The age of the seafloor increases with distance from mid-ocean ridges. It is youngest at mid-ocean ridges, where new oceanic crust is formed through volcanic activity, and oldest near continental margins where it eventually subducts back into the Earth's mantle.
The age of rocks gets progressively younger as you move away from the mid-ocean ridges, where seafloor spreading occurs. This supports the theory of seafloor spreading, as new crust is being formed at the ridges and then moves away from them over time. This process leaves a record of older rocks further from the ridges and younger rocks closer to them.
The age of seafloor bedrock increases with distance from a mid-ocean ridge. At the ridge, the bedrock is young, as it is continuously being formed by volcanic activity. As it moves away from the ridge through the process of seafloor spreading, it cools and ages over time.
Yes, there is evidence supporting seafloor spreading, including magnetic striping patterns on the ocean floor, the age progression of seafloor away from mid-ocean ridges, and the presence of hydrothermal vents along mid-ocean ridges that release magma from the Earth's mantle.
Age is based on fossils that are found in the rock.
Seafloor is youngest near the mid-ocean ridges and gets progressively older as you move away from the ridge. Magnetic stripes on the seafloor provide evidence of seafloor spreading, as they show alternating patterns of normal and reversed magnetic polarity that match the Earth's magnetic reversals over time. This supports the theory of seafloor spreading as new oceanic crust is created at the mid-ocean ridge and spreads outward.
The price of economic goods fell during the time period from 1865 to 1896
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Age of seafloor rock and sediment increases with distance from the oceanic ridges.
The economy was strong throughout the Gilded Age.
The current geologic age is referred to as the Holocene epoch.
The Victorian Age was a time period that began in 1837 and ended in 1901.
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the use of scientific procedures to determine the age of artifacts
The age of rocks gets progressively younger as you move away from the mid-ocean ridges, where seafloor spreading occurs. This supports the theory of seafloor spreading, as new crust is being formed at the ridges and then moves away from them over time. This process leaves a record of older rocks further from the ridges and younger rocks closer to them.
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A period of time beginning about 455 AD and extended for about 1000 years.