The theory that explains how the continents have moved apart is called plate tectonics. This theory suggests that the Earth's outer shell is divided into several plates that move and interact with each other, causing continents to drift over long periods of time. This movement is driven by processes such as seafloor spreading and subduction.
The theory that explains how continents moved apart is called plate tectonics. It proposes that the Earth's lithosphere is divided into several large plates that move and interact with each other, causing phenomena like continental drift, earthquakes, and volcanic activity.
The theory that continents drift apart in the past and continue to do so today is called plate tectonics. This theory explains the movement of Earth's lithosphere (the outermost layer of the planet) and the formation of various geologic features such as mountains, earthquakes, and volcanoes.
The theory that explains how continents move apart from each other is called plate tectonics. This theory states that the Earth's lithosphere is divided into several large plates that float on the semi-fluid asthenosphere underneath, causing the plates to interact and move over time. As the plates move, they can separate from each other, leading to the drifting of continents apart.
The theory that explains how continents move apart is called plate tectonics. This theory suggests that the Earth's lithosphere is divided into several rigid plates that float on the semi-fluid asthenosphere below. These plates can move relative to each other, causing continents to separate due to processes such as seafloor spreading at divergent plate boundaries.
The theory that explains how continents slowly move apart from each other is called plate tectonics. This theory states that Earth's outer shell is divided into several plates that move and interact with one another, causing phenomena such as earthquakes, volcanic activity, and the formation of mountains.
The theory that explains how continents moved apart is called plate tectonics. It proposes that the Earth's lithosphere is divided into several large plates that move and interact with each other, causing phenomena like continental drift, earthquakes, and volcanic activity.
The theory that continents drift apart in the past and continue to do so today is called plate tectonics. This theory explains the movement of Earth's lithosphere (the outermost layer of the planet) and the formation of various geologic features such as mountains, earthquakes, and volcanoes.
The theory that explains how continents move apart from each other is called plate tectonics. This theory states that the Earth's lithosphere is divided into several large plates that float on the semi-fluid asthenosphere underneath, causing the plates to interact and move over time. As the plates move, they can separate from each other, leading to the drifting of continents apart.
The theory of Pangaea is the theory that the Earth was once covered by one giant continent or land mass. The land mass supposedly started to break apart when the dinosaurs went extinct. The theory explains why different continents look like they are part of a jigsaw puzzle, and how the same type of fossil was found on to different continents. The theory also explains why our continents today are slowly drifting apart.
Wegener's theory of continental drift proposed that the continents were once joined together in a single supercontinent called Pangaea. Over time, the continents drifted apart to their current positions. This idea eventually led to the development of the theory of plate tectonics, which explains the movement of Earth's lithosphere on the underlying asthenosphere.
The theory that explains how continents move apart is called plate tectonics. This theory suggests that the Earth's lithosphere is divided into several rigid plates that float on the semi-fluid asthenosphere below. These plates can move relative to each other, causing continents to separate due to processes such as seafloor spreading at divergent plate boundaries.
The theory that explains how continents slowly move apart from each other is called plate tectonics. This theory states that Earth's outer shell is divided into several plates that move and interact with one another, causing phenomena such as earthquakes, volcanic activity, and the formation of mountains.
Alfred Wegener's hypothesis of continental drift explains that continents were once part of a single supercontinent called Pangea, which over time drifted apart to their current positions. This theory is supported by geological evidence such as the matching shapes of continents on opposite sides of the Atlantic Ocean.
The theory that continents can drift apart and have done so in the past is known as "continental drift." This theory suggests that continents were once united in a single landmass called Pangaea and have since moved to their current positions over time.
Alfred Wegener called his theory of moving continents "continental drift." He proposed that Earth's continents were once joined together in a single supercontinent called Pangea, which later broke apart and drifted to their current positions.
The theory that states continents can drift apart from each other is called plate tectonics. It explains how the Earth's lithosphere is divided into large plates that move and interact with each other, leading to processes like continental drift and the formation of mountains, earthquakes, and volcanoes. This theory is supported by evidence such as the matching coastlines of continents, the distribution of fossils, and the presence of deep ocean trenches.
The theory that explains how Earth was once a single supercontinent is called the "Theory of Plate Tectonics." This theory suggests that Earth's outer shell is divided into several plates that move and interact with one another over time, causing continents to drift apart or come together. The supercontinent that is believed to have existed in the past is known as Pangaea.