Mystery in the Rocks
 A physicist's discovery begins an extraordinary odyssey 
through pride and prejudice in the scientific world.
By Dennis Crews
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Independent research is costly and difficult apart from the 
sophisticated laboratory facilities of a modern university, but 
Gentry was persevering. In a makeshift laboratory at home he 
began to study all the radiohalo specimens he could find, funding 
his research by working as a substitute high school math teacher. 
Patiently and meticulously he gathered data and catalogued the 
specimens according to type and quality.   
Henderson had named the anomalous halo types he had observed 
A, B, C and D halos. Of all the halo types that had been documented, 
the ones that commanded Gentry's attention first were the ones 
most different from the others. The D halos were smaller than 
the others, with only a single fuzzy disc instead of a series 
of rings. Gentry split D specimens so that the halo centers were 
on the surface, then poured a special liquid photographic emulsion 
over the surface. When the emulsions were developed after a time 
and inspected microscopically, tiny alpha-emission trails were 
found radiating from the centers. This demonstrated that the 
centers were not extinct at all, but still radioactive.  
Further research indicated that the D halos were simply uranium 
halos in early stages of development. It was a previously unknown 
but rather unsurprising bit of information, since the half-life 
of uranium-238 is calculated to be 4.5 billion years. Next Gentry 
turned his attention to the A, B and C halos.  Henderson had 
believed these halos to be caused by alpha radioactivity from 
three isotopes of the element polonium, all members of the uranium 
decay chain. He theorized that some time in the past, water or 
some other solution containing uranium and its daughter elements 
must have flowed through tiny cracks in the rock and enough polonium 
had accumulated at certain points along the way to form halos. 
He had suggested that his hypothesis for this secondary mode 
of halo origins be tested, but World War II had intervened and 
the research was dropped. 
Gentry's measurements confirmed that the rings were indeed 
produced by radioactivity from polonium isotopes. But the more 
he studied the specimens, the greater problems there seemed to 
be with Henderson's hypothesis for their origin. Close examination 
revealed many halos in solid areas that were free of any fissures 
or pathways by which radioactive atoms could have penetrated 
the rock. Further, there was no discoloration or any other typical 
evidence of uranium having flowed through the rock previously. 
Ultra-sensitive testing detected only minute traces of uranium 
in the surrounding rock—the same amount that existed throughout 
all mica specimens.  
At last, all attempts to confirm Henderson's theory of a secondary 
origin for the polonium halos failed. Emulsion tests had shown 
the radioactivity of polonium halo centers to be extinct, which 
was expected from isotopes with such brief half-lives as polonium. 
For Henderson this had posed no great problem—but now that he 
had disproven Henderson's hypothesis, a profound new dilemma 
appeared. Polonium atoms decayed so rapidly there was no conventional 
way to account for their having existed in the rock at all.  
 
The longest-lived polonium isotope, polonium-210, has a half-life 
of 138.4 days. Two beta-emitting elements precede polonium-210 
in the decay chain, the longest lasting of which has a half-life 
of 22 years. If either of these parent elements were deposited 
in rock, the halo would begin to form as soon as the beta-emitting 
parents had decayed into polonium, an alpha-emitter. Polonium-214, 
which has a half-life of 164 microseconds, is preceded by two 
beta-emitters with respective half-lives of only 27 and 20 minutes. 
And polonium-218 has a half-life of just three minutes—with no 
beta progenitor at all.  Thus polonium-218 would have to be deposited 
inside solid rock the same moment it came into existence, in 
order to form a halo. Now he clearly saw why Henderson had suggested 
a secondary mode of origin for polonium halos.  
To find radiohalos in granite caused by such short-lived isotopes 
as polonium was an utter scientific paradox, he realized. Why? 
Radiohalos can form only in solid rock. Much of the granite encasing 
the polonium halos was Precambrian, which is believed by most 
scientists to have taken millions of years to cool from its molten 
state. Since so few of the rocks which encased the halos had 
clefts or passages by which polonium atoms could have entered, 
the polonium had to have existed from the very formation of the 
rock itself. Yet polonium isotopes have an extremely fleeting 
existence, and would decay away long before even a small chunk 
of molten granite could cool and solidify. Was this the kind 
of discovery the head of the physics department had feared he 
would make? 
All the evidence indicated that the polonium had originated 
concurrently with the formation of the granite itself.  Yet if 
it had, according to conventional science it quickly would have 
decayed away, and in the molten primordial mass its telltale 
halos never would have formed.  Was it irresponsible to consider 
that the tiny radiohalos—a minor, overlooked mystery for so many 
decades—might be evidence of instantaneous creation locked into 
the earth's crust?  And of crucial importance—was it possible 
that he had overlooked something that could provide a more conventional 
explanation for the halos? 
 
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	For readers interested in a more comprehensive treatment of this story, Robert Gentry's book, Creation's Tiny Mystery, is available for $18 (U.S.) + S/H.
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			The above page was found at https://www.halos.com/book/mystery-in-the-rocks-03.htm on November 3, 2025.
  
			© 2009 
			Earth Science Associates
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