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The new data fits perfectly with a first century dating of the Shroud.
Namely, the geological makeup of the hills is weak.“That hillside that failed is basically a stack of clay on the bottom, then sand, then glacial till — which is compressed clay, sand, and boulders — and then more sand and gravel on top,” Montgomery said.
More research into the older landslides is needed to find out how many were triggered by earthquakes and how many by rain.“That’s a question that disaster planners and emergency people should want to know the answer to,” Montgomery said.
If landslides happen after rainfall, they’re more likely to be a one-off event, while an earthquake might trigger many at once. According to La Husen and Montgomery, the study’s methods might vary from place to place (the exact curve only works for the Oso area).
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