the crust
The lithosphere is the layer of the Earth that is broken up into tectonic plates. These plates are like puzzle pieces that move and interact with each other, causing geological phenomena like earthquakes and volcanic activity.
The pieces of the Earth's crust are called tectonic plates. These plates float on the semi-fluid layer of the Earth's mantle and interact with each other, causing movements such as earthquakes and volcanic activity.
The Earth's lithosphere, which is the outermost layer of the Earth's surface, is broken into tectonic plates. These plates float on the semi-fluid asthenosphere below and move relative to each other, causing geological phenomena like earthquakes, volcanic eruptions, and the formation of mountain ranges.
The outer layer of the earth where the land masses are is called the crust
The rigid layer of the earth that surround the asthenosphere is also known as the lithosphere. The lithosphere layer is further broken into several large sections which are known as tectonic plates. These plates ride above the asthenosphere.
outter court
The lithosphere is the layer of the Earth that is broken up into tectonic plates. These plates are like puzzle pieces that move and interact with each other, causing geological phenomena like earthquakes and volcanic activity.
The layer of the Earth that is broken into large and small tectonic plates is the lithosphere. This rigid outer layer encompasses the crust and the uppermost part of the mantle. The tectonic plates float on the semi-fluid asthenosphere beneath them, leading to geological activities such as earthquakes and volcanic eruptions as they interact with one another.
The layer that fits this description is the lithosphere. The lithosphere is comprised of the uppermost part of the mantle and the crust, and it is broken into tectonic plates that move on the Earth's surface.
The pieces of the Earth's crust are called tectonic plates. These plates float on the semi-fluid layer of the Earth's mantle and interact with each other, causing movements such as earthquakes and volcanic activity.
The Earth's lithosphere, which is the outermost layer of the Earth's surface, is broken into tectonic plates. These plates float on the semi-fluid asthenosphere below and move relative to each other, causing geological phenomena like earthquakes, volcanic eruptions, and the formation of mountain ranges.
The middle layer of earth that is MANTLE. It has the tectonic plates floating on it.
The outer layer of the earth where the land masses are is called the crust
The rigid layer of the earth that surround the asthenosphere is also known as the lithosphere. The lithosphere layer is further broken into several large sections which are known as tectonic plates. These plates ride above the asthenosphere.
The lithosphere is the layer that moves with the tectonic plates. The lithosphere is made up of the crust and the upper part of the mantle, and it is broken into tectonic plates that move and interact with each other.
The plates are part of the crust, the upper layer of the Earth. The plates are moved by currents in the upper mantle. The plates and flexible upper mantle are referred to collectively as the lithosphere and sit atop the mantle layer called the aesthenosphere.
The Earth's lithosphere, which is the outermost layer of the Earth's surface, is broken into 12 major tectonic plates that float on the semi-fluid asthenosphere below. These plates interact at their boundaries, causing geological processes such as earthquakes, volcanic eruptions, and the formation of mountain ranges.