A University of Houston (UH) professor led a team of scientists to uncover the largest
single volcano yet documented on Earth. Covering an area roughly equivalent to the
British Isles or the state of New Mexico, this volcano, dubbed the Tamu Massif, is
nearly as big as the giant volcanoes of Mars, placing it among the largest in the
Solar System.
William Sager, a professor in the Department of Earth and Atmospheric Sciences at
UH, first began studying the volcano about 20 years ago at Texas A&M’s College of
Geosciences. Sager and his team’s findings appear in the Sept. 8 issue of Nature Geoscience,
the monthly multi-disciplinary journal reflecting disciplines within the geosciences.
Located about 1,000 miles east of Japan, Tamu Massif is the largest feature of Shatsky
Rise, an underwater mountain range formed 130 to 145 million years ago by the eruption
of several underwater volcanoes. Until now, it was unclear whether Tamu Massif was
a single volcano, or a composite of many eruption points. By integrating several
sources of evidence, including core samples and data collected on board the JOIDES
Resolution research ship, the authors have confirmed that the mass of basalt that
constitutes Tamu Massif did indeed erupt from a single source near the center. “Tamu Massif is the biggest single shield volcano ever discovered on Earth,” Sager
said. “There may be larger volcanoes, because there are bigger igneous features out
there such as the Ontong Java Plateau, but we don't know if these features are one
volcano or complexes of volcanoes.”
Tamu Massif stands out among underwater volcanoes not just for its size, but also
its shape. It is low and broad, meaning that the erupted lava flows must have traveled
long distances compared to most other volcanoes on Earth. The seafloor is dotted with
thousands of underwater volcanoes, or seamounts, most of which are small and steep
compared to the low, broad expanse of Tamu Massif.
“It’s not high, but very wide, so the flank slopes are very gradual,” Sager said.
“In fact, if you were standing on its flank, you would have trouble telling which
way is downhill. We know that it is a single immense volcano constructed from massive
lava flows that emanated from the center of the volcano to form a broad, shield-like
shape. Before now, we didn't know this because oceanic plateaus are huge features
hidden beneath the sea. They have found a good place to hide.”
Tamu Massif covers an area of about 120,000 square miles. By comparison, Hawaii’s
Mauna Loa – the largest active volcano on Earth – is approximately 2,000 square miles,
or roughly 2 percent the size of Tamu Massif. To find a worthy comparison, one must
look skyward to the planet Mars, home to Olympus Mons. That giant volcano, which is
visible on a clear night with a good backyard telescope, is only about 25 percent
larger by volume than Tamu Massif. The study relies on two distinct, yet complementary, sources of evidence – core samples
collected on Integrated Ocean Drilling Program (IODP) Expedition 324 (Shatsky Rise
Formation) in 2009, and seismic reflection data gathered on two separate expeditions
of the R/V Marcus G. Langseth in 2010 and 2012. The core samples, drilled from several
locations on Tamu Massif, showed that thick lava flows (up to 75 feet thick), characterize
this volcano. Seismic data from the R/V Langseth cruises revealed the structure of
the volcano, confirming that the lava flows emanated from its summit and flowed hundreds
of miles downhill into the adjacent basins.
According to Sager, Tamu Massif is believed to be about 145 million years old, and
it became inactive within a few million years after it was formed. Its top lies about
6,500 feet below the ocean surface, while much of its base is believed to be in waters
that are almost four miles deep.
“It’s shape is different from any other sub-marine volcano found on Earth, and it’s
very possible it can give us some clues about how massive volcanoes can form,” Sager
said. “An immense amount of magma came from the center, and this magma had to have
come from the Earth’s mantle. So this is important information for geologists trying
to understand how the Earth’s interior works.”
The project was funded by the National Science Foundation, both through direct grants
and through its Integrated Ocean Drilling Program, an international research program
dedicated to advancing scientific understanding of the Earth through drilling, coring
and monitoring the subsea floor.
###
Additional Contacts for Media Inquiries:
Will Sager, wwsager@uh.edu or 713-893-0717
Matt Wright, mwright@oceanleadership.org or 202-448-1254
Karen Riedel, kriedel@tamu.edu or 979-845-0910
Keith Randall, keith-randall@tamu.edu or 979-845-4644
About the University of Houston
The University of Houston is a Carnegie-designated Tier One public research university
recognized by The Princeton Review as one of the nation’s best colleges for undergraduate
education. UH serves the globally competitive Houston and Gulf Coast Region by providing
world-class faculty, experiential learning and strategic industry partnerships. Located
in the nation’s fourth-largest city, UH serves more than 40,700 students in the most
ethnically and culturally diverse region in the country. For more information about
UH, visit the university’s newsroom at http://www.uh.edu/news-events/.
About the College of Natural Sciences and Mathematics
The UH College of Natural Sciences and Mathematics, with 193 ranked faculty and nearly
6,000 students, offers bachelor’s, master’s and doctoral degrees in the natural sciences,
computational sciences and mathematics. Faculty members in the departments of biology
and biochemistry, chemistry, computer science, earth and atmospheric sciences, mathematics
and physics conduct internationally recognized research in collaboration with industry,
Texas Medical Center institutions, NASA and others worldwide.
To receive UH science news via email, sign up for UH-SciNews.
For additional news alerts about UH, follow us on Facebook and Twitter.