The mid-Atlantic ridge. Similar geology and fossils in once adjacent areas.
One piece of evidence that indicates the continents were once connected is the shape of the continents. Many of the continents look as if they fit together like a puzzle.
There is no city present in all continents. Each continent has its own distinct cities.
Geothermal energy is present on all continents.
Gondwanaland is a landmass thought to have been compromised of present-day southern continents.
Continental drift :)
The present continents are not permanent features on Earth. They are part of the constantly shifting tectonic plates that make up the Earth's crust. Over millions of years, continents have moved and changed positions due to the movement of these plates through processes like plate tectonics.
The present tense indicates an action or condition that is currently happening or exists in the present time.
The present tense of indicated is:I/You/We/They indicate.He/She/It indicates.
The present-day continents that made up Gondwana are South America, Africa, Antarctica, Australia, the Indian subcontinent, and the Arabian Peninsula.
Through the passage of time, the continents have gradually moved across the earth's surface into their present positions. This is called the continental drift.
The theory of Pangaea is the idea that all continents were once connected in a single supercontinent that broke apart over millions of years to form the present-day continents. This theory is supported by evidence such as matching rock formations, fossils, and geological features found on different continents. The concept of Pangaea helps explain how continents have drifted apart and provides insight into Earth's geological history.
The continents are currently in their present shapes due to the movement of tectonic plates over millions of years. The Earth's surface is divided into several major plates that are constantly shifting, causing the continents to move and change position. This movement, known as plate tectonics, is responsible for the current shapes and positions of the continents.