Mesozoic
The continents assumed their current positions during the Cenozoic Era, particularly in the latter part known as the Neogene and Quaternary periods. This movement of the continents is part of the ongoing process of plate tectonics, where the Earth's lithospheric plates shift and collide over millions of years, leading to the arrangement of the continents as we see them today.
Mesozoic Era
Pangaea began to break apart around 200 million years ago during the Mesozoic Era. The separation process is estimated to have taken about 50-60 million years before the continents assumed their current positions.
During the Tertiary period, Earth's continents were continuing to drift apart due to plate tectonics. This movement led to the formation of new mountain ranges and the reshaping of landmasses. The configuration of the continents during this time was closer to their current positions compared to earlier periods.
The continents were once part of a supercontinent called Pangaea, which began to break apart around 200 million years ago during the process of plate tectonics. Over time, the shifting of tectonic plates caused the continents to drift to their current positions, creating the continents as we know them today.
Modern continents began to take shape around 200 million years ago during the breakup of the supercontinent Pangaea. This process resulted in the formation of the continents we see today, as they drifted into their current positions.
Mesozoic Era
Pangaea began to break apart around 200 million years ago during the Mesozoic Era. The separation process is estimated to have taken about 50-60 million years before the continents assumed their current positions.
During the Tertiary period, Earth's continents were continuing to drift apart due to plate tectonics. This movement led to the formation of new mountain ranges and the reshaping of landmasses. The configuration of the continents during this time was closer to their current positions compared to earlier periods.
The continents were once part of a supercontinent called Pangaea, which began to break apart around 200 million years ago during the process of plate tectonics. Over time, the shifting of tectonic plates caused the continents to drift to their current positions, creating the continents as we know them today.
Cenozoic Era,third of the major eras of the Earth's history, beginning about 65.5 million years ago and extending to the present. It was the interval of time during which the continents assumed their modern configuration and geographic positions and during which the Earth's flora and fauna evolved toward those of the present.
Modern continents began to take shape around 200 million years ago during the breakup of the supercontinent Pangaea. This process resulted in the formation of the continents we see today, as they drifted into their current positions.
The original super-continent of Pangaea broke up about 200 million years ago during the Paleozoic era forming the continents of Gondwanaland and Laurasia. Gondwanaland later fragmented into Antarctica, Africa, Australia, India and South America. Similarly, Laurasia broke up into Asia, Europe and North America. The current 7 continents have been more or less in their current positions for the past few million years.
Pangaea was a supercontinent that existed during the late Paleozoic and early Mesozoic eras, approximately 335 million years ago. It was a single landmass comprising most of today's continents before they drifted apart to their current positions. The theory of Pangaea provides evidence for the concept of continental drift.
They will still be together
The landmass before the current seven continents was known as Pangaea. Pangaea was a supercontinent that existed during the late Paleozoic and early Mesozoic eras.
The early continents are known as "cratons" or "proto-continents." These were the building blocks of the current continents and formed during the Precambrian era.
they will all be together