As
new ocean crust is created through erupting underwater volcanoes, iron - rich minerals are fired out in the upwelling magma.
Such vents line the midocean ridges, where magma wells up to form
new ocean crust.
Plunging into the ocean off the west coast of Vancouver Island, the more than 800 kilometers of fiber optic cables that connect the research stations stretch across the continental shelf, plummet down the slope and across an abyssal plain, and skirt hydrothermal vents near a mid-ocean ridge where the Earth gives birth to
new ocean crust.
Through the process of seafloor spreading,
new ocean crust continually comes into being here.
Not exact matches
This week brings a video reconstructed from images of the Philae lander's approach to a comet, and a major
new analysis of data from the Cassini mission that bolsters the case for a global, not just local,
ocean beneath the icy
crust of Enceladus
A crack in the Earth's
crust — which could be the forerunner to a
new ocean — ripped open in just days in 2005, a
new study suggests.
The evidence comes from seafloor spreading centers: sites throughout the
ocean where plates of
ocean crust move apart and magma erupts in between, building
new crust onto the plates» trailing edges.
A
new ocean drilling expedition will try to settle the question by drilling into
crust where high temperatures are found unusually close to the sea floor, bringing life's thermal limit within reach.
To untangle the impacts that these three climate stressors will have on seafloor diversity in the future, the researchers examined existing published data and collected
new data on organisms living in deep - sea sediments in upwelling regions along continental margins, where the
ocean and continental
crusts meet along the seafloor.
Just as on land, we learn about
ocean volcanoes by studying vibrations to see what is happening deep inside as plates separate and magma rushes up to form
new crust.
As for Dione, the
new study finds it harbors a deep
ocean between its
crust and core.
A global
ocean lies beneath the icy
crust of Saturn's geologically active moon Enceladus, according to
new research using data from NASA's Cassini mission.
They formed along the Gakkel Ridge, a lengthy crack in the
ocean crust where two rocky plates are spreading apart, pulling
new melted rock to the surface.