Whose Fault?

  

     When it comes to situations that create the possibility of precious metal ore to be present in our predominately sedimentary rocks of Kentucky, they are rare, for sure.  Geologist consider the far reaching coal beds and limestone sediments formed from decaying swamp forests and marine bottom deposits respectively to offer little room for the right type of activity that would allow the presence of silver or other precious minerals.  There are exceptions, as I've pointed out in the past.  Take for example the curious peridotite deposits in Elliot County, Kentucky or the channel fill as describe of Bell Falls in the Red River Gorge.

The Glencarien fault 

     In our discussions, we must not forget the many fault systems in our state.  A fault is simply a place where the earth breaks and the land is moving apart in two different direction.  There are different kinds of faults but basically, on one side of the fault the land is moving up or down relative to the rock and ground on the  opposite side.  Imagine breaking an arm bone and it becomes separated, moving apart. The obvious pain not withstanding, the bone is broken and moves apart in different directions.  The doctor "sets" the bone by moving (painfully) back together.  A fault is just like that, though it will never likely move back together.

The rock beds are tilted causing a shallow water fall

     Now a fault is ultra slow moving, taking centuries to move only a few inches.  However, sometimes they move with extreme speed and large distances.  We saw this in the Japanese earthquake earlier this year.

The very contact point of two opposite moving masses of stone

If the fault reaches deep enough into the earth sometime in its life and gets close enough to the hot gases, and molten materials deep within our crust, some of these gases can carrying minerals to the surface.  Over eons of time the cooling uprising of the gases through the fault cracks can produce deposits of minerals.  And yes, silver ore can be one of these deposits. There could be and likely are many faults that are not even exposed at the surface of the earth today, they existed millions of years ago and have long since been covered by other rock deposits in the earths never, ever ending changing events.

Striation marks or scratches are called slicken sides

     The faults we see in Kentucky today on the surface at this point have not been known to produce anything other than the rock that is present on the fault.  One such fault I really like is  the Glencarien fault.  It is located just southeast of Natural Bridge State Park which is part of the Red River Gorge area.  Here the limestones and shales have broken apart, tilting slightly dropping one side down dramatically below the other.  The fault like continues for miles but  can only be observed here.

How the Project Evolved-Part Two

Landmarks and clues are abundant all over the  state

     After retiring from the State Parks in 2003, in November the following year, I was interviewed by Byron Crawford, a Courier Journal writer.  Mr. Crawford came to me as if I were "the" expert on the Legend of John Swift. There are many more around the country that are far more expert on the Swift legend than me, for sure.  Anyway,  I remember we had a very enjoyable visit and before he left, he made the comment, "you should write a book."  His was referring, of course, writing about the John Swift Legend.  After his article appeared in the Courier Journal, I had numerous phone calls, crank letters and renewed interest in the story.  So I decided to write a book.  I determined early that I wanted to write a novel since the story had been factually about written to death.  After my experience with the multi-media program I  just thought a good story with good characters, playing on some known historical facts would be just the ticket.  Now, my first concern dealt with the issue I could make both historians and treasure hunters mad.  Tinkering with historical characters is no easy task and is something not to be messed with unless, it is made very clear the story is fictional.  On the other hand, the treasure hunters might not agree with the truly fictional characters and clues.  I struggled with that a bit but soon got over it with the realization of two important facts. It was my story and there's nothing like a disclaimer.  I was healed and work could begin.

Indian stair steps carved into face of cliff in Red River Gorge.  Most Swift Journals mentioned  Indian stair  steps

     Besides my personal knowledge, I already had a pretty extensive collection of materials and information.  Knowing  the Red River Gorge area,  being familiar with the legend and some of key people involved made the task of writing a novel a little easier.

The :Blue Hole at McConnell Springs

    So the following year I began writing my first draft.  This historical novel is set in Kentucky but it is two time periods running together.  One could say flashbacks, but really I set out to write two distinct stories, one set in the late eighteenth century and the other in recent times.  I spent two years getting the first draft completed and I discovered that in my writing style, though the characters might be imagined, my place locations are not and could not be for me.  I actually, had to visit places such as Pilot Knob, Rock Bridge, Indian Stairway and McConnell Springs and on to get the feel and detail of the place.  Keep in mind, I never actually visited the silver mine!  These places are central to the story and without them, the story would not be believable.  For example, there is a rock shelter at Pilot knob and while there are many very old carvings, there is not a rock wall map.  There is a turkey track on Rock Bridge, an Indian Stairway,  the Warriors Path and caves at McConnell Springs. Then there are some places I can't tell you about, you'll need to read it for yourself.