The oldest ice cores (taken from the Antarctic) date back some 1.5 million years. There are some variables that can introduce error, but it (the error) will be small compared to the age of the recovered materials. This is not theory. Proven laboratory techniques allow us to make these statements. No one who understands the physics of the methods will gainsay them. The physics is not that difficult to get a handle on. But remove any religious (or other) blinders before looking at the science. A link is provided to the white paper on these core samples.
Metamorphic rocks are the oldest continental rocks.
They tend to be preserved in the core of continental crust (known as cratons) and form some of the oldest rocks on the planet, including the 4.28 billion year old Nuvvuagittuq Greenstone belt in Canada (the oldest rocks on the planet) and the Narryer Gneiss Terrane in Western Australia which contain the oldest individual crystals found on the planet at 4.404 billion years old.
The oldest rocks of terrestrial origin (i.e. they were formed on earth) are 4.28 billion years old.
However the oldest rock found on Earth is a meteorite that is 4.56 billion years old.
The ice in Antarctica covers approximately 98% of the Antarctic continent. The ice sheet on the continent of Antarctica is about 4,500 years old.
The oldest oceanic crust is in the west Pacific and north-west Atlantic. They are about 180 to 200 million years old.
The Zircon Crystal, found in Western Australia, is a sedimentary rock and is about 4.3 billion years old.
The oldest continental crust would be between three and one half to four billion years older than the oldest oceanic crust. This is due to the fact that ocean plates are subducted under the continental plates, subjected to partial melt and essentially recycled in the mantle before reforming.
The oldest continental crust would be between three and one half to four billion years older than the oldest oceanic crust. This is due to the fact that ocean plates are subducted under the continental plates, subjected to partial melt and essentially recycled in the mantle before reforming.
oldest
Because the oldest parts reach the continental crust and then the ocean floor sinks beneath the continental crust, into the mantle.
The oldest ocean, geologically, is the Panthalassa Ocean which was around 220 million years ago in the Triassic era. It encompassed the whole Earth except the land mass Pangea. See related link for more information.
The oldest continental crust would be between three and one half to four billion years older than the oldest oceanic crust. This is due to the fact that ocean plates are subducted under the continental plates, subjected to partial melt and essentially recycled in the mantle before reforming.
The oldest continental crust would be between three and one half to four billion years older than the oldest oceanic crust. This is due to the fact that ocean plates are subducted under the continental plates, subjected to partial melt and essentially recycled in the mantle before reforming.
The oldest continental crust would be between three and one half to four billion years older than the oldest oceanic crust. This is due to the fact that ocean plates are subducted under the continental plates, subjected to partial melt and essentially recycled in the mantle before reforming.
The oldest continental crust would be between three and one half to four billion years older than the oldest oceanic crust. This is due to the fact that ocean plates are subducted under the continental plates, subjected to partial melt and essentially recycled in the mantle before reforming.
The oldest continental crust would be between three and one half to four billion years older than the oldest oceanic crust. This is due to the fact that ocean plates are subducted under the continental plates, subjected to partial melt and essentially recycled in the mantle before reforming.
The oldest continental crust would be between three and one half to four billion years older than the oldest oceanic crust. This is due to the fact that ocean plates are subducted under the continental plates, subjected to partial melt and essentially recycled in the mantle before reforming.
The oldest oceanic crust is in the west Pacific and north-west Atlantic. They are about 180 to 200 million years old.
The oldest continental crust would be between three and one half to four billion years older than the oldest oceanic crust. This is due to the fact that ocean plates are subducted under the continental plates, subjected to partial melt and essentially recycled in the mantle before reforming.
The oldest rocks are actually on land but in the ocean crust they would be the rocks closest to land. The mid-ocean ridge forms new rocks. They are usually located in the middle of the ocean.
The oldest rock in oceanic crust is that which is found the greatest distance from a mid-ocean-ridge.
oldest
Because the oldest parts reach the continental crust and then the ocean floor sinks beneath the continental crust, into the mantle.