I have experienced all three types,, Vertical plate motion, horizontal, and both motions at once. The vertical one I call the "rumbling turd quake".
It's like a hard bowel movement that rolls down the intestines like a bowling
ball and blows out with one great vibrating jolt. The second (horizontal) I call the "drunken quake"
because at first one might feel drunk or that one has lost their equilibrium. It sways back and forth
sometimes like a baby's cradle but other times with enough force so
that you lose your balance.
The third is the "full monty" because it contains the
other two motions. It is the most dangerous and causes the most damage. There was one about a year ago,,
its epicenter 300 kilometers away. That was a full monty. However most of
the quakes I have experienced have had epicenters far from Tenancingo on the pacific coast.
I originally came from the northeast, a relatively quiet area seismically,, at least in comparison to Mexico. Eighty percent of all quakes occur on the pacific rim of fire, and Mexico's pacific coast is part of that rim. When there is an earthquake in Pinotepo in Oaxaca we feel it here. The appalachians are for the most part tranquil,, their volcanic days a distant memory. The mountains around Tenancingo remind one of a relatively recent volcanic past,, geologically speaking. On the northwestern horizon the dormant volcano, Nevado de Toluca or Xinantecatl is visible and often covered in snow.
Xinantecatl
From the top of Christo Rey in Tenancingo one can see Popocatepetl smoking. }
The geology of Mexico is volcanic and more recent than the northeast. Rocks here look so different from the granite, shale,and sandstones I was used to. If you drive 9 miles west of Tenancingo there are mountains of white-gray limestone that glisten with crystals. The limestone was deposited by ancient sea then volcanically reborn as something "other". A few years ago the town opened a dump on the side of a small mountain in front of Pueblo Nuevo. When they cut deep into the mountain side to gain a flat area black porous lava rock was exposed like that found at Paricutin, the most recent volcano on earth found in the State of Michoacan.
And then there is Paricutin, Hephaestus's sudden outburst. I remember reading its history when I was a little boy just five years after the event. The geology in my zone seemed ancient and predictably stable. I was young and didn't know the geologic nuances under my feet. An earthquake was non-existant. Rocks were usually dark-greenish-gray to black, fine-grained, dense, hard basalt that they broke up for driveways. The most unusual rock I ever found was a piece of coke from the coal burning days that I dug up near the foundation of the house. A decorative brick seemed more unusual than the rocks of the area.
When I read about Paricutin I tried to imagine a volcano spurting out of the ground one day in the backyard then burying our entire town. Paricutin is the youngest volcano of its kind and is also considered one of the new wonders of the world. One day it revealed itself to Dionisio Pulido, who, while working his land heard the earth rumble at his feet, then open up, and begin to spout steam. Gradually a hill grew into mountain with a height of more than 2,808 meters. By the time it achieved that height the eruptions were terrifying, some thought eternal, because the volcano spewed lava for 9 years 11 days and 10 hours, then sputtered, and stopped.
Paricutin at night
During After
I was lucky enough to see Paricutin in person a few years back and crawl around the sharp black lava fields and the ruins of the church in the pueblo that doesn't exist anymore called, San Juan Parangaricutiro. One sees the destruction,, the church tower more like a disconnected cruel sculpture, and there is a silence now. Birds sing and the only sizzle is of gorditas on the comal of Doña "Lite", the Purepecha that has one of the puestos nestled in the lava field.
Xinantecatl
From the top of Christo Rey in Tenancingo one can see Popocatepetl smoking. }
The geology of Mexico is volcanic and more recent than the northeast. Rocks here look so different from the granite, shale,and sandstones I was used to. If you drive 9 miles west of Tenancingo there are mountains of white-gray limestone that glisten with crystals. The limestone was deposited by ancient sea then volcanically reborn as something "other". A few years ago the town opened a dump on the side of a small mountain in front of Pueblo Nuevo. When they cut deep into the mountain side to gain a flat area black porous lava rock was exposed like that found at Paricutin, the most recent volcano on earth found in the State of Michoacan.
And then there is Paricutin, Hephaestus's sudden outburst. I remember reading its history when I was a little boy just five years after the event. The geology in my zone seemed ancient and predictably stable. I was young and didn't know the geologic nuances under my feet. An earthquake was non-existant. Rocks were usually dark-greenish-gray to black, fine-grained, dense, hard basalt that they broke up for driveways. The most unusual rock I ever found was a piece of coke from the coal burning days that I dug up near the foundation of the house. A decorative brick seemed more unusual than the rocks of the area.
When I read about Paricutin I tried to imagine a volcano spurting out of the ground one day in the backyard then burying our entire town. Paricutin is the youngest volcano of its kind and is also considered one of the new wonders of the world. One day it revealed itself to Dionisio Pulido, who, while working his land heard the earth rumble at his feet, then open up, and begin to spout steam. Gradually a hill grew into mountain with a height of more than 2,808 meters. By the time it achieved that height the eruptions were terrifying, some thought eternal, because the volcano spewed lava for 9 years 11 days and 10 hours, then sputtered, and stopped.
Paricutin at night
During After
I was lucky enough to see Paricutin in person a few years back and crawl around the sharp black lava fields and the ruins of the church in the pueblo that doesn't exist anymore called, San Juan Parangaricutiro. One sees the destruction,, the church tower more like a disconnected cruel sculpture, and there is a silence now. Birds sing and the only sizzle is of gorditas on the comal of Doña "Lite", the Purepecha that has one of the puestos nestled in the lava field.
In 1985 an 8.1 earthquake shook Mexico City leaving vast destruction and killing thousands. On this day in 1985, a magnitude 8.1 earthquake rocked Mexico City and its surrounding environs at 7:17 AM central time.The quake was felt as far away as Guatemala City, Guatemala and Houston, Texas, over an area of about 319,000 square miles 825,000 square kilometers, but the most intense shaking occurred in Mexico City, Ciudad Guzman and the Pacific Coast towns of Lazaro Cardenas, Ixtapa and La Union, according to the U.S. Geological Survey. Tenancingo is 100 kms. from Mexico City and in 1985 buildings were dancing, but there was a more severe quake a few years later that tumbled the parochial school. My wife remembers that one when the buildings swayed so much it seemed they would topple over. I don't ever want to experience one of those. One feels out of control even with a small quake yet respectful of this power to move the earth underneath your feet even if it originated hundreds of kilometers away.
We live close to Mexico's trans mexico volcanic belt. Above the Nevado de Toluca is moving east. Below that,, where we are located, is moving west. In 5 million years I will have beachfront on the pacific coast.
The trans Mexican Volcanic belt is a subduction zone that runs across central Mexico. Volcanoes both active and dead protude like pimples across this swath of Mexico. The volcanic activity over millions of years has been responsible for the great height above sea level in central Mexico. The result of this uplift is the best kept climate secret in the world. Tenancingo, for example, is 18 degrees above the equator. It should be infernally hot but the height, 2020 meters above sea level, gives us warm days and cool nights. I can grow bananas, apples, and oranges and many of the plants are similar to the far north.
As
such, the majority of the Mexican central and northern territories are
located at high altitudes, and the highest elevations are found at the
Trans-Mexican Volcanic Belt: Pico de Orizaba (5,700 m, 18,701 ft),
Popocatépetl (5,462 m, 17,920 ft) and Iztaccíhuatl (5,286 m, 17,343 ft)
and the Nevado de Toluca (4,577 m, 15,016 ft). - See more at:
http://www.eosnap.com/tag/trans-mexican-volcanic-belt/#sthash.PSXStlzk.dpuf
May all your earthquakes be mild ones, not wild ones.
ReplyDeleteThank you for your comment. I have never received one before. And by the way there hasn't been an earthquake in a long time,, at least one that moves the hanging lamps.
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