the way the altitude changes the temperature changes
Surveyors (sometimes called Engineering Surveyors) lay out boundary lines between parcels of land, and draw maps.
The Gutenberg Discontinuity, is the boundary, as detected by changes in seismic waves, between the Earth's lower mantle and the outer core about 1800 miles below the surface. It is also called the core-mantle boundary.
That they both investigate to find their answer
when two plates are slide past one another an example is the san Andreas fault California which is the boundary between the north America and pacific plates
A transform boundary.
The boundary between the mantle and core is known as the core-mantle boundary. It lies approximately 2,900 kilometers below the Earth's surface. This boundary separates the molten iron-nickel outer core from the solid iron-nickel inner core.
Doesn't it have to be Europe? That's what I have.......
The boundary between the troposphere and stratosphere is called the tropopause. It is characterized by a stable temperature inversion where the temperature stops decreasing with altitude and instead starts to increase. This boundary is located at an altitude of around 8-15 kilometers above the Earth's surface.
The crust is part of the lithosphere, so there is no boundary between them. There is a boundary between the crust and the other part of the lithosphere which is the uppermost mantle. It is called the Mohorovicic Discontinuity or the 'Moho' for short.
ummm hello! its just the moho layer! the moho layer is the boundary between the mantle and the crust!there is absolutely no boundary between the moho layer and the mantle! you think i am wrong? then drill to the moho layer and find out!
The lower boundary of the Earth's crust is called the Mohorovičić discontinuity, or Moho for short. It is typically located between 5 and 10 kilometers beneath the ocean floor and around 20 to 70 kilometers beneath the continents.
The boundary between the mantle and the core is called the core-mantle boundary and also The Gutenberg Discontinuity which marks the upper boundary of the D'' (D Double Prime) layer.
The Rio Grande River, defining 3,141 Kilometers (1,952 miles) of the border.
The tropopause is the boundary between the troposphere (the lowest layer of Earth's atmosphere where most weather occurs) and the stratosphere (the layer above the troposphere where the ozone layer is located). This boundary is characterized by a change in temperature and is found at an average height of about 8-15 kilometers above the Earth's surface.
Balloons typically operate in the stratosphere, which is the second layer of the Earth's atmosphere. This layer begins around 10 kilometers above the Earth's surface and extends up to about 50 kilometers. As they ascend, balloons approach the boundary between the troposphere and the stratosphere known as the tropopause.
the active boundary between plates is a ?
the boundary between mantel and crust is mohorovisic the boundary between mantel and core is guttenberg