Measurement of location east or west of the prime meridian at Greenwich, England
Latitude
Measurement of location north or south of the equator
Locating places using
1. Latitude and Longitude (Earth's Grid System)
2. Landmasses and Bodies of Water
Northern Hemisphere
Part of the Earth that lies north of the equator
Southern Hemisphere
Part of the Earth that lies south of the equator
Five lines of latitude
Arctic Circle
Antarctic Circle
Tropic of Cancer
Equator
Tropic of Capricorn
Lines of latitude
Tell us whether a place is located in the Northern or Southern Hemisphere as well as how far North or South from the Equator it is
Prime Meridian
The line of 0° longitude, the starting point for measuring distance both east and west around Earth
Lines of longitude
Indicate how far East or West of the Prime Meridian a place is
Parallels
Lines of latitude
Meridians
Lines of longitude
Equator
The 0-degree latitude line
International Date Line
An imaginary line that runs from the North Pole to the South Pole, primarily along the 180th meridian of longitude in the Pacific Ocean. It serves as the boundary between one calendar day and the next.
Geographic coordinate system
A system that is used to locate places using the degree of latitude and longitude
Coordinates
A pair of numbers that describe the position of a point
How to get the coordinates of a place
1. Open Google Maps
2. Right-click the place or area on the map
3. Left-click on the latitude and longitude to copy the coordinates
Lithosphere
The crust and the upper layer of the mantle together make up a zone of rigid, brittle rock called the Lithosphere
Layers of the Earth
Crust
Mantle
Core
Crust
It is the thinnest and the outermost layer of the earth's interior
Thickness varies, under mountains it can be as thick as 60 km and less than 5 km under the ocean
It is the least dense of all the layers
It is made up of silicon and oxygen
Oceanic crust
Very dense, made of Basalt
Continental crust
Less dense, made of Granite
Mantle
It is the largest layer of the Earth
It is made of hot, dense rock
The rock in the mantle flows like asphalt because of the temperature differences found in the mantle
Asthenosphere
Part of the mantle, made of bendable rock, like a marshmallow, still a solid but it can move and flow
Mesosphere
Lower part of the mantle, touches the outer core, made of hard strong solid rock/minerals
Core
It is the innermost and the central region of the Earth's interior
The core is divided into 2 layers—Outer and Inner
The core is so hot and has so much pressure that if you were to go there—you would be squished into something even smaller than a marble
Outer Core
Composed of iron-rich metal alloy, and it is inferred to be in liquid form
Inner Core
Comprises the entire center of the Earth's interior
The crust can be as thick as 3 miles to 75 miles in size
No one has ever been below or even drilled below the crust
The center of the Earth is hotter than the surface of the Sun
The temperatures in the mantle range from 2000-5000 °F
The temperatures in the core range from 7000-12000 °F
The core creates the Earth's magnetic field
3 main layers of the Earth
Crust
Mantle
Core
Crust
Very thin
The mantle is the largest layer of the Earth
The Outer Core is a liquid
Lithosphere
The "crunchy" layer of the crust and uppermost part of the mantle