Erosion in fine-grained limestones at the Western Wall is up to 100 times faster than other stones that have almost not eroded at all in 2,000 years ago stones, according to Hebrew University researchers.
The Kotel is not in danger of collapsing, but some of the stones have receded by several inches.
The erosion of some stones is good news for people placing prayer notes in the wall’s cracks and crevices, but presents a problem for engineers concerned about the structure’s stability.
To calculate the erosion in the different kinds of limestone that make up the Western Wall, a remnant of the ancient wall that surrounded the courtyard of the Holy Temple, researchers from the Hebrew University of Jerusalem used a laser scan to create an accurate three-dimensional computer model.
As reported in an article accepted for publication in the journal Geology, researchers Dr. Simon Emmanuel and PhD student Mrs. Yael Levenson found that stones made up of relatively large crystals were resistant to wear, so that they were almost unchanged in the 2000 years since they were originally put in place. By contrast, limestone with very small crystals (about one thousandth of a millimeter in size) eroded far more quickly.
In some cases, extreme erosion rates in fine-grained micritic limestone blocks were up to 100 times faster than the average rates estimated for the coarse-grained limestone blocks. In some places, these stones had receded by at least a foot, potentially weakening the overall structure.
To understand what causes the two types of rock to behave differently, the researchers collected samples from ancient quarries thought to have supplied the stones for the Second Temple. Using a powerful atomic force microscope, they were able to see how the rocks disintegrated when they came into contact with water. During the experiments on rocks made up of small crystals, tiny particles rapidly detached from the surface of the rock. These experiments simulated the way in which rain water interacts with limestone in nature.
Observed for the first time in Dr. Emmanuel’s lab, this process of accelerated erosion can explain why some rocks are more weathered than others. While mechanical weathering is thought to act on blocks and chips of rock at the visible outcrop scale, the researchers showed for the first time that chemo-mechanical erosion extends down to the tiny micron scale. The findings could have important implications for regional and global carbonate weathering.
“Understanding such weathering processes could help guide the development of effective preservation techniques,” according to Dr. Emmanuel.“ For example, it may be possible to develop materials that slow the rate of erosion by binding the tiny crystals in the rock together. Advanced engineering techniques like this should assist efforts to protect not only the Western Wall, but other cultural heritage sites in Israel and around the world.”
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