No, due to plate shifting, earthquakes, volcanoes, erosion, and sediment settling it will most definitely be very different in a million years.
The ocean is 4 billion yars old, however due to subduction, the oldest sediment found in the ocean's floor is 180 million years old.
Less than 200 Million years old.
Because the oldest parts reach the continental crust and then the ocean floor sinks beneath the continental crust, into the mantle.
The ocean floor is approximately 180 million years old due to the process of seafloor spreading, which occurs at mid-ocean ridges where tectonic plates diverge. As magma rises and solidifies, new oceanic crust is formed, gradually moving away from the ridge. The oldest oceanic crust is typically found at the edges of ocean basins, as it gets subducted back into the mantle at tectonic plate boundaries. This cycle of creation and destruction helps explain why the ocean floor has sections that are around 180 million years old, correlating with the geological history of the Earth.
In 1990, after 20 years of searching, geologists found the oldest oceanic rocks by drilling into the seafloor of the western Pacific. These rocks turned out to be about 200 million years old, only about 4% of the Earth's age.
The ocean floor
The age of the sea floor varies, with the youngest being less than 200,000 years old and the oldest being over 200 million years old. This variation is due to the process of seafloor spreading at mid-ocean ridges and the subduction of older seafloor at deep-sea trenches.
The oldest rock on the ocean floor can be found in the central parts of the ocean basins, particularly in regions known as abyssal plains. These rocks are generally around 200 million years old or older.
The oldest rocks on the ocean floor are found in the eastern Mediterranean Sea, dating back to about 200 million years, while the youngest rocks are typically associated with mid-ocean ridges, where new oceanic crust is formed through volcanic activity. For instance, the youngest ocean floor rocks, around a few million years old, can be found near the Mid-Atlantic Ridge. These variations in age highlight the dynamic processes of seafloor spreading and plate tectonics.
On average, continents are older than ocean basins. Due to the action of plate tectonics, ocean crust is being formed and destroyed continuously. The oldest oceanic crust is about 200 million years old, whereas continents, which are less dense than oceanic crust and tend not to be subducted into the mantle, can be more than 3,000 million years old in places.
200 million
The youngest rocks on the ocean floor are located at mid-ocean ridges, where new oceanic crust is constantly being formed through volcanic activity. These rocks are typically less than 5 million years old.