soft layer of the mantle on which pieces of the lithosphere move Mesosphere- literally, the "middle sphere"- strong, lower part of the mantle between the asthenosphere and the outer core Outer core- liquid layer of the earth core that lies beneath the mantle and surronde the inner core Inner core- the solid, dense centre of earth Sea Floor Spreading Boundary Occur where the plates are moving apart the lava tends to be quite 'runny' and it gently seeps out of the fissures( cracks in the earth's surface This lava can run for a considerable distance and may form a lava plateau Lava fountains’ can also occasionally form along these fissures – fig 6.13 p 137 Continental Drift

NATHO POWERPOINT TEMPLATE

Transcript: Wrap up quickly * Summarize each point you made * Give quick call-backs so your audience remembers * Make it clear this is the end The results Dive deeper Put a bold statement here This is where your presentation starts. Provide context for your audience and make it easy for them to follow. Provide statistics, go into detail, or more — whatever works best for your presentation. Keep your words short and punchy so your audience stays focused. You can add imagery and frames to keep their attention where you want it. Provide any important context here Put a bold statement here 1 Short headline goes here Keep your words short and punchy so your audience stays focused. You can add imagery and frames to keep their attention where you want it. Provide any important context here. Introduce a topic 2 Name your presentation * Quickly cover the important parts of this topic * Limit your words so your audience stays focused * Use visuals to help you 3 6 You can put a subtitle here Quote or caption here 4 5 Introduce a topic Make a bold statement * Quickly cover the important parts of this topic * Limit your words so your audience stays focused * Use visuals to help you Use this space for details that you haven’t talked about yet. Relate what you’re saying to the nearby image so your audience has a visual, too.

PowerPoint Portrayal Template

Transcript: huddle Mrs. Rossi huddle to crowd together crowd huddle separate

Geology

Transcript: The Geologic History of Minnesota Minerals Rocks •MN was covered by an ocean for 2.3 billion years. •The Mesabi, Cuyuna, Vermillion, and Gunflint began to form minerals, and they would sink and go to the bottom of an inland sea. •Algae are little green plants in water. Usually feels slimy. •Algae grow in the shallow waters on the North Shore. It is the earliest form of life we know of. •Scientist found fossil algae in our rocks. (We have some of the oldest in the world.) •Agates are MN's state rock. They are made of warm water in the valley, which carries the silica into the volcanic rock. •Scientist don't believe there were never any dinosaurs in Minnesota. •The ice age began 2 million years ago. •The glaciers melted into lakes and everything that wasn't a lake, forest covered. •8 million years ago, people relied on birds, fish animals, deer, bison, nuts, berries, and wild vegetables to eat. www.DNR.state.MN.us/snas/natural- history.html Iron ore has been around and mined for over a century. Copper and nickel have been mined with 4.4 millions tons since they first started which also includes platinum which groups them all into one metal resourse. www.tigerminerals.com Minnesota’s oldest rocks are within the Canadian shield belts, which is under the north half of the state and most of the Minnesota river valley. The belts under the surface are of volcanic and sedimentary rocks, granitic rock materials are in the areas between the belts. Gneiss and metamorphic rock that are along the side of the Minnesota river valley that were formed 3,600 million years ago. They were formed from granite and other rocks put into various temperatures of hear into the earth. Copper Copper Calcite Groutie Rhodochrosite History of our city and state http://www.dnr.state.mn.us/education/geology/digging/fossils.html By: Lexi, Chelsey, and Ellie Groutie Calcite Fossils http://socialstudies.mpls.k12.mn.us/uploads/mn_ historical_society_slides_early_mn_history.pdf http://www.jeanhenning.remax-northcentral.com/ remaxhc/modules/agent/agent.asp?p=pagecontent. asp&nav=1&pia=6181 Fossils are made by recently deceased bodies or footprints quickly buried in sediment. The sediment hardens and then the animal’s body decays and leaves an imprint. Fossils of all ages can be found throughout Minnesota's gravel pits, beaches and other glacial features. As glaciers from Canada came down to Minnesota, they picked up rocks that had fossils in them. As the glaciers went back up north, the fossils were left behind in Minnesota. Pathologists use fossils to discover our states history, but anyone can collect fossils. All you need are a few simple tools and permission. Make sure you ask the person who owns the land you are on before you start looking. www.sciencebuzz.org Sources Rhodochrosite

Geology

Transcript: National Earnings Bachelor's Degree Related Occupations Technical Skills National Employment and Outlook Master's Degree Thank You! Career Clusters Education and Training Social/Organization/Research Skills Training, Other Qualifications, and Advancement photo credit Nasa / Goddard Space Flight Center / Reto Stöckli Salaries from 2002-2010 with Years of Experience Job Description Suggested High School Subjects Geologist Pennsylvania Salaries Physical Abilities Paleontology Employment and Outlook Future Goals "Only a geologist is a true rock star. We will rock your world." Pennsylvania Employment and Outlook Career Pathways/Majors Occupations Specialties Work Environment Work Environment Skills Earnings Doctoral Degree Employment Opportunities The study of the forms of life existing in prehistoric or geologic times, as represented by the fossils of plants, animals, and other organisms. Nature of the Work Duties and Responsibilities Personal Qualifications By: Jenna Faith

Office PowerPoint Template Guide

Transcript: Designing Effective Templates Color Schemes and Fonts Choose a color palette that aligns with your brand identity while ensuring legibility. Pair fonts effectively by selecting a readable typeface for body text and a complementary font for headings, limiting to two or three fonts. Layout and Structure An effective layout organizes content logically, improving comprehension. Use a grid system for alignment, prioritize key information through hierarchy, and maintain consistency across slides for a unified look. Incorporating Branding Office PowerPoint Template Guide Integrating brand elements like logos, colors, and fonts creates professional consistency. Ensure that all slides reflect your organization's identity and values to reinforce recognition and trust with your audience. Designing Effective Templates Creating a well-designed PowerPoint template can significantly enhance the effectiveness of presentations. Focusing on layout, color schemes, and branding ensures clarity and promotes engagement. Content Creation Strategies Visuals that Engage Effective presentations incorporate visuals that complement the message. Use charts to illustrate data trends, and images to evoke emotions. For example, a before-and-after image can powerfully highlight the success of a project. Structuring Information Captivating Headlines Organizing content logically guides the audience through your presentation. Use bullet points for quick insights, and follow a clear progression from introduction to conclusion. This helps maintain audience focus and enhances retention. Headlines should grab attention and summarize key points. Using action verbs and clear language helps create intrigue. For instance, instead of "Company Performance," use "Driving Growth: Our 2023 Performance Highlights" to stimulate interest. Content Creation Strategies Creating compelling presentations requires effective content strategies that enhance clarity and engagement. Focusing on headlines, visuals, and structured information can significantly elevate the impact of your presentation. Creating Effective Presentations for the Workplace Mastering Presentation Techniques Mastering Presentation Techniques Effective presentation skills are crucial for conveying messages and engaging audiences. Proper rehearsal, audience interaction, and adept handling of questions can elevate the success of any presentation. Handling Questions and Feedback Rehearsing Your Presentation Encourage questions at appropriate times, fostering an open dialogue. Acknowledging feedback shows receptiveness and can enhance audience connection, along with providing valuable insights for future presentations. Rehearsal is essential for ensuring clarity and confidence. Practicing multiple times enables presenters to polish their delivery, address timing, and refine transitions, leading to a smoother presentation experience. Engaging Your Audience Engagement can be fostered through relatable content and interactive elements such as polls or questions. Connecting personally through storytelling increases audience investment and interest in the presentation's objectives. Introduction to Office PowerPoint Templates Benefits of Using Templates Templates save time and resources by minimizing the design process. They enhance brand consistency and improve audience engagement through polished visuals, allowing presenters to focus on content delivery without getting bogged down by format issues. Purpose of Templates Types of Office Templates The primary purpose of Office PowerPoint templates is to provide a structured framework for presentations. Templates help standardize visual elements, ensuring that all slides maintain a cohesive look and feel, which is critical for effective communication in professional settings. There are various types of Office templates including general presentation templates, specialized templates for reports, charts, and infographics, as well as industry-specific templates. Each template type serves different needs, facilitating tailored presentations for diverse audiences. Introduction to Office PowerPoint Templates Office PowerPoint templates streamline the creation of professional presentations, ensuring consistency and visual appeal. By utilizing templates, users can focus on content while saving time on design elements, making them indispensable in the workplace.

Geology

Transcript: Joshua Szymanski Presenting.. Geology! The rock cycle goes in order starting with igneus rocks becoming sedimentary then metamorphic to igneus again Granite Sedimentary Rocks: Sandstone is a rock made from sand being packed together, it is used for building stone walls/statues Limestone is again also used for making things like statues/countertops, but also white pigment in paints/toothpastes Metamorphic Rocks: Marble is compacted limestone and used to make statues/countertops Daimonds are compacted carbon and used to make jewelry and very strong tools due to their hardness. Granite is strong and used for countertops Obsidian is sharp, used for cutting tools They're formed when heat/compression is added to a rock deep beneath the earth Obsidian is made when lava hits water and rapidly cools Metamorphic Rocks: Formed 'under heat/pressure & the Rock Cycle! ..and fun ones! Formed from volcanoes! Obsidian is a sharp volcanic glass used in cutting tools Igneous Rocks: Granite is the continental bedrock and used for countertops They're made when runoff of weathered igneus rock is compacted into something else

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