The Death of Heezen

Bruce Heezen, 1975

Bruce Heezen, 1975

The Des Moines Register described Bruce Heezen as a large man. This, they said, contributed to his early death at age 53, on this day in 1977. But when we look at photographs of Bruce Heezen, he doesn’t appear to loom so large. Husky, they called that shape back in the 1970s. Normal, we call it today. We will get to his untimely death and its unusual circumstance in a few moments.

The native Iowan – a farm boy who grew up raising turkeys – played an important role in plate tectonics theory. But Continue reading

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Mountains by Destruction

The Blade - vertical beds of sandstone

The Blade – vertical beds of sandstone

Gustave-Émile Haug. Now, there’s a name you don’t hear everyday. Unless you specialize in the obscure. But everyone has a birthday, today would have been Haug’s, so let us remember the French geologist for his role in helping to develop the failed geosynclinal theory of mountain building. Born in 1861, his 1907 Traité de géologie was “an invaluable reference” to those who valued it. It spoke of the way seaside synclines – actually massive trenches – fill with continental sedimentary runoff, then mysteriously rebound as mountain ranges. Haug’s playground was Continue reading

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Earth’s Mid-life Crisis

maninhammockSome researchers think the Earth went through a mid-age doldrum, a sleepy period of listless ennui. Its plates slowed down, they claim. Or maybe stopped churning completely. For about a billion years, (1.7-.75 bya) the planet was boring. No serious tectonic excitement. Instead, supercontinent Roodinia assembled and then sat like an old frog on an old log on the ocean, doin’ nothin’.

Professor Kent Condie (New Mexico Institute of Mining and Technology) says that crustal movement may be speeding up since those days of yore. He wasn’t there in the old days, so we assume he has used some geo-magic to learn this. And he apparently has. Geomag signatures in old rock indicate to Condie that the plates  (previously usually thought to move at a stable pace) are picking up speed. It is not Continue reading

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How Hot is Hot?

Sorry, photograph of the core-mantle boundary is temporarily unavailable.

Sorry, photograph of the core-mantle boundary is temporarily unavailable.

How Hot is Hot?  4,000 degrees K, according to new study.  Researchers at the Magma and Volcanoes Laboratory (CNRS U Blaise Pascal) and the European Synchrotron (ESRF) have collided to make sense of the really hot temperatures at the core-mantle boundary. The CNRS-ESRF study, “New Insight into the Temp- erature of Deep Earth,” has mimicked the conditions at 2,900 kilometres below surface. Plate tectonics theory tells us that our ocean crust is subducted towards that mantle-core interface. CNRS-ESRF tells us that at the boundary temperatures rise rapidly to 4,000 K and the basaltic former crust produces a silica-rich liquid that reacts with the surrounding mantle material. As one approaches the lower mantle (hopefully in an insulated jump suit), one finds that the temperature gradient increases more rapidly than it does at shallower mantle depths. The scientists tell us that the temperature increases about 1,000 in the last few hundred kilometres.

The point of the study was to observe what happens to basalt as it approaches lower-mantle conditions. This was achieved in the lab. Discovering the traits of the basalt seems to have shed some light on mysteries surrounding seismic wave propagation in the D” (D” being geo-speak for the mantle-core region). By recreating a pressure of 46 GPa (That’s right, 46-gazillion pascals of pressure!) the team found that they had created a basaltic slurry that could be giving the seismic anomalies others have observed. They realized that the temperature would have to be between 3800 and 4150 K  for this to occur, hence their prediction that this is the D” zone’s temperature. You can read the paper by Denis Andrault et.al. in the journal Science by following this link.

It is interesting that we are still working out the temperatures down there. In The Mountain Mystery, I told part of the story of Joseph Fourier and his thought-experiment that placed a piece of the Sun 12 miles below our surface. He said it would take 200,000 years before the dissipating heat reached the surface through conduction. Fourier pre-dated Lord Kelvin with heat-transfer calculations and his math was better, but Kelvin was a powerful force and his errors about the Earth’s temperature, heat dissipation, and the planet’s age are what we remember today. Kelvin thought the Earth’s internal heat was largely residual and the Sun’s heat was due to gravitational pressure. (When radiation and X-rays were discovered, the elderly Kelvin declared them to be hoaxes.)  Consequently, he opted for a young-aged Earth of some 20 million years. He also soundly rejected the idea of mantle convection when it was presented to him by his colleague and assistant, John Perry in 1898. Perry published his idea in Nature and Kelvin ruined his career for his insubordination. And yet, we calculate the core-mantle boundary temperature as 4,000 K. Four thousand Lord Kelvins – now that’s a disturbing mental image!

Read the book,  The Mountain Mystery.

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Oklahoma – An Earthquake Hot Spot?

USGS Oklahoma Seismicity Map

USGS Oklahoma Seismicity Map

When we think of American earthquakes, we think of California where the huge plates of the San Andreas are slip-sliding past each other. Or maybe the south coast of Alaska, near the subduction zone that formed the Aleutian and Kuril island arc chains. But Oklahoma? Not likely. In the former case, the continental transform fault marks the boundary between the North American and Pacific Plates. In Alaska, the subduction of the Pacific Plate under the North American Plate create the dish rattling. But Oklahoma’s bull’s-eye forces more than a moment’s pause to see how it fits with the general scheme of plate tectonics.

In a recent USGS press release, the government says earthquake activity in Oklahoma has been surging. Although Oklahoma has long been known as Continue reading

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Kickstarting Tectonics

The Mountain Mystery. tells the story of how (most) geologists and geophysicists finally agreed that plate tectonics moves the continents, opens ocean basins, and scrunches crust into mountains. But what started the tectonic motion? Most of us assume that the scheme kicked into action about three billion years ago as a result of temperature differentials – the lower mantle was (and is) hotter than the near-surface. As heat dissipated, convection currents began.

We are fairly certain today that convection is moving the continents. As Robert Dietz wrote in “Continent and Ocean Basin Evolution” in 1963:

Thermal convection cells in the mantle provide the fundamental driving force and the mid-ocean rises mark their divergence while the continents tend to lie over the convergences. . . The principle novelty of this concept is that no fixed layer separates the sea floor from the convection process; rather the ocean bottom is the exposed and outcropping limb of this convection. Although perhaps alarming at first thought, seafloor spreading is an orderly, evolutionary and actualistic process consonant with geologic history.”

The bold lettering is mine, added to be sure you noticed what Dietz is saying – the ocean crust is part of the moving convection cell. Dietz calls this alarming. Creepy is another good word. His thesis – sometimes called the “Commotion in the Ocean” paper – followed Harry Hess’s work and generally spoke the same words regarding spreading seafloor and mobile crust.

But is it necessary to have convection currents dissipating the Earth’s primordial heat? Lord Kelvin didn’t think so. And he made life unbearably difficult for his long-suffering assistant and junior professor, John Perry, who disagreed with him. Perry tried to convince the Lord of the possibility of mantle convection currents. Lord Kelvin believed the planet was solid to the core and nothing inside flowed. He had calculated that Earth cools only through conduction and his math showed the planet has been cooling since it formed 20 million years ago. That’s right – 20 million years. That’s almost as wrong as 6,000 years. In 1900, when Kelvin was tossing Perry out of his office (because Perry had published in Nature that the Earth is over a billion years old and the mantle dissipates heat via convection), Kelvin stubbornly refused to entertain anything close to a billion years as even remotely possible. Kelvin insisted the planet lost heat through conduction alone and his calculations arrived at something around 20 mya, based on the planet’s rate of heat loss.

Kelvin may have been right about conduction, except he got the planet wrong. Mercury and Mars likely lost their primordial heat mostly through conduction. Not so with planet Earth. The mantle moves, and it seems it has been in motion for a long time.

asteroid impactA recent article in Astrobiology Magazine reports tectonics may have been kickstarted by a 50-kilometre-wide space rock that crashed into what we now call South Africa. This is according to Donald Lowe and Norm Sleep who published their thoughts in the journal Geochemistry, Geophysics, and Geosystems. Their paper, “Physics of crustal fracturing and chert dike formation triggered by asteroid impact, ∼3.26 Ga, Barberton greenstone belt, South Africa.” alleges that the asteroid locally fractured the primitive crustal plate. Others have pointed out that the Late Heavy Bombardment era, as that time in Earth’s history was called, experience a lot of ‘heavy bombardments’ all of which helped break up the plates – perhaps into today’s known pieces.  Would the plates arisen and then moved from convection alone, or was the bombardment a necessary prerequisite? Or was the bombardment simply coincidental to the beginning of crustal mobility? Do we know?

Read the book,  The Mountain Mystery.

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Searching for Haida Gwaii

haidagwaiibook

The just-released book

Haida Gwaii. Totem poles and sea mist shroud the west coast islands of Canada. Rain is occasionally heavy enough to drown a duck. (30 cm a day is possible.) Or maybe the ducks drown in the tsunamis – earthquakes give the place a good stern shaking every few years with 8.1 (1949) and 7.8 (2012) as recent examples.

Stepping off the west coast of the islands could also get a duck wet – it is a 3,000 metre drop-off into something resembling the abyss. No gradual shelf here.

 

Continue reading

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Doodling Mary Anning

Image

Today Google has a doodle honouring Mary Anning, one of palaeontology’s pioneers. The reason Google chose Anning on this day?  It remembers her birthdate – she would have been 215 years old today. Alas, she didn’t reach 50. Here is her story, lifted from the book  The Mountain Mystery:

    “Anning was a child when she found her first extinct giant. Such fossils were Continue reading

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It’s different

geologist Amos Eaton

Amos Eaton

Convicted of forgery, American attorney Amos Eaton spent five years in prison. Released at age 40, his law career ruined, and still protesting his innocence, he moved on. That was in 1815. Geology became his greatest interest and teaching was his passion. His finest accomplishment was the introduction of a new style of science education – based on learning by doing. This fit well with the new country’s ‘can-do’ philosophy and utilitarian approach to everything. Eaton’s method of hands-on teaching had a huge impact on the level of science education in the United States for the next two centuries. He sometimes embarked students on barges and floated them along the Erie Canal where they sketched rock outcrops as they drifted along. In 1824, Eaton co-founded the Rensselaer School, dedicated to the “application of science to the common purposes of life.” Today the school is known as Rensselaer Polytechnic Institute and it is America’s oldest technology university.

We are remembering Amos Eaton on his birthday today (born in 1776) because Continue reading

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Columbus rides again

columbus landing    It seems the Santa Maria has been found. Marine archaeologist Barry Clifford and his team believe they have found the sunken vessel. Columbus left Europe in August, 1492, with three ships – La Pinta, La Nina, and Santa Maria, reaching the Caribbean sometime in October. He toured the islands, visiting San Salvador, Cuba, and Haiti – picking up cheap bling to bring back to Spain so he could impress his family (and the queen). It was offshore Haiti that Columbus, captain of the boat, ran Santa Maria aground in December. He abandoned her, Mary sank in uncharted waters, Columbus abandoned Continue reading

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