Drilling in the Holy Land
About 50
miles from Bethlehem, a drilling project is
determining the climate and earthquake activity of the Holy
Land. Scientists from eight nations are examining the ground below
the Dead Sea, by placing a borehole in this
deepest basin in the world. The International Continental Scientific Drilling
Program (ICDP) brings together research teams from Israel,
Japan, Norway, Switzerland,
the United States and Germany. Researchers
from Jordan and Palestine also are involved.
Scientists and technicians of the GFZ German Research Centre for Geosciences now have completed a geophysical measurement procedure in the hole, and helped with the initial examination of the cores in a field laboratory. "We have drilled through about half a million years of sedimentary deposits," estimates Dr. Ulrich Harms from the ICDP's operational support group at the GFZ. "From this, we can deduce not only the climate history, but also the earthquake activity in this seismically very active region." The direction and inclination of the well were determined with precision below this lake, which is around 984 feet deep here, and the physical properties of the rocks were measured down to the bottom of the more than 1,500-foot-deep borehole.
These unique measurements are used to record a continuous survey of the deposits in the Dead Sea and to compare it with the recovered cores. Although scientific drilling attempts to recover cores over the entire length of a hole, it is not always possible. These special borehole measurements are conducted to cover the gaps. In addition, a second series of cores is obtained from a second well in order to verify and secure the data.
"If everything goes perfectly, we may soon be able to provide information about past climate and environmental changes in the Bethlehem area," says Ulrich Harms. His colleague Professor Achim Brauer, a paleo-climatologist at the GFZ, is one of the initiators of the ICDP project. He and his team will analyze the drill cores. They are not interested just in the climate at the time of Jesus' birth, but in the climate of the whole of human history. The region of the Holy Land is considered a land bridge across which early man migrated in several waves from Africa to the north, and the climate history of the area therefore is considered closely connected with the history of mankind.
Scientists and technicians of the GFZ German Research Centre for Geosciences now have completed a geophysical measurement procedure in the hole, and helped with the initial examination of the cores in a field laboratory. "We have drilled through about half a million years of sedimentary deposits," estimates Dr. Ulrich Harms from the ICDP's operational support group at the GFZ. "From this, we can deduce not only the climate history, but also the earthquake activity in this seismically very active region." The direction and inclination of the well were determined with precision below this lake, which is around 984 feet deep here, and the physical properties of the rocks were measured down to the bottom of the more than 1,500-foot-deep borehole.
These unique measurements are used to record a continuous survey of the deposits in the Dead Sea and to compare it with the recovered cores. Although scientific drilling attempts to recover cores over the entire length of a hole, it is not always possible. These special borehole measurements are conducted to cover the gaps. In addition, a second series of cores is obtained from a second well in order to verify and secure the data.
"If everything goes perfectly, we may soon be able to provide information about past climate and environmental changes in the Bethlehem area," says Ulrich Harms. His colleague Professor Achim Brauer, a paleo-climatologist at the GFZ, is one of the initiators of the ICDP project. He and his team will analyze the drill cores. They are not interested just in the climate at the time of Jesus' birth, but in the climate of the whole of human history. The region of the Holy Land is considered a land bridge across which early man migrated in several waves from Africa to the north, and the climate history of the area therefore is considered closely connected with the history of mankind.
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