Mini lesson plan 1
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The Earth is divided into three main layers - the crust, mantle, and core. The crust floats on top of the mantle, which is below the crust. The core, made of an outer liquid layer and inner solid layer, is at the center of the Earth.
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Mini lesson plan 1
The Earth is divided into three main layers - the crust, mantle, and core. The crust is the solid outermost layer that varies in thickness from 5 to 25 miles thick and has a cool temperature. Underneath the crust is the mantle, the thickest layer at around 1800 miles thick with a hot and solid but plastic texture. The innermost layer is the core which is divided into the solid inner core and liquid outer core with very hot temperatures.
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The document summarizes the four main layers that make up the structure of the Earth - the crust, mantle, outer core, and inner core. It provides details about the composition and characteristics of each layer, including that the crust is broken into tectonic plates that move atop the mantle, the mantle is the largest layer and drives plate tectonic movement through convection currents, and the inner core is a solid ball of iron due to extreme heat and pressure deep within the Earth.
Plate tectonics
Here are the steps to demonstrate a transform boundary using the snack tectonics materials:
1. Place a small amount of icing along the edge of one piece of wax paper to represent the plate boundary.
2. Hold the two pieces of wax paper next to each other with the icing in between.
3. Slowly slide the pieces of wax paper past each other along the icing, which represents the plates moving horizontally in opposite directions.
This demonstrates how transform boundaries form as the plates slide past each other laterally without either plate subducting under the other. The icing represents the fault line where energy is released through earthquakes as the plates shear and grind against each other.
02: Words And Definitions
This document defines 10 important Earth science terms: the asthenosphere is the layer between the upper and lower mantle; the inner core is made of iron and nickel at the center of Earth; the outer core is the coating around the inner core; P waves and s waves are types of seismic waves that can travel through solids and liquids; L waves only travel on land and cause the most damage; convection is the transfer of heat through liquids; convection currents involve warm fluid rising and cool fluid sinking in the mantle; density refers to how tightly packed atoms are in an object; and the exosphere is the outermost layer of the atmosphere.
06: Earth Interior Vocab
The document presents an overview of the main layers of the Earth, including the crust, upper mantle, and asthenosphere. The crust is the top-most solid layer that humans live on. Below the crust lies the upper mantle, which is both solid and liquid. Deeper still is the asthenosphere, the middle layer of the mantle located below the crust and above the core.
Ocean Layers
This document discusses the three main layers of the ocean - the surface layer, thermocline layer, and deep ocean layer. It provides details about each layer:
1) The surface layer or epipelagic zone is mixed by wind and currents, keeping temperatures relatively constant down to around 200m.
2) The thermocline layer lies below and temperatures drop rapidly with depth down to around 1000m, separating the warm surface waters from the cold deep waters.
3) Below the thermocline, the deep ocean layers of bathypelagic, abyssopelagic and hadalpelagic zones have cold, dense waters where temperature and salinity remain uniform with increasing depth.
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Mini lesson plan 1
The Earth is divided into three main layers - the crust, mantle, and core. The crust is the solid outermost layer that varies in thickness from 5 to 25 miles thick and has a cool temperature. Underneath the crust is the mantle, the thickest layer at around 1800 miles thick with a hot and solid but plastic texture. The innermost layer is the core which is divided into the solid inner core and liquid outer core with very hot temperatures.
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The document summarizes the four main layers that make up the structure of the Earth - the crust, mantle, outer core, and inner core. It provides details about the composition and characteristics of each layer, including that the crust is broken into tectonic plates that move atop the mantle, the mantle is the largest layer and drives plate tectonic movement through convection currents, and the inner core is a solid ball of iron due to extreme heat and pressure deep within the Earth.
Plate tectonics
Here are the steps to demonstrate a transform boundary using the snack tectonics materials:
1. Place a small amount of icing along the edge of one piece of wax paper to represent the plate boundary.
2. Hold the two pieces of wax paper next to each other with the icing in between.
3. Slowly slide the pieces of wax paper past each other along the icing, which represents the plates moving horizontally in opposite directions.
This demonstrates how transform boundaries form as the plates slide past each other laterally without either plate subducting under the other. The icing represents the fault line where energy is released through earthquakes as the plates shear and grind against each other.
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This document defines 10 important Earth science terms: the asthenosphere is the layer between the upper and lower mantle; the inner core is made of iron and nickel at the center of Earth; the outer core is the coating around the inner core; P waves and s waves are types of seismic waves that can travel through solids and liquids; L waves only travel on land and cause the most damage; convection is the transfer of heat through liquids; convection currents involve warm fluid rising and cool fluid sinking in the mantle; density refers to how tightly packed atoms are in an object; and the exosphere is the outermost layer of the atmosphere.
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The document presents an overview of the main layers of the Earth, including the crust, upper mantle, and asthenosphere. The crust is the top-most solid layer that humans live on. Below the crust lies the upper mantle, which is both solid and liquid. Deeper still is the asthenosphere, the middle layer of the mantle located below the crust and above the core.
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This document discusses the three main layers of the ocean - the surface layer, thermocline layer, and deep ocean layer. It provides details about each layer:
1) The surface layer or epipelagic zone is mixed by wind and currents, keeping temperatures relatively constant down to around 200m.
2) The thermocline layer lies below and temperatures drop rapidly with depth down to around 1000m, separating the warm surface waters from the cold deep waters.
3) Below the thermocline, the deep ocean layers of bathypelagic, abyssopelagic and hadalpelagic zones have cold, dense waters where temperature and salinity remain uniform with increasing depth.
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Mini lesson plan 1
- 3. Composition of Earth Thickness(Miles) Texture Temperature Crust 25 Solid, Brittle Cool Mantle 1800 Solid, Plastic Hot Core 2175 Outer 1360 Liquid Very Hot Inner 815 Solid Very Hot
- 4. Diagram of the Earth's layers: