Total Pageviews

Showing posts with label faults. Show all posts
Showing posts with label faults. Show all posts

Tuesday, October 1, 2019

Machu Picchu: 15th Century Incan Sanctuary Purposely Built on Faults




     "The ancient Incan sanctuary of Machu Picchu constructed in the mid to late 15th century, is considered one of humanity's greatest architectural achievements. Built in a remote Andean setting atop a narrow ridge high above a precipitous river canyon, the site is renowned for its perfect integration with the spectacular landscape. Yet the sanctuary's location has long puzzled scientists -- Why did the Incas build their masterpiece in such an inaccessible place? Research suggests the answer may be related to the geological faults that lie beneath the site."(Wow, ancient ecoarchitects meet ancient Scientific Stephs ;-)).

       "On September 23, 2019, at the Geological Society of America (GSA) Annual meeting Dr. Rualdo Menegat, a geologist at Brazil's Federal University of Rio Grande do Sul,  presented the results of a detailed geoarchaeological analysis that suggests the Incas intentionally built Machu Picchu -- as well as some of their cities -- in locations where tectonic faults meet. "Machu Pichu's location is not a coincidence," says Dr. Menegat. "It would be impossible to build such a site in the high mountains if the substrate was not fractured."


    " Using a combination of satellite imagery and field measurements, Menegat mapped a dense web of intersecting fractures and faults beneath the UNESCO World Heritage Site. His analysis indicates these features vary widely in scale, from tiny fractures visible in individual stones to major, 175-kilometer-long lineaments that control the orientation of some of the region's river valleys."


     "Dr. Menegat found that these faults and fractures occur in several sets, some of which correspond to the major fault zones responsible for uplifting the Central Andes Mountains during the past eight million years. Because some of these faults are oriented northeast-southwest and others trend northwest-southeast, they collectively create an "X" shape where they intersect beneath Machu Picchu. X marks the Machu Picchu spot.



     "Dr. Menegat's mapping suggests that the sanctuary's urban sectors and the surrounding agricultural fields, as well as individual buildings and stairs, are all oriented along the trends of these major faults. "The layout clearly reflects the fracture matrix underlying the site," says Dr. Menegat. Other ancient Incan cities, including Ollantaytambo, Pisac, and Cusco, are also located at the intersection of faults, says Menegat. "Each is precisely the expression of the main directions of the site's geological faults."



     Dr. Menegat's results indicate the underlying fault-and-fracture network is as integral to Machu Picchu's construction as its legendary stonework (as above). This mortar-free masonry features stones so perfectly fitted together that it's impossible to slide a credit card between them. Aside from the obvious aesthetic benefits of this building style, there are engineering advantages. Peru is a seismically unstable country; both Lima and Cusco have been leveled by earthquakes. When an earthquake occurs, the stones in an Inca building are said to “dance;” that is, they bounce through the tremors and then fall back into place. Without this building method, many of the best known buildings at Machu Picchu would have collapsed long ago.




       "As master stoneworkers, the Incas took advantage of the abundant building materials in the fault zone, says Dr. Menegat. "The intense fracturing there predisposed the rocks to breaking along these same planes of weakness, which greatly reduced the energy needed to carve them."





     "In addition to helping shape individual stones, the fault network at Machu Picchu likely offered the Incas other advantages, according to Dr. Menegat. Chief among these was a ready source of water. "The area's tectonic faults channeled meltwater and rainwater straight to the site," he says. Construction of the sanctuary in such a high perch also had the benefit of isolating the site from avalanches and landslides, all-too-common hazards in this alpine environment, Dr. Menegat explains."




     "The faults and fractures underlying Machu Picchu also helped drain the site during the intense rainstorms prevalent in the region. "About two-thirds of the effort to build the sanctuary involved constructing subsurface drainages," says Dr. Menegat. "The preexisting fractures aided this process and help account for its remarkable preservation," he says. "Machu Picchu clearly shows us that the Incan civilization was an built on well-fractured rocks. 

Have any PEOTS folks visited Machu Picchu? How was the experience?

And Happy 6 year anniversary to PEOTS! 


  • We had a Japanese cardiologist stay with us in March 2008. He took the leftover Colorado trail GORP with him to his next stop at MP and sent this image. So it's almost like I've been there...and it looks deserted.




Tuesday, November 25, 2014

Mazarine Deep Blue, Oldest Paris Public Library Mazarine, and Transform Faults of the Deep Dead Sea

           Any day I learn a new word, especially a colorful one, is a good day. Mazarine blue made Tuesday for me this week:



           Apparently it is all the rage in athletic footwear colors as an internet search of images produced butterflies,





shirts,




and an inordinate amount of running shoes:



       
           It is also the name of the oldest public library in Paris, dating to 1643:




     How to get from a deep, deep blue, to the oldest public library in Paris, to the lowest elevation on earth (excluding subsea topography, of course) in the Rift Valley of the Dead Sea?



          Just look at that mazarine blue color of the Dead Sea, which is up to 34 percent saline, nine times the salinity of the ocean, and is over 1,000 feet at its deepest point. The Dead Sea straddles Israel/Palestine to the west and Jordan to the east:


     The Dead Sea is part of the longer and larger rift zone extending from the Red Sea through the Gulf of Aqaba and through the Dead Sea via the Dead Sea Rift Zone or Dead Sea Transform Fault:
         




          This left lateral-moving transform fault lies along the tectonic plate boundary between the African Tectonic Plate and the Arabian Tectonic Plate. It runs between the East Anatolian Fault zone in Turkey and the northern end of the Red Sea Rift offshore of the southern tip of Sinai Peninsula.

          The geologic history of the area is the subject of much debate. It is a complicated area both geologically and politically.

          The blue of the Dead Sea water approaches Mazarine Blue, yes?


          Mazarine Blue: new to you? Thoughts on the Dead Sea transform fault and the Dead Sea rift zone?

Happy Mazarine Blue Thanksgiving!
Steph  






     

Tuesday, May 6, 2014

Fast and Slow Rates of Tectonic Change: New Zealand and Arizona

     I received an alert from The New York Times today with this "breaking news" about climate change. Temperatures rising slightly less than 2 ° F are certainly cause for concern but, for most scientists it is hardly breaking news. The data are important, though, especially the possible projected rise in mean temperatures by up to 10 °F by the end of this century:

        CLIMATE CHANGE REPORT

    As a focus today, I'd like to compare the relatively quickly-changing tectonic geomorphology of New Zealand to the much slower-changing tectonic geomorphology of Arizona.
Tectonic geomorphology involves the interplay of surface features with underlying tectonics.

     In this geologic map of New Zealand, rates of up to 5 mm uplift per year are noted in red:




      Areas of rapid uplift are marked by active faults, seismic activity, waterfalls, and newly developing stream systems:





     New Zealand sits at the junction of the Australian and New Zealand tectonic plates and displays the features of a rapid convergent plate tectonic zone.

      In contrast, Arizona sits within the North American plate, rather than at the convergence of two plates. The fluvial (river) geomorphology is well developed and integrated. The landscape has had long periods of time to adjust to ancient fault scarps creating well-developed alluvial fans:


     One of the most interesting parts of tectonic geomorphology to me is that features like alluvial fans may also mark places of more rapid uplift, where the alluvium is adjusting to more active uplift as in here in Iran:



     But, back to climate change (you knew I'd get back there, right?), the increased overall temperatures, torrential downpours, and periods of drought are all intimately connected to this skin of our earth. The climate we are changing will inevitably affect the tectonic geomorohology as landscapes adjust to the wide swings in temperature and rainfall.

      Looking forward to your thoughts on this interplay of climate and tectonic geomorphology, all you alluvial fans!

Tectonically,

Word Woman (aka Scientific Steph)


P.S.

Mid May in the Colorado Mountains: