my son did it aged 8
in the middle of the ocean ridge
You would want to look for rocks at the center of the Mid-Atlantic Ridge, where new oceanic crust is forming through seafloor spreading. The rocks found closest to the ridge axis are typically the youngest, as they have most recently solidified from magma.
The youngest sediments found near the Mid-Atlantic Ridge are typically associated with the oceanic crust formed at the ridge itself, which is less than a few million years old. These sediments primarily consist of pelagic clay, biogenic material, and volcanic ash, accumulating as the seafloor spreads. The rate of sedimentation is relatively low, meaning that the youngest sediments are generally found closest to the ridge and become progressively older with distance from it.
The age of the oceanic crust increases with distance from mid-ocean ridges. As tectonic plates diverge at these ridges, magma rises to form new crust, which is youngest closest to the ridge. As the crust moves away from the ridge due to seafloor spreading, it cools and ages, leading to progressively older crust farther from the ridge. This pattern is a key feature of plate tectonics and helps scientists understand the dynamics of the Earth's lithosphere.
The two main routes to climb Mount Everest are the South Col - South East Ridge from Nepal and the North Col - North East Ridge from Tibet.
Near the mid-Atlantic ridge.
The two main routes to climb Mount Everest are the South Col - South East Ridge from Nepal and the North Col - North East Ridge from Tibet.
in oak ridge, with his wife and his three youngest sons
at the mid-ocean ridge you can find the youngest oceanic plate and a divergent boundary.
The two main routes to climb Mount Everest are the South Col - South East Ridge from Nepal and the North Col - North East Ridge from Tibet.
in the middle of the ocean ridge
The two main routes to climb Mount Everest are the South Col - South East Ridge from Nepal and the North Col - North East Ridge from Tibet.
You would want to look for rocks at the center of the Mid-Atlantic Ridge, where new oceanic crust is forming through seafloor spreading. The rocks found closest to the ridge axis are typically the youngest, as they have most recently solidified from magma.
The Mid-Atlantic Ridge is neither Continental rock or indeed the oldest rock on the planet. The rock in the ridge is commonly the youngest, or of the youngest, on the planet, as it was formed most recently, and is oceanic, not continental, crustal rock.
The youngest rocks in the Atlantic Ocean are found along the mid-ocean ridge system, where new oceanic crust is formed through volcanic activity. This process, known as seafloor spreading, occurs along underwater mountain ranges, such as the Mid-Atlantic Ridge. As molten rock cools and solidifies at the ridge, it creates new oceanic crust, making this region home to some of the youngest rocks in the Atlantic.
The youngest sediments found near the Mid-Atlantic Ridge are typically associated with the oceanic crust formed at the ridge itself, which is less than a few million years old. These sediments primarily consist of pelagic clay, biogenic material, and volcanic ash, accumulating as the seafloor spreads. The rate of sedimentation is relatively low, meaning that the youngest sediments are generally found closest to the ridge and become progressively older with distance from it.
The youngest oceanic crust in the Indian Ocean is located at the Central Indian Ridge, which is a mid-ocean ridge that runs roughly north-south between Madagascar and India. This area is characterized by active seafloor spreading, where new crust is formed as magma rises to the surface. The youngest crust typically lies closest to the ridge axis and becomes progressively older as you move away from it.