Students also viewed. Unit 1: Origin of the Universe and Our Solar System. Inferred Properties of Earth's Interior. Density of the Crust on the ESRT Increasing Depth Increasing Density.
Asthenosphere (hot, partially melted) 150 km thick on average. Unit 5: Climate Change Throughout Earth's History - Design Blueprint. 5100 km (remember units!!! Unit 3: Homeostasis in Human Body Systems. Inferred Properties of Earth's Interior: Three Level Guide to Diagram Interpretation. In configuration 1, they are all placed on the circumference of a narrow ring of radius R and are uniformly distributed so that the distance between adjacent electrons is the same everywhere. Unit 3: Earthquakes, Volcanoes, and Tsunamis - Who's at Risk? If you see a message asking for permission to access the microphone, please allow.
• - • - • - Inner Core. Represents the Pressure at different depths What is the Pressure at the mantle and outer core boundary? Data Tools: Living Environment Historical Regents Data. Unit 2: Nutrients, Energy, and Biochemical Processes. The Earth contains the following layers (spheres) or boundaries: Crust - continental crust and oceanic crust. Resource: New Visions Instructional Materials. Unit 6: Climate Change and Severe Weather - Full Unit. Information about interior of earth. What does melting point mean? Simple Model of Earth's Interior Crust Mantle Outer Core Inner Core.
In configuration 2, N - 1 electrons are uniformly distributed on the ring and one electron is placed in the center of the ring. Describe the changes in density as depth within the Earth increases. Unit 1: Characteristics of Living Things. Unit 7: Geography, Climate, and Human Cities. Log in: Live worksheets > English. All rights reserved. Data Tools: Earth Science Historical Regents Data Tools. Interior of earth ppt. For that value of N, consider any one circumference electron - call it. Mantle - forms three quarters of the volume of the Earth and two thirds of its weight. • Continental: • - • Oceanic: • -. What is the approximate density of Oceanic crust? MOHO- Mohorovicic Discontinuity: • - Andriji Mohorovicic.
What do you want to do? Review Question What are the major differences between the continental crust and the oceanic crust? Unit 3: Landscapes and Surface Processes. It can be divided into four spheres: lithosphere (cool and rigid). A liquid outer core. How thick is the mantle? Unit 5: The Earth-Sun-Moon System. Interior portion of the earth. Resource: Materials from Past Workshops. Unit 2: Early Earth - Design Blueprint. List the four (4) main layers of the Earth from thinnest to thickest (include the asthenosphere as part of the mantle. Unit 4: Disease and Disruption of Homeostasis. ESRT page 10 Yes, take out your ESRT NOW! What is the temperatures at the lithosphere and asthenosphere boundary? Resources: Getting Started.
This dotted line shows the melting point of material in the Earth. From Solid to a Liquid If the temperature is below the melting point, what phase is it in? How many other circumference electrons are closer to than the central electron is? Professional Learning. What is the Inner Core? ESRT pg 10 More on the Interior. 1000°C Line represents the temperatures inside the earth.
Resource: Quiz Banker. Final Question: • Which type of crust is the most dense? Unit 1: Discovering New Worlds - Full Unit. Solid Solid Solid Liquid Solid Which layers in the diagram have temperatures below the melting point?