
Estava encantada amb el seu noi, semblava l'amant perfecte, i el marit ideal, fins que va despertar després d'aquell cop que va rebre en el seu cap,amb la taula al caure del fort impacte d'una mà que li era coneguda.
El perill de certes reflexions (com la que jo encete ara) és la seua pretensió de generalitzar a partir d’un suposat determinat i, de vegades, puntual. Però tot i així, de quan en quan, em trobe amb persones, de conviccions abrandades pel moment de la discussió, que se senten fidelitzats fins al moll de l’os en possicionaments fàcilment discutibles. Conec gent que fins i tot saliva més del compte quan parla de l’avortament. El seu bagatge ideològic els situa clarament i incondicionalment en contra mentre intenten augmentar el pes específic de la seua minsa i peregrina argumentació amb paraules com “assassinat”, “homicidi legalitzat”, i altres perles que, supose, a l’alçada d’aquesta entrada ja tots s’haureu imaginat. El que em sembla francament curiós és que aquestes mateixes persones no dubten en resoldre els conflictes professionals o, fins i tot, personals, de maneres ben expeditives, sense que els tremole la sensibilitat de les seues conviccions. No se n’amaguen de glorificar, per exemple, els mètodes disciplinaris a l’escola del franquisme per tal d’acabar de colp (mai millor dit) amb els “defectuosos” que ara miren d’amagar-se rere els qualificatius de “hiperactius”, “dislèxics”, etc. i que endarrereixen les ànsies d’acabar homogèniament un programa curricular pensat des del despatx d’algun psicopedagog desenfeinat. Tampoc dubten en defensar la pena de mort per a “certs casos”, perquè són l’única manera de tallar de soca-rel el càncer de tanta violència i inseguretat al carrer. Ja no entrarem amb les solucions que exposen sobre la immigració, ni el que pensen sobre la igualtat entre homes i dones, ni el que farien amb la democràcia que, al seu parer, no causa més que problemes i mal de caps. Em faig creus al pensar com acceptarien ells finalment (i gestionarien posteriorment) la naixença de criatures generades en experiències espatllades. Ja he dit al principi que les troballes puntuals no poden generalitzar-se. De ben segur que hi haurà qui, des de la tolerància i la sensibilitat més exquisida, seran capaços de posar damunt la taula fets que permeten la discussió asserenada i la reflexió. Jo, no en conec encara (no perd l’esperança tampoc). Simplement us conte el que em trobe de quan en quan.
You can also clearly see the Mid-Atlantic Ridge, an underwater mountain range in the Atlantic Ocean where two tectonic plates are moving away from one another. If you look closely, you can see this ridge connects with others around the globe, forming a nearly continuous mountain range that is over 60,000 kilometers long.But so far nothing has sparked quite as much interest as this funny looking pattern off the west coast of Africa:
Patterns like this can actually be seen over much of the ocean floor in Google Earth. What is it? Is it real? Why does it look like this?
Some have speculated that these are the plow marks of seafloor farming by aliens. If there really are little green men hiding somewhere, the ocean's not a bad place to do it. Mars, Venus, the moon, and even some asteroids are mapped at far higher resolution than our own oceans (the global map of Mars is about 250 times as accurate as the global map of our own ocean).
One theory that's gained more traction is that these marks might be the ruins of the lost city of Atlantis. If that were the case, some of the city blocks would have to be over eight miles long - that's about fifty times the size of a city block in New York City (if you zoom in and use the measurement tool in Google Earth, you can do this comparison yourself).
So what is it? The scientific explanation is a bit less exotic, but we think it's still pretty interesting: these marks are what we call "ship tracks." You see, it's actually quite hard to measure the depth of the ocean. Sunlight, lasers, and other electromagnetic radiation can travel less than 100 feet below the surface, yet the typical depth in the ocean is more than two and a half miles. Sound waves are more effective. By measuring the time it takes for sound to travel from a ship to the sea floor and back, you can get an idea of how far away the sea floor is. Since this process — known as echosounding — only maps a strip of the sea floor under the ship, the maps it produces often show the path the ship took, hence the "ship tracks." In this case, the soundings produced by a ship are also about 1% deeper than the data we have in surrounding areas — likely an error — making the tracks stand out more. You can see all of the soundings that produced this particular pattern with this KMZ file.Echosounding with sonar is currently the best method for collecting this kind of data, but it's not perfect. One challenge is that it's quite slow. It has to be done from ships or underwater vehicles, and they can't go very fast or they'll spoil the measurement. As a result, not much of the ocean has been mapped this way, and huge gaps remain all over the ocean. In fact, the typical hole between tracks is about 20,000 square kilometers, or about the size of the state of New Jersey.
Now you're probably wondering where the rest of the depth data comes from if there are such big gaps from echosounding. We do our best to predict what the sea floor looks like based on what we can measure much more easily: the water surface. Above large underwater mountains (seamounts), the surface of the ocean is actually higher than in surrounding areas. These seamounts actually increase gravity in the area, which attracts more water and causes sea level to be slightly higher. The changes in water height are measurable using radar on satellites. This allows us to make a best guess as to what the rest of the sea floor looks like, but still at relatively low resolutions (the model predicts the ocean depth about once every 4000 meters). What you see in Google Earth is a combination of both this satellite-based model and real ship tracks from many research cruises (we first published this technique back in 1997). If you zoom in and take a look around the ocean for yourself, you can see higher resolution patches where ships have studied the sea floor and all the places we've still yet to explore. Here's a good example just north of Hawaii: So, what if we really wanted to find Atlantis? We probably couldn't do it with satellites — man-made structures simply aren't big enough to be measured that way. But we could map the whole ocean using ships. A published U.S. Navy study found that it would take about 200 ship-years, meaning we'd need one ship for 200 years, or 10 ships for 20 years, or 100 ships for two years. It costs about $25,000 per day to operate a ship with the right mapping capability, so 200 ship-years would cost nearly two billion dollars. That may seem like a lot of money, but it's not that far off from the price tag of, say, a new sports stadium.
For now, keep exploring the ocean in Google Earth, and continue to share what you discover. It's great to have so many sets of eyes looking at the data currently in Google Earth and asking questions about what it represents. We and our fellow oceanographers are constantly improving the resolution of our seafloor maps, so we promise to work with Google to keep the virtual explorers out there busy.