7
There are around 15-20 minor tectonic plates on Earth, in addition to the major plates that comprise the Earth's lithosphere. These minor plates are smaller in size compared to the major plates and play a role in the movement and dynamics of tectonic activity.
7
The Earth's crust is divided into several large tectonic plates, with around 7 major plates and several smaller ones. These plates float on the semi-fluid upper mantle and interact at their boundaries, where most of the Earth's seismic activity occurs.
Earth's crust is divided into a series of large and small plates, known as tectonic plates. There are about 7 major plates (e.g., the Pacific Plate, North American Plate) and several minor plates that make up the Earth's crust.
There are multiple tectonic plates that make up Earth's crust, with the number of major plates usually defined as around 7 to 8. These plates are in constant motion due to the process of plate tectonics, leading to various geological activities such as earthquakes and volcanic eruptions.
20
seven
twelve (12)
There are around 15 minor tectonic plates in the Earth's crust, in addition to the major plates. These minor plates contribute to the overall movement and interaction of Earth's tectonic plates.
There are around 15-20 minor tectonic plates on Earth, in addition to the major plates that comprise the Earth's lithosphere. These minor plates are smaller in size compared to the major plates and play a role in the movement and dynamics of tectonic activity.
The Earth's surface is divided into about 15 major land plates and other smaller sub-plates.
There are 7 major tectonic plates: African, Antarctic, Eurasian, North American, Pacific, South American, and Indo-Australian plates.
7
The Earth's surface is divided into about 15 major land plates and other smaller sub-plates.
none
The Lithosphere is a mechanical layer on Earth that contains seven major plates.
The Earth's crust is divided into several large tectonic plates, with around 7 major plates and several smaller ones. These plates float on the semi-fluid upper mantle and interact at their boundaries, where most of the Earth's seismic activity occurs.