Earth structure for S2
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The Earth is made up of layers including an inner solid iron core, outer liquid core, mantle composed of silicates and magnesium oxide that is mostly solid but allows for convection currents, and a thin crust on top made of oceanic or continental plates that are the youngest and most brittle part of the planet.
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Earth´s inner and outer core (Presentation #1 Biology L2 project)
The document discusses Earth's inner and outer core. The inner core is a solid ball of iron, nickel, and other elements with a radius of 1,220 km located at the center of Earth. It was discovered in 1936 by Inge Lehmann using seismic waves. The temperature of the inner core is around 5,700 K and pressure is between 330 to 360 gigapascals. The outer core is a liquid layer of iron and nickel around 2,266 km thick located above the inner core and below the mantle. Convection in the outer core generates Earth's magnetic field, which protects the planet from solar winds.
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The document discusses the structure and composition of the Earth's interior. It can be summarized as follows:
1) The Earth has three main layers - the crust, mantle, and core. The crust is the outermost layer, the mantle is below the crust, and the core is at the center.
2) The crust and upper mantle make up the rigid lithosphere, while the lower mantle and outer core flow slowly like hot asphalt in the asthenosphere.
3) The inner core is solid iron, surrounded by the liquid outer core, with the mantle in between composed of silicate rock that flows via convection currents.
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Earth's interior consists of four main layers - the inner core, outer core, mantle, and crust. The inner core is solid iron, the hottest part of Earth at 5,000 C. The outer core is liquid metal. The mantle is the largest layer, making up 67% of Earth and slowly flows like putty. It has an upper lithosphere and lower asthenosphere. The crust is the thinnest outer layer with ocean crust thinner than continental crust.
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The Earth is divided into four main layers: the crust, mantle, outer core, and inner core. The crust makes up only 1% of the Earth's volume and is broken into tectonic plates. The mantle, the largest layer, lies below the crust and is divided into upper and lower sections. The outer core is liquid and made of iron, while the inner core is solid due to extreme heat and pressure at the Earth's center.
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The document describes the different layers that make up the Earth's interior, including the crust, upper and lower mantle, outer and inner core. It also defines key terms like P-waves and S-waves that travel through the Earth during seismic activity, as well as convection, which transfers heat via fluid movement caused by temperature differences. Geology is identified as the study of the solid Earth.
Earth's layers power point notes
The Earth is divided into four main layers - the crust, mantle, outer core, and inner core. The crust is the thin outer skin of the Earth, making up only 1% of its volume. Below the crust lies the mantle, which is the largest layer and divided into upper and lower sections. Within the Earth is the core, with the outer core being liquid iron and the inner core being incredibly hot solid metals.
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Earth's layers power point notes
The Earth is divided into four main layers - the crust, mantle, outer core, and inner core. The crust is the thin outer skin of the Earth, making up only 1% of its volume. Below the crust lies the mantle, which is the largest layer and divided into upper and lower sections. Within the Earth is the core, with the outer core being liquid iron and the inner core being incredibly hot solid metals.
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This unit aligns with the Next Generation Science Standards and with Common Core Standards for ELA and Literacy for Science and Technical Subjects. See preview for more information
If you have any questions please feel free to contact me. Thanks again and best wishes. Sincerely, Ryan Murphy M.Ed www.sciencepowerpoint@gmail.com
Teaching Duration = 4+ Weeks
The Changing Earth - 01 The Structure of the Earth.
A closer look at the structure of the earth for Year 8 Science students at Saint Ignatius College Geelong.
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The document summarizes key aspects of Earth's structure and composition. It describes Earth's distinct atmospheric layers and how pressure decreases with altitude. It also outlines Earth's internal layering, including the crust, mantle, and core. The crust is divided into continental and oceanic types based on differences in density and thickness. The mantle conveys heat via convection currents. The liquid outer core generates Earth's magnetic field through the geodynamo process.
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The document discusses various impacts of tourism on the Jurassic Coast World Heritage Site in England, including inappropriate fossil collecting, litter, and "urban blight" from overdevelopment. It also mentions "coastal squeeze" where habitat is limited by human activities like sea defenses. Potential impacts from water sports like jet skis and windsurfing include disturbing wildlife and damaging habitats. Solutions proposed include voluntary marine conservation areas and zoning areas of the coastline for different activities.
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Ebony will be visiting Australia from November 16th to December 18th. The schedule includes orientation activities, school assemblies, concerts, tours of Glasgow, Stirling, Edinburgh, and trips to London and Italy. Some key events include the S5 Parents' Night, a geography field trip to Glasgow, a visit from an international exchange group, and departing for the return flight on December 18th.
Tourism and recreation_tourism_is_dorset_s_pred[1]
The Jurassic Coast in England is the country's only natural World Heritage Site, attracting up to 1.5 million visitors annually to experience its sandy beaches and fossil hunting. However, large numbers of visitors can negatively impact the environment through inappropriate fossil collecting, coastal squeeze limiting habitats, littering, and disturbance of wildlife from water sports. Solutions include voluntary marine conservation areas, zoning parts of the coast for different uses, and establishing "gateways" to educate visitors and concentrate tourism spending in sustainable ways.
Tombolo
Tombolos are ridges of sand or pebbles that connect islands to the mainland. They are formed over time by longshore drift, which is the movement of beach materials like sand and pebbles along the coastline. When the direction of the coastline changes, beach materials continue to be transported in their original direction and build up underwater to create spits. As spits grow larger, they can eventually connect to nearby islands, forming tombolos like Chesil Beach, an 18-mile-long ridge of pebbles in the UK.
Comenius partnership presentation
This document outlines a Comenius partnership between schools in the UK, Germany, and Poland over two years focused on urban spaces, regeneration, and design. The partnership will receive EU funding to support travel for staff and pupils between the schools. They will work with local artists and community groups on projects like photo essays, films, writing, and study tours of each other's cities, as well as renovating and planting hidden gardens. E-twinning will also be used to facilitate online collaboration between students and teachers.
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This document discusses a cause that had certain effects, to which responses were made, leading to further effects, prompting questions about additional responses. Multiple responses are then listed.
Blogs And Wikis 2.0
Blogs and wikis allow for two-way communication and sharing of information online. They encourage independent learning, feedback, and collaboration. Blogs can be used by teachers to post materials for students and encourage participation and dialogue. Wikis allow for collaborative editing of content online. Setting up blogs and wikis helps make information sharing digital at Hutchesons' Grammar School.
Blogs And Wikis
This document discusses the use of various Web 2.0 tools like blogs, wikis, Flickr, YouTube, and social networking sites for educational purposes. Blogs can encourage independent learning, allow students to display and get feedback on their work, and enable teachers to post additional materials. Wikis support collaborative learning by providing shared online workspaces. Tools like Flickr and SlideShare allow students to share photos and presentations online and get feedback from peers and teachers.
J8 London
We provide a variety of solutions to help businesses. Our AI assistants can answer customer questions through natural conversations to provide 24/7 support. Our analytics tools help companies better understand customer behavior and needs to improve products and services. We also offer customized consulting to help organizations implement the right technologies for their specific needs and goals.
Weather And Climate
1. The document discusses weather elements such as temperature, precipitation, wind speed, and cloud cover. It also describes how these elements are measured using instruments like a thermometer, rain gauge, and anemometer.
2. Common types of clouds are described as cirrus, cumulonimbus, cumulus, and stratus. The Stevenson screen, used to shelter instruments, is also characterized.
3. The difference between weather and climate is explained as weather referring to short term atmospheric conditions while climate describes average conditions over a long period.
Glaciation On Arran
The document contains 16 photographs of glacial landforms and features found in the Arran Mountains in Scotland, including U-shaped valleys, corries, tarns, erratics, misfit streams, moraines, hanging valleys, arêtes and pyramidal peaks, providing visual evidence of past glaciation.
Settlement Map Questions
The document provides instructions for analyzing and comparing different urban environments and residential areas based on map evidence. It prompts the reader to look for features like land use, industry, housing patterns, open spaces, and street grids to describe the differences between model areas, a commuter belt versus modern housing development, and specific places like Nunthorpe versus Linthorpe/Marton Grove, Denniston versus Castlemilk, and residential areas in Coatbridge and Sunnyside. The reader is asked to specifically refer to map evidence in their analyses and descriptions.
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The document contains 16 photographs of glacial landforms and features found in the Arran Mountains in Scotland, including U-shaped valleys, corries, tarns, erratics, misfit streams, moraines, hanging valleys, pyramidal peaks, arêtes, and examples of glaciation visible from different locations in the mountains.
Desert Landforms
Wind erosion in desert environments forms distinctive landforms including mushroom rocks where wind erodes the soil around rock pedestals while leaving the rock intact, as well as sand plains and dunes which accumulate windblown sand and wadis which are dry river beds that only flow after rain.
6 Figure Grid References
The document discusses 6 figure grid references, which provide more precise locations than 4 figure grid references by dividing grid squares into tenths. It explains that the first 3 figures indicate easting and the second 3 indicate northing. Several examples are given of determining the 6 figure grid reference for points on a map and answering questions about references.
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- 1. Unit 1AAnatomy of the Earth
- 2. 1 in 5
- 3. Core
- 6. 1000 miles an hour
- 8. Solid
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- 10. Iron, Nickel
- 11. Dense
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