He finished his thesis while settling into his new job at the Bureau of Mines.
But even before it was finished, coal mine engineers embraced his stability factor.
At conferences, they’d come up to him after he’d explained his work and say,
what you are doing is the future.
They hadn’t felt compelled to do the work themselves, but they were delighted that he spared them these roof falls that cost them $200 a minute to clean up.
There was a limit to its practical usefulness, though, as the stability of a coal mine roof depended on its specific geology.
And the geology varied from coal field to coal field.
“In some places, like Pittsburgh, you needed a higher stability factor,
and in other places, like Alabama, you could use a smaller one,” said Chris.
The same stress that caused a mine roof outside Pittsburgh to crumble and collapse would have no effect on a mine roof in Alabama.
It wasn’t enough to know the load on the pillars.
You needed also to know more about the rock mass over them.
In some coal fields, the sedimentary layers were as thick and cohesive as a chocolate fudge cake,
in others as thin and flaky as a mille-feuille.
Some mines had more moisture in them than others,
and some rocks, in the presence of moisture, would return to mud.
Layers of laminated shale tended to be weakly bonded and vulnerable to horizontal stress.
All else equal, a layer of sandstone was a good sign.
Yes, it had once been a beach, but grains of sand tended to bond more strongly than other particles.
Between a rock and a rock mass was the difference between a person and a society.
Hard as it was to understand a rock,
it was far harder to understand masses made of lots of different rocks.
And so Chris spent much of the late 1980s and early 1990s figuring out which qualities in rock masses caused their strength to vary.
“What I realized very quickly was that none of the existing classification systems for rocks were going to work for coal mine roofs.
You are evaluating not a rock but a structure.
There’s enormous variety.
That’s the key, to look past that variety and come up with a measure.”
Again, he found work done by others and repurposed it for his uses.
Back in the 1940s, geologists working for the Agriculture Department in national forests created a crude method for work crews to determine if some rock would work as a road:
whacking it with a ball-peen hammer.
Oddly, it didn’t matter how hard you whacked it.
There were just a handful of ways the rock might react,
and its specific reaction revealed its strength.
Chris started whacking mine roofs with ball-peen hammers.
“It’s not precise,” he said, “but it does get you in the ballpark.”
The why of it all often remained out of view.
He couldn’t explain why certain traits in a rock mass made it less prone to collapse.
He could just show that they did.
But as Chris set out to classify rock masses, he noticed an odd force that was often observed inside underground coal mines:
the massive horizontal stress on the rock.
“There’s a textbook explanation for stress in the ground,” he said.
“You have the vertical stress of the rock above.
And any time you apply stress from above, the rock below tries to expand laterally.
But at depth it can’t expand laterally in either direction because it is confined by other rock.
So you get horizontal stress.”
In the textbooks, the rule of thumb was that the horizontal stress was about one-third of the vertical stress.
In fact, as mine engineers had known from the stress gauges they drilled into rock,
the forces on the rock running parallel to the Earth’s surface were often two to three times greater than the vertical pressure from the rock pressing down directly from above.
Often miners could even see this horizontal stress
— say, in a buckled mine floor.
But its source was a mystery.
“No one could explain it,” said Chris.
“Nobody had any theory of it.”
It finally occurred to him that what coal miners were seeing near the surface of the Earth
was simply an expression of forces deeper in the Earth’s crust:
plate tectonics.
He made a study and sure enough, the direction of the horizontal stress in coal mines lined up exactly with the definitive plate tectonics stress map that had been created in the 1970s.
The plates pushing against each other directly below West Virginia create a stress running from east to west.
West Virginia mines that ran north to south had always experienced more roof collapses than those that ran east to west,
but no one knew why.
Now they did:
It was as if they were trying to saw against a wood’s grain instead of with it.
“Once you figured that out, it was like magic,” said Chris.
“You would see people’s eyes light up.”