Seismic Circles Cover



Cover. A depiction of the seismic circles which emanated from the impact that formed the Adirondack Mountains in upper New York State, in the United States. The remains of this impact are seen in the coast line, the rivers, the political boundaries and numerous other geographical features shown in more detail on the Adirondack Mountains page, linked below.


Introduction

      This is about the meteors, asteroids and comets that bombarded the Earth over the last billion years or so, how those impacts created our geography, and how man has used those land forms. What drove me on this research is the increasing exactness in which these discoveries were made. As a child, my family would take excursions in the car, to see the country and what was there. To keep me occupied, my Mother would give me the map, and she showed me how the different lines and symbols meant different things. From that, I learned to read and understand the maps, and this set me on a course of my life that I would read and collect all the maps that I could find of the area where I was, because they gave me a better understanding of the world around me..

     In my mid 20's I was living in the State of Oregon and I came across a map of Oregon that was hand drawn, but done so to a very high degree. As I studied it, I found what looked like a large crater in the southeastern part of the State. Comparing that to other maps I had, I could only get rough 'Maybes' from them for confirmations of the idea. Then one day I ran into a much older man, a professional geologist (whose name is long ago gone), who I thought would have some insight into this, and I queried him on the idea. His response was that there were no craters on the Earth, and the reason it looked like one to me was because the map was hand drawn.

      That didn't answer my curiosity in the way I wanted to hear, but at the time there were no other sources of information available. And it stayed that way until Google Earth came along. Using that I found my childhood home, where I kissed my high school sweetheart, and a number of other such things, and then I remembered that map! "Is that possible?", I said to myself. So I went to Oregon on Google Earth and looked, and there it was, plain as day. And then - there was another one.... and another and soon I had circles that described nearly every geographic feature of those high desert plains.

     That started a journey of discovery. From there I started to see how the land was formed, over and over again there were circles, just like on the Moon. Yes, they were eroded, covered with vegetation or farmed over for many years, even centuries, but the main features were there. These impact circles formed the mountains, the rivers, the coastlines and more, all over the world.  Then after a time, I started to see that many of these impacts left not just one circle, but a series of concentric circles around them, seismic shock wave circles. And, I was increasingly amazed at how these circles expanded over vast distances, forming the geography of places hundreds and sometimes thousands of miles away from the impact. Then I started to see how man has been using the land forms created by these seismic waves, and so the research continues.
Galaleo and the Church       While much of this work is here simply to demonstrate why our world is as it is, it is also here to provide overwhelming evidence of the impacts, and how the Earth was formed to the non believers and the professionals who refuse to look at anything unless it was in their 19th century based text books.

     Hopefully some of you will use these studies as a template, and begin a search for discoveries of your own as there is still much to be done. And when you see those geographical features falling exactly on that perfect circle, you will say as I did "No Way!",  "Are you serious?", "That's incredible!" Then by studying more of the evidence you will see that yes, it is serious. Yes, it is incredible. Our world did came to be by Catastrophic Impact, and the remains of those impacts, those Seismic Circles, are what we know today as Geography.


Galileo Galilei demonstrating his telescope to the Catholic Church, the mountains on the Moon, the moons of Jupiter, and his theories that the Earth is not the center of the universe. These views were not in line with those of the church, subsequently he was tried by the Inquisition, found "vehemently suspect of heresy", forced to recant, and spent the rest of his life under house arrest.




Forward
This work is based on the works of:
Google Earth
NASA - National Aeronautics and Space Administration
Cnes/Spot Image - Centre National d'Études Spatiales the French government space agency
Data SIO    - the Scripps Institution of Oceanography, University of California San Diego
NOAA - National Oceanic and Atmospheric Administration
U. S. Navy
NGA - National Geospatial-Intelligence Agency
GEBCO - General Bathymetric Chart of the Oceans
U. S. Department of State Geographer
U. S. Geological Survey
Geo Eye
MapLink
Tele Atlas
Terrametrics
GeoBasis -DE/BKG
Europa Technologies
GIS Innovatsia
ORION-ME
DigitalGlobe
Basarsoft
European Space Imaging
Province of British Columbia
Mapabc.com
Whereis®Sensis Pty Ltd
Inav/Geosistemas SRL
ZENRIN
SK Energy
Kingway Ltd.
INEGI
Texas Orthoimagery Program
USDA Farm Services Agency
GIS Innovatsia
Mapabc.com


    These people have put together the best of the imagery of our Earth so that we can see and study our world in a way that was not possible before. They have created the tools which allow us a new understanding.


      It is a commonly accepted theory that all the continents of the Earth were joined at one time into a super continent named Pangaea. Then for some reason this super continent broke up into many pieces, or sub-continents. These sub-continents then floated around on the surface of the Earth, sometimes colliding with one another, one rising to form the mountain chains, and the other diving down returning the surface to magma. At these boundaries, volcanoes form which spew lava and ash which re-covers the Earth, all of this like a giant boiling pot. Then erosion from the atmosphere carves the river valleys and glaciation wipes everything clean. Now, finding any traces of anything that happened before all of this is further complicated by the plant life that covers the planet reclaiming any remains.

      This idea of Pangaea comes from the early 1900's where from a map of the Earth, it appeared as if the east coast of South America, and the west coast of Africa would fit together, if you cut the continents out of the map and then thought of them as a jig-saw puzzle. Then with enough imagination, subduction, erosion, volcanoes and the all powerful 'fudge factor', you could fit all the pieces back together into the super-continent Pangaea, in one shape or another. From there, if it happened once, it probably happened several times before. And so the modern Geo-sciences were born.

     However the question comes up "If the oceans were 100 feet higher, 100 feet lower, or did not exist at all, would we ever have had a theory of Pangaea?"

     Secondly, in regards to the surrounding planets that we have been able to photograph and examine with some clarity, the Moon, Mars, Venus and Mercury,  why do we not see evidence of floating continental plates there, but instead see landscapes pockmarked by a billion years of meteor impacts?

far side of the Moon

The Far Side of the Moon



      Until recently all of our observations of the Earth were made on the ground. Geographers measure the surface of the Earth and plot their findings on paper drawing maps of all sorts. While these maps are necessary and useful, using them as a basis for the Earth sciences is problematic. Maps are drawings of what we understand to be there, rather than the real thing, and the various projections used to draw the surface of a nearly spherical Earth on a flat sheet of paper distorts the dimensions, or cuts the geography into pieces, leading sometimes to questionable conclusions.

      Then came aerial surveys, photography from five or six miles up. These are good for property analysis, roads and land use planning. From these are drawn maps of excellent quality, but even with these we cannot see enough of our planet to get a good look at it, as many of the features of our Earth are 10s or 100s or 1,000s of miles across.

     Geologists use microscopes, gas chromatography, radiation, spectral analysis or other means to analyze what they found on or near the surface. Sometimes they find shatter cones, microscopic diamonds or iridium layers and this is evidence that a meteor impacted the Earth there.  This evidence is then compared with other findings to confirm the impact. This seems to work for smaller impacts, but the larger ones are beyond the scale of these methods.  Then to try to understand the past, theories come up about dust clouds from the impact that blocked out the sun, super tsunamis and strange gases that killed off all the dinosaurs with this impact or that one, many millions of years ago. 

      To understand our Earth, we need to see it as the sphere that it is, and we need to be able to see it at distances where the geographic features can be seen in their entirety, and in relation to the surrounding area. And, we need views that are as free of clouds as possible. Satellite imagery is the only way to do this.

      Google Earth has made this possible. They have assembled the imagery of a myriad of organizations and companies, which have been filled with an untold number of highly skilled scientific people, all with the quest to understand our Earth better. They have provided us with a tool from which we can see our entire planet from its' entirety, down to fine geographic detail. With this comes new understandings of our Earth.



      Our Earth was built over billions of years by the bombardment of an untold number of asteroids, meteors, comets, and extra terrestrial objects of all kinds, shapes and sizes, just like the Moon, Mars, Venus and Mercury. These impacts created the form of our Earth, building it up layer by layer, one impact after another. Gravity then pulls the Earth into a nearly perfect sphere, and the rotation of the Earth causes a bit of a bulge around the Equator. Then, with erosion from the atmosphere, vegetation covering things over, glaciation, volcanoes and other natural forces, we have what we have today.

      While very small impacts may have been obliterated by time and erosion, the larger impacts left substantial marks and many times in grandiose design. In fact, these impacts gave us our geography. They are the valley that the river flows in, the mountain top Skyline Drive that gives us those exhilarating views. They are the coast lines, the national parks and the dirt you walk over every day. The formations left from these impacts are where towns and cities where built, and many of them are our political boundaries. Often they define the way we plant our crops, where we build our roads and reservoirs, and where we find the minerals that enrich our lives. These impacts placed the volcanoes and the fault lines where earthquakes occur, and they shaped the continents.

      This new evidence demonstrates that the surface of the Earth has remained relatively unchanged for a long, long time. Where it was thought that most of the formations of Earth were formed slowly over millions of years of time, in fact most of the formations on the Earth came to be by catastrophic impact. These impacts then caused seismic shock waves which expanded across the Earth in the form of concentric circles similar to a stone thrown into a still pond of water. While our atmosphere and time have eroded these forms, the remains of these seismic waves are precise and still clearly visible today. Where it was thought that the mountains were raised by continents colliding, and the rivers formed by erosion, it can be shown now that the mountains were raised and the rivers valleys were formed by these seismic circles.

     While it is certain that the crust of the Earth is shifting in places, which is the cause of earthquakes, this is something quite different than the idea of Pangaea and continental plates floating on the surface of the Earth which collide to form mountains. These geographic circles provide evidence that contradicts those ideas. Many of these seismic circles are hundreds and sometimes thousands of miles in radius. Some of them span continents, a few circle the globe and sometimes the concentric circles from individual impacts are visible on six continents, Antarctica being too ice covered for analysis. Had the continents been drifting, then parts of the circles would be moved. Yet the circles are intact.

     Most of the impacts that are discussed here are huge, but the principles that are shown apply to impacts of all sizes. By understanding them, the reason why the local river flows where it does will become evident. Why towns and cities were built where they were, and where minerals are found will become more clear. The soil sciences, land use planning, geology and Earth Sciences generally will have new insights to advance their knowledge base.

     This treatise is not intended to be all inclusive of all impacts. That would not be possible. It is intended to demonstrate the major impacts of a variety of types and how they formed the Earth. Nor is this intended to be the last say in the formation of the Earth. To the contrary, it is intended to act as a guide to further research, to help us form a new understanding of our home planet, how it came to be, and why it is as it is. What you see here is just a beginning. The more we look, the more we see. With these new tools, a whole new world awaits.


The Beginning

 Tycho Crater on the Moon
The idea of an impact is typically a crater like we see on the Moon. This image of Tycho Crater on the Moon is generally of how we think of them, as a depressed area with a circle of steep walls surrounding it, and a central peak. This is only the case sometimes.
     Whether or not an impact raised a rim when it was formed is dependent on a number of factors, such as the size of the impactor, the difference in density between the earth and the impactor, relative speeds, and the terrain where the impact occurs (mountainous, plains, water). Also the stronger gravity is, the less steep the resulting walls can be, and the less high.
      A peak in the center is also a rarity. As the gravity of the Earth is six times that of the Moon, the impactors come in faster, and hit harder. What is left is usually smashed to bits and scattered in all directions, or buried deeply in the Earth.




Water ripples expanding

     Far more often than forming a crater, an impact will end up looking very similar to the water pictured here. The evidence of impacts lies more in these circular waves that radiate out from the center, than in the central area where the hit actually occurred. The extreme energy of the impact sends out seismic shock waves through the Earth, powerful enough that the ground acts as if it were liquid. The difference between the water and the land, is that the waves in the water will continue until the water is again a still flat surface. But on the land when the energy has been expended, the waves stop where they are and the land retains that form.
     These seismic waves travel out from the center for long distances, rearranging the land as they go into geographical alignments in the form of concentric circle waves. We know these alignments as mountains, hills, valleys, coast lines and other phenomena. Larger impacts will show concentric circles out to great distances, each circle with the same center point.

      As more impacts occur, the land then looks more like the water ripples in the rain, pictured below.
Raindrops in the water.




Tamiahua Meteor Impact Site, Veracruz, Mexico
Tamiahua Impact, Veracruz State, Mexico.
 The Impact site is about 95 miles in diameter.
      The shock waves may form a circular rim of hills, or they form valleys lower than the surrounding areas. Rivers then form there. This is why many of the rivers flow where they do, and why many lakes, mountains and coastlines are where they are, and shaped as they are.
        This is the case for the Tamiahua impact site on the Gulf Coast of Mexico, pictured right, where the Rio Panuco defines the northwest edge, and the Rio Tuxpan defines the southern edge. An examination of the image at right will show other smaller impacts, some of them are marked, most of them are not.
      As each impact is marked, the formation of the land becomes more and more organized, so that the majority of land forms can be ascribed to one or more impacts. By defining the land this way, then the effects of the various other geological forces can be more easily recognized and understood.
     Since most impacts do not leave craters, it is more accurate to call these Impact Sites.






Himalayan Mountains Impact
Himalayan Mountains Impact
It is theorized that these mountains may still be increasing in height due to plate tectonics. If so, the shape of the plate was caused by the shock wave of the impact.
    While the center of the impact may take many forms, the seismic shock wave is always a true circle. However nearly all impacts have one side more pronounced than the other, due to the angle of impact. The impactor nearly always comes in at some angle other than straight down. This means that the shock wave deformations in front of the impact will be more pronounced than those behind it. Roughly then, half of the circle will be easily seen, and the other half will be more faintly marked. This is how the varying directions of impact can be noted.
      In the image left, the Himalayan Mountains form a near perfect circle from the shock wave that formed the mountain chain. The impactor here then came in from the North northeast at a steep angle. This is a very old impact with many impacts after it. These later impacts obliterated part of the earlier impact to make shock wave circles of their own. This is one reason why it is rare that we see a complete circle, particularly on the larger strikes.


     Another reason the concentric circles will not show in their entirety, is that as the shock wave travels through the Earth, some of the surface is more easily moved around by the wave than other parts. In the image below the lower Red River joins the Mississippi River Delta and aligns perfectly with the shock wave from the Adirondack Impact,  at 1315 miles distance(2,110 kilometers). Then at the top left of the image the alignment disappears. This shows the difference between softer soils, and harder packed earth to the north. Thus what we see are bits and pieces of the circle and we must connect the dots.
     Yet another reason is that our ability to decipher fine topographic detail is limited on this scale. A circle of 1,315 miles radius has a circumference of over 8,000 miles. To track the undulations over all types of terrain at this distance is a daunting task, as such only the most obvious can be shown. The image to the right shows about 650 miles of the arc, from an effective altitude of over 750 miles.
     When we look for the evidence of the impact, the seismic wave deformations of the land are definitive. These deformations will be aligned very closely to the circle, and there will be a number of them spaced around the circle to define the circle specifically. The more alignments, the higher the certainty of formation by impact. More alignments allow the circle to be drawn with more accuracy, and the center of impact ascertained more precisely.
    River valleys are the easiest to follow, as the valleys they follow have been produced by the seismic wave, and their flows are easy markers following the ring sometimes for considerable distances. The lines of hills and mountains that are formed are easily followed, but a degree less distinct than following the rivers, as the rivers continually wear down their paths, while the tops of the hills continually erode.
Red River and Mississippi River Delta
The Red River flows to the southeast and joins the Mississippi River Delta, as formed by the Adirondack Impact, in northern New York State at 1,315 (2,110 km) miles distance.

       It is not unusual to see the largest alignments at great distances from the point of impact, with smaller alignments before and after. This may be a clue as to the speed of impact. Often, the alignments seem to reverberate from one side to the other, such that a major alignment will be seen on one side of the impact with one ring, and then on a different side of the impact with the next ring.


     It is generally not sufficient to note a shock wave by only one alignment. As the Earth was impacted many, many times, any one geographical feature could have been formed by any of number of impacts. The proof lies in being able to show sufficient alignments to demonstrate each circle specifically. A larger or smaller circle will not fit, and moving the circle a little to one side or the other doesn't work either. There will be a specific center of impact, which may be far smaller than the impactor. The impactor could have been an asteroid of 50 miles diameter. But the center of impact will still be a point, and all shock waves will radiate from that point, rather than an area 50 miles in diameter. The shock waves from the impact create a pattern of concentric circles, all emanating from one specific point, the center of impact.
     While the shock wave circles will be near perfect, the alignments to it may show some variation. The variations are primarily because rocks rarely break on the smooth line where you would like them to break. Instead it breaks along the natural structure lines of the rock. These variations are rarely more than 1% of the radius.
      The more alignments that follow the circle, and the more concentric circles found, the more evidence of the impact. It may be possible to find one or two circular alignments from any point you want due to chance. However to find specific circles, and then again to find concentric circles, brings the probability of chance closer to zero with each alignment found. Finding the alignments that follow these guide lines demonstrates the proof of impact with increasing certainty.

If the impact was in the ocean the impact may create a huge tidal wave. In the image to the right, the limit of the tidal wave created by the Cape Verde Islands Impact is still visible 771 miles to the east of the impact. The line closely resembles the high tide line seen on beaches after the tide recedes. This impact is the probable cause of the Mid Atlantic Ridge.
The jog in Kinbasket Lake, British Columbia, Canada. The jog in Kinbasket Lake, British Columbia, Canada and the alignment of the adjacent mountains were the result of an impact 95 miles (155 km) to the northwest.
Evidence of the tsunami from the Cape Verde Impact.

    Hill and mountain chains too big for the shock wave to re-align, break in line with the wave, providing valleys where the rivers and streams flow. Where it seems that the cracks, or valleys in the mountains have little order other than that of erosion, the vast majority can be ascribed to one or more impacts, where the seismic wave broke the mountains and left the valleys where the rivers flow.
Formation of the Columbia River George by the Mt. Baker Impact.
The Columbia River George is a break in the Cascade Mountain Range.
It was caused by the shock wave from an impact 220 miles North.  That impact caused Mt Baker,  a volcano in northern Washington State, to form.

     Above is the Columbia River George as it passes through the Cascade Mountain Range forming the boundary between Washington and Oregon states. Before this break, the area to the East of the mountains and primarily in Washington State was a large inland lake, fed by the Columbia River as it drained a large part of the Pacific Northwest and British Columbia. When this impact occurred, the shock wave caused this break in the mountain chain, and the lake drained through here forming the Columbia River George and many of the geographical features of eastern Washington state as the water drained away.

    The larger hits have the potential to crack the outer shell of the Earth. Some had the power to shape the continental plates. A knowledge of where these hits were, can help us define the cracks in the Earth's surface and the various shifting land masses we have. This would be a basic area of study for people involved in the science of earthquakes and plate tectonics.
      As some of these circular alignments are large enough to fall on more than one continent, they can be used as a form of measurement for the movement of continents. If the age of the impact can be determined, then the amount of continental drift can be established over that time period. Or that idea can be dis-proven.

    With the right tools, these alignments become easily visible and the formation of our Earth then begins to take shape and make sense.
The San Andreas Fault
The impact at Yellowstone National Park produced a shock wave that aligns
the San Andres Fault line in California, 760 miles (1,245 km) distance from the center of impact.


    The actual impact site, the center, may be round or deformed depending on many variables. What was the shape of the object? Was it round, or perhaps some other shape. How did it hit? Straight down or at an angle? Was it a hard rock asteroid, or a dust ball comet? There are many variables, but more often than not, the center is flat, perhaps a little higher or lower than the surrounding area, but generally flat. On some occasions the impact may raise a center peak, or make a deep impression, but most often the center is not much different than the surrounding area, as the impact blasts everything flat.
     It is common to see a lake in the center, as the center is sometimes depressed. On smaller impacts, the farm house and other buildings may be in the center, probably because the ground there is somewhat higher, so that is where they built the buildings. On larger sites, the center area may have been blasted nearly level by the impact. These level areas are then excellent areas for towns and cities to be built, such as Mexico City, Tokyo or Moscow.
Ébano Impact, Veracruz, Mexico      In the image at right, the  Ébano Impact, is on the northwestern border of the State of Veracruz with San Luis Potosi State, Mexico. This impact is on the eastern coastal plane of Mexico. The soil there being relatively soft and wet was easy to penetrate deeply with a high speed, hard asteroid.
     The asteroid itself ended up deep underground, leaving the surface as a depression where the lake formed, with a raised center area, and low hills surrounding it.



 Norfolk Nebraska meteor field     Often times the object may simply go splat, blowing the material of its making out across the Earth in all directions, and leaving little evidence of its existence other than a few inches of soil.
     The image at left is of an area south of Norfolk, Nebraska. A first look seems to show nothing but almost flat farm lands. However if you study the image, the shapes of numerous impacts will start to form.  Click on the image for more on this.
       Often the impact site is best described by a change in vegetation patterns, this due to different soil types from one impact to the next. These patterns can often be seen only from high above. Those that study the various soil types could benefit from a knowledge of  the limits of each type, as an aid to agriculture, land use planning and other sciences that base decisions on soil types and their properties.
 
       There are many kinds of impacts. When we look at them we must consider what the object must have been. On one extreme, it may have been formed from a solar flare that blew heavy metals out into space at tremendous speeds. These metals fused together by solar heat, and then tempered by the near zero degrees Kelvin of the deepest expanses of space, could be the hardest material imaginable. This type of object at incredible velocities would be like a bullet into the Earth, penetrating deeply leaving only a minimum crater, but perhaps sending out a shock wave that circles the impact site at hundreds of miles distance.
 

Craters of the Moon, Idaho, USA

Craters of the Moon National Monument.
     This impact was one of the hard, high velocity impacts that punched a hole in the Earth, from which the lava flowed on a number of occasions.





Major landmarks on the Moon      They could come from a planetary sized object that was somehow torn apart to form asteroids such as in the asteroid belt between Mars and Jupiter. In this case they could have densities similar to that of the Earth.
     Sometimes they may explode when they hit, where pieces fly off in all directions, like throwing a piece of dried dirt against a concrete wall. This is the case of the Tycho Crater on the Moon, shown in the image at left, bottom center of the Moon.
 


 



It is also the form of the impact at El Perdido, Mexico that blasted rays over half the country.














     The image above is an impact site in Northeastern Quebec, Canada. This asteroid came at a low angle from the SE, and plowed a deep 'V' while cracking the surface enough to let the lava flow. The lava flowed both north and south. As it came up from the center of impact, the lava cooled to form a cap, which then split in two as more lava surfaced.
      Asteroids coming in at various, and sometimes very low angles, could leave scars and skid marks on the surface of the Earth. They could plow a deep long 'V' in the Earth, sometimes plowing deep enough that the lava would flow. 

     On the other extreme a comet could have been roaming the galaxy for billions of years collecting particles bit by bit and slowly growing to something perhaps a hundred miles across or more. However, if gravity is proportional to mass, then even if the comet was 100 miles in diameter, the gravity of it would be infinitesimal compared to the gravity of Earth. Considering this, the comet would then be so loosely packed that only the light of the sun would be enough to blow material from the surface, and that would form the tail of the comets we see in the sky.
    Many of the impactors that hit the Earth were these giant dust balls. This is not to discount their significance because some of them still contained enough material to shape the continents and form the mountains. When they hit a large percentage of the material of their making is blasted out in all directions to form a new layer on the Earth. The hit still produces the circular shock waves which reform our Earth. In the center, the comet collapses and depending on several variables, the center may end up higher or lower than the surrounding terrain.

    Oddly enough, when these impact sites are seen from above, they may look like the classic idea of a crater with the center looking like a raised area, a hill or mountain. But on examination, by moving closer and tilting the view, the areas generally look nearly flat. This illusion is caused by the differences in the soil types from one area to another within the impact site.
     The Navajo Impact site is one of these. While the center is raised, the amount of rise, compared to the length and width shows how loosely packed is was.


Mt Kilimanjaro

Then there are other impacts, big ones that punched a big hole in the crust of the Earth. They let the lava flow making large volcanoes, and the seismic waves from them formed great valleys where large lakes formed, and the largest of rivers flow. Often these seismic lines are then used as political boundaries. This is the case of Mt. Kilimanjaro in eastern Africa. This impact was one of a number of impacts that formed the Great Rift Valley of eastern Africa, and shaped a large part of the continent.



Then comes the problem of size.

How big are these things?

Considering the Earth to be 8,000 miles in diameter, and that the formula for the volume of a sphere is:

Description: Description: V = 4/3 pi r^3

 Then 4 /3 x 3.14159 x 4000 x 4000 x 4000 = the volume of the Earth = 268,082,346,667 cubic miles.
That means that if the average size of an object that hit the Earth was one cubic mile,
then the Earth must have been hit more than 268 Billion times.

Or from another angle, if the earth received 1,000,000 hits,
 the average size of the object must have been 268,082 cubic miles in volume,
 or 80 miles in diameter.

While that may seem like a lot, if the Earth's diameter is 8,000 miles,
 it would take 100 of those side by side, just to make one diameter!

   An object depositing 268,000 cubic miles of material on the Earth would act significantly to define the continents. That would add one mile of thickness to an area more than 580 miles in diameter. An impact that big would leave some pretty serious marks. Many of these objects then would have been many times that in diameter, and by impacting such volumes of material on the Earth, we can start to understand how the shape of the Earth was determined.  

But now...

     The probability is that the largest impacts came first, as larger objects have more gravitational attraction, and that was a very long time ago. What is left for us to see on the surface are with a few exceptions, the remains of much smaller impacts. These impacts generally smash themselves to bits as they hit, throwing the material of their making out over the surface in every direction and adding a new layer to the Earth. Or they bury themselves in the Earth.

However the shock waves they produce, in those expanding circles, deformed the land to make the mountains, hills, river valleys, coastlines and more for hundreds, and sometimes thousands of miles in radius.

   When we look at the Earth for evidence of impacts, we need to be thinking on this large scale.

We should not be aghast should someone suggest an impact site of 1,000 or 2,000 miles diameter. In fact, we should expect them.






                  Dinamita Impact Crater, Gomez Palacio, Mexico

Dinamita Impact Site, Durango, Mexico

Should we be worried about large impacts today?

     Our Earth came together violently. Considering that these impacts create shock waves that form mountains and river valleys as they expand, and that the difference in elevations between them is often hundreds, if not thousands of feet, a hit by one of these would be like a circular tidal wave of solid earth, hundreds or thousands of feet high, expanding and reverberating at tremendous speeds. The shock waves may expand for thousands of miles. Entire cities would be reduced to unrecognizable rubble. Plant life could re-root, but anything else that walks, crawls or swims would be devastated.

      As far as mass extinctions are concerned, noxious gas plumes or dust clouds that blocked out the sun may have happened, but after a land wave 500 feet high passed over the continent,  gas and dust clouds would not have much significance.  And it looks like there were many, many of these impacts.

     It must be understood that our Earth, as big as it is to us, is no more than a tiny speck in the universe, and there are many things out there far bigger than us. Just to orbit the Earth requires a velocity of about 15,000 miles per hour. These space rocks may be traveling at 25,000 to 50,000 miles per hour and more. The energy of a medium sized asteroid hitting the Earth would be far greater than anything man has seen before. The impact pictured above of the Dinamita Crater near Durango, Mexico shows circular seismic wave alignments that deformed the ground at 950 miles (1,525 km) distance and beyond.  It is likely that if this asteroid hit today, every building within 950 miles of it and possibly farther would fall. These things make earthquakes at 9 and above on the Richter scale look like kindergarten play time.

     Such was the formation of our Earth!

Rock formation showing the layer build up.
      As the Earth was formed by a bombardment of various objects, when they hit, often times they blew the material that made them in all directions to form sedimentary layers, one after another which built up the planet. Every impactor was as different as the universe that it passed through, and so each layer is as different as that which formed it.

      Interesting studies could be made using the logs of well drillers to map out the 3 dimensional underground extents of the various soil types encountered down into the earth. According to this theory, the extents of the impact circles could be determined by the extents of the various soil types described on the well drillers logs. Maps could be made to demonstrate the various accumulations at their depths.  And perhaps, if there was an asteroid made of gold that impacted the earth,  the extents of that impact could be mapped.

    Knowledgeable well drillers of all types should keep samples of the layers they drill through for a chemical analysis. At some point they will drill through a valuable layer. Once they find a valuable layer, the rest of the impact can be mapped, and the concentrated deposits then found.

     We see in many places here on the Earth, how minerals have come together so that we can mine them in great quantities. Gold, for instance, will erode down from the mountains and collect in the sand bars of the rivers and streams to form placer deposits where miners pan for gold. This happens because of the specific characteristics of gold. Other minerals accumulate in different ways because of their specific characteristics and circumstances. If this happens here on Earth, is logical that it happens also out in the vast reaches of space, so that over billions of years like elements come together.

     Thus, while most of the impactors would be composed of plain old dirt like you walk over every day, some of them could be highly concentrated with specific minerals. Is it possible then, that some of them are made up of gold, copper, aluminum or titanium? Could this be one reason why minerals here on Earth are concentrated as they are? Is this why in some places we have mines that are miles across and go deep into the Earth? Is there a connection between the mines we have found and impacts? If so, then where do the minerals end up after impact?




    One last thing. While these impacts will show the basis for the formation of the Earth, this is not to discount the actions of volcanoes, earthquakes, erosion, glaciation or plate tectonics. Those forces are still there and still hard at work. By studying the impacts that formed our world, we can separate the effects of the various forces better than we could before, and this leads us to a better understanding of our world.




Notice About the Images


     In the following pages, what we are looking for are geographic phenomena that closely follow the circles. These can be in many forms such as rivers, mountains, a line of lakes, a coast line,  or a break in a mountain chain, all with the primary feature that they all follow the circles closely.
     The images of the impacts are formatted in the browser window at 800 pixels wide. This is to accommodate a smaller sized viewing screen. While many of the geographical features shown can be seen in this small format, many of the seismic waves represented cover a circle hundreds or thousands of miles in diameter. To show the details necessary to describe these circles is difficult. Generally, only the largest and most easily seen features are shown here. A more detailed analysis will bring out numerous other geographic features that were caused by the seismic waves.
     Two methods are used to demonstrate the shock wave phenomena. The first is the images may be expanded for increased clarity.  This is done on most computers by the (ctrl + +) function. The various browsers also may have zoom add-ons that are useful. The majority of the images are 1368 pixels wide and occasionally as large as 4800 pixels wide. The larger images are often shown in the smaller size and linked to the full size images. These links are noted where appropriate.
     The other method of demonstrating the details is to show only that part of the circle where the details are. As there are usually several images shown around the circumference of the circle, the proof that these images are parts of the same circle is in the white box, in the lower right of the images, which shows radius, circumference, and area. That these numbers are the same denotes the same circle.
     The lower right of the images shows the coordinates of the pointer where the screen shot was taken. Generally I tried to use the center of the image for these coordinates, or in other cases the center of impact if possible. The naming of the images also shows their location, for example the image Eurasia1075ESE.jpg in an image of the Eurasia Impact showing that part of the circle that is 1075 kilometers in radius, to the East South East of the center of impact. Most of the images are shown in miles, others in kilometers. The white box, lower right, should be consulted when in question.


We start in Arizona
with

Barringer Crater
as this crater is well documented and studied.
Barringer is a small impact, but the effects of it can be seen for many miles around.
Studying the effects of this impact on the surrounding land provides a basis of understanding for the larger impacts.



Index of Impact Sites
North America Asia
Europe Africa
United States Canada Mexico


Adirondack
Mountains

Cover Image, Formed Half the US
Baffin Island
Formed the Hawiaan Islands
Heard around the world

Chicxulub
puts North America and
South America firmly in place
for 65 Million years

Aral Sea
Formed the Coast of
Iran and Pakistan

Eurasia
Caused Volcanoes Across
Southern
Europe and Asia
The Eye
 of the Sahara

A Double Hit
Barringer Crater
Meteor Crater, a Fine Example

Dinamita
Fresh and Obvious
Burma
Describes India's West Coast

Cape Verde Islands
Formed the Mid Atlantic Ridge
Craters of the Moon
A High Speed Bullet
British Columbia
The Coastal Range Formation
Ébano
With Lab Video Demonstrating its' Formation
Putorana Plateau
The Siberian Traps

The Formation of Russia

The Great
Rift Valley
Ain't Rifting Anywhere
East Coast
and the Caribbean

The Burmuda Impact
Mt Burdett
Helped Form 2/3 of North America
Tamiahua
90 Miles Diameter
The Tunguska Event
June 30,1908 in Russia
as bright as the Sun

Greece
Coming Soon
Kilimanjaro
Caused by a Meteor
Felt Across Africa

The Great
Salt Lake Impact

A Six Continent Impact
Hudson Bay Cabo Rojo The Bosporus Straits
Broken by a Small Impact
Gibraltar
Coming Soon
Lake Victoria
How it Was Formed
Indiana
A Really Really Big One
Hudson Bay I
Himalayas
Shaped by a Meteor Impact

Mambi
A large Bullet Causing
Numerous Volcanoes

Mt. Baker
The Columbia River George



Spain
Coming Soon
Mayka
Seen to 9600 Miles Diameter
Navajo
A Huge Dust Ball
NE Quebec
A Low Ball With Lots of Lava
El Perdido
A Starred Impact
India
Madhya Predesh
Disproves India's
Continental Drift


Mogadishu
The Great Rift Valley
to the Maldives

Norfolk, Nebraska
An Impact Field

Isla Clarion

Indonesia
The Great Circle of SE Asia

*Mueda*
Seen on 6 Continents
Omaha
An Engineers Delight

Isla Guadalupe Japan
Tana Lake
North Africa's Reason for the Rift
Oregon
A Crater Field
The Columbia River Bend
The Impact that Bent the River

Isla Socorro

Sirte
Coming Soon
Sierra Nevada
The Making of the Mountains

Mexico City


Wyoming
The Coast Range
Western U.S.



Syria


Yellowstone
Formed the San Andreas Fault

Tampico


Yosemite
Describes the Outer Rim
of the Rocky Mountains

























Google Earth is leading the way on this. With their work, they have opened new doors for a number of sciences. This is a new tool to help us describe how our Earth was formed and why the mountains and plains, lakes and rivers are where they are. This new tool will prove instrumental when it comes to finding minerals, analyzing agriculture, land use planning, water resource development, environmental protection, and many other areas that depend on knowing more about where we live. With this new tool, we can see our world in a way that we have never been able to see it before.  And it's free!

twest@tampicoventures.com

©Terry Westerman 2012