- Briefly identify different features of continents and ocean basins.
- Define constructive forces and give a few examples.
- Define destructive forces and give a few examples.
- constructive forces
- continental margin
- destructive forces
- mid-ocean ridge
- ocean basin
- ocean trench
Earth’s surface features are the result of constructive and destructive forces. Constructive forces cause landforms to grow. The eruption of a new volcano creates a new landform. Destructive forces wear landforms down. The slow processes of mechanical and chemical weathering and erosion work over time to change once high mountains into smooth flat plateaus.
below is a slice through a relief map of Earth’s surface without the water in the oceans. What are its two most distinctive features?
In this figure, color indicates elevation. Red represents the highest mountains with orange, yellow, and green indicating lower elevations. Light blue to darker blue to bluish-purple descends to the deepest ocean floor.
- The continents are large land areas extending from high mountaintops to sea level.
- The ocean basins extend from the edges of the continents down steep slopes to the ocean floor and into deep trenches.
The oldest continental rocks are billions of years old, so the continents have had a lot of time for things to happen to them. Constructive forces
cause physical features on Earth’s surface known as landforms
to grow. Crustal deformation – when crust compresses, pulls apart, or slides past other crust – results in hills, valleys, and other landforms. Mountains rise when continents collide, when one slab of ocean crust plunges beneath another or a slab of continental crust to create a chain of volcanoes. Sediments are deposited to form landforms, such as deltas.
Volcanic eruptions can also be destructive forces
that blow landforms apart. The destructive forces of weathering and erosion modify landforms. Water, wind, ice, and gravity are important forces of erosion.
Landforms in this radar image of the Crater Highlands of Tanzania are accentuated by 2x vertical relief and also by color. The highest elevations are white and lowest elevations are green.
Look for constructive and destructive landforms in Figure
above. This scene is within the East African Rift where the crust is being pulled apart to form a large valley.
- Which features result from constructive forces? Volcanoes have been constructed within the valley by rising magma.
- Which features result from destructive forces? Volcanic explosions or collapses have destroyed volcanic mountains to form craters. Fractures caused by the rifting in the valley are signs that the valley is breaking apart. Streams are eroding downward into the slopes of the volcanoes. Landslides erode the steep volcanoes. A landslide scar is seen on left side of the small, very steep volcanic cone near the center of the image, and landslide deposits have traveled outward from the scar.
The ocean basins
are all younger than 180 million years. Although the ocean basins begin where the ocean meets the land, the continent extends downward to the seafloor, so the continental margin
is made of continental crust.
The ocean floor itself is not totally flat, as illustrated in Figure
below. The most distinctive feature is the mountain range that runs through much of the ocean basin, known as the mid-ocean ridge
. The deepest places of the ocean are the ocean trenches
, many of which are located around the edge of the Pacific Ocean. Chains of volcanoes are also found in the center of the oceans, such as in the area of Hawaii. Flat plains are found on the ocean floor with their features covered by mud.
Major features of the world’s ocean basins. Salmon = continental margins, yellow-green = the mid-ocean ridge system, deep purple = trenches, and bluish purple = flat regions.
Earth’s surface changes over short and long periods of time. Constructive forces cause new features to form by volcanic activity or uplift of the crust. Existing landforms are modified by destructive forces, perhaps even eroded away by water, wind, ice, and gravity. Beneath the oceans, volcanic activity forms new seafloor while old seafloor is destroyed at the trenches. You will explore many ways that the Earth’s surface changes as you proceed through this book.
- For the most part, continents are much older than ocean basins.
- Both the continents and ocean basins are covered by many types of landforms, including mountains and flat plains.
- Constructive forces cause landforms to grow.
- Destructive forces modify or even destroy landforms.
- Earth’s surface is constantly changing. Change can happen rapidly, as when a volcano blows itself apart, or slowly, as in the grain by grain erosion of a stream into a canyon.
- What are constructive forces and what landforms do they create?
- What are destructive forces and what landforms do they create?
- In a single region, are only constructive or only destructive forces at work?
- In terms of Earth’s surface, what is the only thing that is constant?
- What are some of the landforms found in the ocean basins?
- Until recently, scientists thought the seafloor was just flat and muddy. Why do you think they thought this? What do they think now?
Further Reading / Supplemental Links
Points to Consider
- If erosion is constantly eating away at landforms, why isn’t Earth’s land surface completely flat?
- Why do you think some regions of some continents, such as the middle part of the United States, are almost entirely flat?
- Why are continents higher than ocean basins?
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