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Mapping the seafloor from space
A new high-resolution marine gravity map that reveals
tiny seafloor features has been created by an international scientific team
using satellite radar measurements of the ocean surfaces.
University of Sydney geophysicist Professor Dietmar Müller is a member of
the team whose research was published today in the international journal
Science. The team combined new radar altimeter measurements from satellites
CryoSat-2 and Jason-1 with existing data to construct a new global marine
gravity model. The result is a model two times more accurate than previous models.
The new map reveals an ancient, extinct mid-ocean ridge from the Jurassic
Period in the Gulf of Mexico and a huge ancient rift scar in the South Atlantic Ocean
formed by a deep-seated "hotspot" leading to a cracking of the ocean floor.
Professor Müller says the disappearance of Malaysia Airlines flight MH370 earlier
this year has heightened global awareness of the poor knowledge of our ocean depths.
"How much do we know about what's actually down there, let alone about what's
underneath the seabed? We know much more about the topography of Mars than
we know about Earth's seafloor," he suggests.
"While thousands of metres of water obscure our view of an incredible array of
geological features populating the seafloor, satellites enable radar beam
"altimetry" topographic mapping from space.
They measure the humps on the sea surface caused by water being attracted by
submarine mountains. Conversely, sea surface levels fall above deep valleys," explains
Prof. Müller says, "The map offers an amazing glimpse of the fine-scale structure of
deep abyssal seafloor, which is normally inaccessible, including thousands of
previously uncharted seamounts."
The new map also reveals previously unknown tectonic microplates in the Pacific
Ocean as well as detailed kinks in fracture zones, linear scars on the seafloor that
trace out plate motion.
"These bends owe their existence to sudden re-organisations of the tectonic
plates, giant shake-ups that can lead to catastrophic events including episodes
of volcanism and climate change," said Professor Müller.
The unknown forces driving these changes are currently being explored by
supercomputer simulations of the slow convective churning of the deep Earth's
mantle, where rocks flow like warm toffee.
The high-resolution digital maps also provide a basis for mapping rough seafloor
patches, which affect deep ocean circulation, with potentially dramatic effects on
global climate by influencing ocean mixing.
These sorts of discoveries allow us to better understand Earth's tectonic engine
and highlight the importance of satellite imaging as one of the primary tools
for the investigation of remote ocean basins.
"One of the most important uses of this new marine gravity field will be to
improve the estimates of seafloor depth in the 80 percent of the oceans without
depth soundings. Even after 40 years of mapping by hundreds of ships one finds
that more than 50 percent of the ocean floor is more than 10 kilometres away
from a depth measurement. Between the soundings, the seafloor depth is estimated
from marine gravity measurements from satellite altimetry," Professor Müller said.