If you mean how many 'spaces' between planets, then eight.
When a rock is broken into many pieces, it is called fragmentation.
The Earth's broken-up pieces are called tectonic plates. These large, rigid slabs of the Earth's lithosphere float on the semi-fluid asthenosphere beneath them. The movement of these plates is responsible for many geological phenomena, including earthquakes, volcanic activity, and the creation of mountain ranges.
They are called plates!
Small pieces of rock from old broken-up comets become meteoroids when they enter Earth's atmosphere. Depending on their size, they can create meteors (shooting stars) as they burn up or meteorites if they survive the journey to the surface of the Earth.
Soil is made up of broken down pieces of living and nonliving earth material. Living material can include plant matter, organisms, and bacteria, while nonliving material can include rocks, minerals, and organic matter.
It is broken up into pieces called tectonic plates
When a rock is broken into many pieces, it is called fragmentation.
earth's crust is broken in 12 pieces that constantly moves
The Earth's broken-up pieces are called tectonic plates. These large, rigid slabs of the Earth's lithosphere float on the semi-fluid asthenosphere beneath them. The movement of these plates is responsible for many geological phenomena, including earthquakes, volcanic activity, and the creation of mountain ranges.
They are called plates!
They are called tectonic (or lithospheric) plates.
Earthquakes
Broken in Pieces was created in 2002.
broken pieces
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.
Small pieces of rock from old broken-up comets become meteoroids when they enter Earth's atmosphere. Depending on their size, they can create meteors (shooting stars) as they burn up or meteorites if they survive the journey to the surface of the Earth.
Soil is made up of broken down pieces of living and nonliving earth material. Living material can include plant matter, organisms, and bacteria, while nonliving material can include rocks, minerals, and organic matter.