Tag: Earthquakes

Danger-Maps, Belief and New Madrid

Danger-Maps, Belief and New Madrid

Schwedigon pagoda, Yangon, Myanmar
Schwedigon pagoda, Yangon, Myanmar (2000) Photo (c) Karen Abrahamson

Most of the maps I’ve written about over the past year have been maps setting out the geographic formations of the world—regardless of how skewed the map-maker might have made the map in order to influence the beliefs of others. But some maps are made to represent truth and to save populations from dangers, so today we’re going to look at a specific type of map—those used to convey earthquake danger. I’ve been researching this because it relates specifically to the current novel I am writing called Aftershock.

Most of us are familiar with California’s San Andreas fault, the 800 mile long fault that stretches northwest-southeast in California and that brings Los Angeles (west of the fault) two inches closer to San Francisco (east of the fault) each year. This much-talked about fault line has been the subject of disaster movies and books, and also of reams of geological research. The damage caused by the fault’s quakes led the State of California to have the San Andreas and other surface faults mapped and to require disclosure of proximity to fault lines in any residential real estate dealings in the state. The trouble is, that even though these maps are available, most people – even those who have lived in proximity to a faults line seem uninformed about the dangers and new buyers of homes are positively unaware of their proximity to faults even though they sign disclosures in their ‘offer to purchase’ agreements. Why? Because maps and the language around them can either be used to convey danger or to minimize it. In the case of the California real estate disclosures they say that the house is in the San Andreas zone, but they don’t specifically use the language ‘earthquake fault zone’.

Cypress knees and trees, Orlando (2012) Photo (c) Karean Abrahamson

Another example or earthquake danger maps, and one dear to my heart (given I live on the south coast of British Columbia, Canada), are the ones that show the Ring of Fire around the Pacific Ocean basin. Nothing brings home the dangerousness of the place I live as seeing the numerous dots presenting quakes over 4.0 magnitude in recent history around the Pacific. You see, there are so many dots that a thick black line extends around virtually all of the Pacific except for the stretch bordering the Antarctic and a small section of North America – the part of the coast where I live. Okay, so there hasn’t been a moderately sized quake here in the past 20-30 years (yes, Seattle has had one, but not here, so far). In fact there hasn’t been a really big one here in a heck of a lot longer than that. But historical evidence and that ring of dots around the ocean says that there’s a very good chance one will happen one of these days. Around here we grow up being told to be earthquake prepared. Are we? Given the number of schools that haven’t been seismically upgraded, I’d say ‘no’, even though the maps are there to show us the danger.

So why do we refuse to listen to the maps? A likely answer lays in another part of America. Right in the heartland of the U.S., where Missouri, Tennessee, Arkansas and Kentucky meet, in 1811/12 near the small community of New Madrid, a series of massive earthquakes (magnitude 7.5 and 8) wiped out entire fledgling towns, sent sand and water geysering into the air and lifted huge chunks of the landscape. The only thing that stopped huge loss of life was the fact that few people lived there.

Research into the quake says this type of quake will happen again. The trouble is the quake zone isn’t at the edge of a tectonic plate and there isn’t something like really a visible fault line to show where the quake will occur because these quakes occur far underground—that’s also why they are so devastating—and so life in the Midwest has mostly been focused on the danger of tornadoes, rather than the lurking danger right underfoot.

Sunrise over Porto, Portugal. (2005) Photo (c) Karen Abrahamson.

The trouble with this type of deep earthquake is that shockwaves travel farther and wreak more damage. In fact, geologists predict that such a quake today would be felt from Colorado to Washington D.C. and could wipe out most of the country’s central infrastructure.

As a result when, in 1990 a prominent inventor named Iben Browning predicted a major quake would occur in the New Madrid fault zone between December 1 and 5th of that year, the media promulgation of maps showing concentric areas of damage seriously impacting cities like St. Louis, Nashville, Birmingham, Little Rock, Jackson and Chicago started to get people taking the danger seriously. Children were kept home from school during the danger days. T.V. crews descended on the area like flies on road kill and everyone held their breath.

When nothing happened, of course finally people began to listen to the scientists who had previously laid out why the big one wasn’t likely to happen at that exact place and time. But the maps had done their damage. They’d laid out a ‘cartography of danger’ that hadn’t arisen. As a result, even though the states of Kentucky, Missouri, Arkansas and Tennessee try to prepare people for earthquakes because the risk of the big one still exists, they have an even more uphill battle than they do in California or here in the Pacific Northwest. You see, seeing a fault line on a map may not bring home the importance of believing, but when what you believe the danger presented on the map and then nothing happens, you’re less likely to believe in future danger.

So when the big one does hit, it will be Aftershock, indeed.

A pile of bricks is all that remains in earthquake-prone Peru. The ruins of Huaca Pucllana, Miraflores, Peru. (2011) Photo (c) Karen Abrahamson.

 

Books and Geology: Mapping Beneath the Surface

Books and Geology: Mapping Beneath the Surface

Cliff-side Monastery, Spiti Valley, India (2000)
Cliff-side Monastery, Spiti Valley, India (2000)(photo (c) Karen Abrahamson)

Recently I was reflecting on the difference between plot and story, with plot being the events that happen to keep the story moving, and ‘story’ being what the book is about and the changes that occur to the characters along the way. Frodo starts out as a happy young hobbit, and returns as someone who understands the price that must be paid for the safety of places like the Shire. Bella starts out as this infatuated, clumsy girl who constantly has to be rescued, and turns out to hold the secret abilities to save everyone.

This got me thinking about mapping beneath the surface. In a book, if you are a plotter, you map out where the actions occur, but also the impact the scene has on the character. I started out writing this way, and used wonderful planning sheets like these. This has allowed me to layer stories with the emotional changes that make a story much richer to read.

A similar process has occurred in mapping the world. Once the surface mapping was well under way, people began to wonder how to map the landscape under the layer of dirt and forests we see. Why? To gain a better sense of the layering of the landscape and the connections between places. For example, the discovery of similar strata layers in both France and England demonstrated that once they were a single land mass.

The process of mapping the underside of the earth began around 1750 when a Frenchman named Jean Etienne Guettard asked just such a question about England and France. Though he posed the question, the first person taken seriously for geological mapping was an Englishman named William Smith who spent a quarter of a century mapping England and Wales beneath the ground. Smith had been a surveyor’s helper and a keen observer who noticed and recorded things like strata exposed in hillsides and in mine shafts. Smith was the first person to have the insight that different strata held different fossils from different time periods, which provided a means to date the strata. He also noted that similar fossils were found in similar strata, even though they were separated by long distances. In 1815, the result of his study was a many-colored map of England and Wales that set out the different geological formations.

Off to the fields, Pumamarka (2011) Photo (c) Karen Abrahamson
Off to the fields, Pumamarka (2011) Photo (c) Karen Abrahamson

Such a map can set out the distribution of various geological units such as glacial debris (if it was near the surface) or deeper formations like igneous, metamorphic or sedimentary rock that underlie the topsoil. Of course, having a general picture of the structure of the earth wasn’t enough for a civilization with an increasing thirst for oil and minerals, so processes were developed that measured gravitational attraction from which geologists could deduce the nature of the subsurface geology. Other processes drew on the ancient Nordic use of magnets to locate ore bodies. A more modern magnetometer was developed in the 1930s and mounted on aircraft to gather readings. The Seismic method was developed after 1875 when an English geologist in earthquake-prone Japan, thought to use a seisomograph to determine where the quakes arose from. A similar process was used in 1909 to discover the boundary between the Earth’s crust and its mantle.

Using sonic sounds or thumpers or vibrators to create sound, the sonic process then uses geophones (or hydrophones for underwater exploration) to read echoes from underground formations that tell the scientists what lies underneath.

This has led to the ability to measure the crust of the earth (which measures from about 6.5 kilometers thick under the ocean to 50-75 kilometers thick under high mountains), the mantle which extends from the crust to about half way to the centre, and the dense, partly molten core. Seismology has led to the ability to map oil deposits and layers of water and natural gas that wait in the earth’s crust. But they have also allowed scientists to reach much deeper.

Main Ghat, Varanasi
Main Ghat, Varanasi (2000) Photo (c) Karen Abrahamson

Geologists are now able to measure and map the underside of the earth’s crust (I alluded to this here). Which is a lot like understanding the underside of a novel, because, like the geothermal power of the earth that may save us from global warming,  it’s really the hot emotional underbelly of a novel that brings out the best of any novelist’s writing.

 

 

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