Hagai Ron
Hagai Ron was a professor at the Institute of Earth Sciences at the Hebrew University of Jerusalem and is considered as the founding father of paleomagnetic research in Israel and a pioneer in the field of the relationship between paleomagnetism and block rotation.
Biography
Ron was born in Kibbutz Beit Ha'Arava in the north of the Dead Sea. In May 1948, when he was three and a half years old, and due to the pressure of the Jordanian army, all the members of the kibbutz and their children were evacuated to Kibbutz Shfayim. After a short time, few of the evacuees, including his parents, founded Kibbutz Kabri in the Western Gallilee. Ron grew up and studied in the kibbutz that was his home throughout his life.He enlisted in the paratrooper brigade in 1962. After his military service, in 1965 he went for a year of national service in Haifa, in the Machanot Ha'Olim Youth movement, where he met Hadva, his wife. During the Six Day War, he participated with his reserve unit in the battle of Umm-Katef in Sinai Peninsula. During the Yom Kippur War he fought with his unit in the Suez Canal Sector.
Ron studied for all his degrees at the Hebrew University in Jerusalem. He studied for a bachelor's degree between 1969 and 1972, and for his Ms.c degree between 1976 and 1978. His studies for the Ph.D degree between 1979 and 1984. Part of his studies for the Ph.D., in 1980 and 1984, he did at Stanford University, where he was also a postdoctoral fellow in 1985–1986.
At the same time as his undergraduate and graduate studies, he served twice as the secretary of Kibbutz Kabri.
At the height of his academic work, and after having trained many students, some of whom were senior academic staff members themselves, Ron fell ill with a serious illness from which he died a short time later. He was laid to rest in the cemetery of Kibbutz Kabri.
Research and career
In his doctoral thesis, which was published in the mid-1980s, Ron entered the then young field of paleomagnetism research. In this work, he developed innovative research methods, including magnetic measurements of sedimentary rocks, that were used to reconstruct tectonic of blocks rotations between the Galillee faults. These methods were a global breakthrough in the interrelationship between geological fieldwork and geophysics, and are an important landmark in paleomagnetic research in general, even by today's standards. He went on for a post-doctorate at Stanford University, California, and returned to Israel with the means to establish the first paleomagnetic laboratory in Israel, which was established at the Geophysical Institute of Israel - one of the first cryogenic magnetometers in the world was placed in this laboratory, which constituted the latest technology of paleomagnetic research. In 2001, Ron moved with the laboratory to the Earth Sciences Institute at the Hebrew University of Jerusalem. He made significant contributions to the timing of hominid dispersal out of Africa, having nailed down the date of the oldest discoveries in Israel. For that time, "he championed the use of Israeli and Jordanian archeological materials, most notably metallurgical slag deposits, for the study of paleointensity variations in the southern Levant".Main studies
His main studies dealt with:- Brittle deformation and breakage - for the first time in the world proof of rotation of limited blocks in replicas around a vertical axis using paleomagnetic measurements. The formation of new faults according to the stress field that has not undergone change and deformation of the oceanic crust.
- Magnetism in present-day lake sediments, and paleomagnetism of dried lakes, as "recordings" of the Earth's magnetic field.
- Magnetostratigraphy - creating a stratigraphic column based on the column of rocks, the variation of magnetism in rocks and seismotectonics, along the Dead Sea transform.
- The development of internal structures of the Dead Sea transform based on paleomagnetic studies carried out mainly on volcanic rocks from the late Cenozoic and Pleistocene periods and on sedimentary rocks combined with them, including determination of isotopic ages.
- The development of magnetism in rocks due to metamorphosis processes.
- A paleomagnetic and rock magnetism study of Precambrian bedrock from Timna.
- Archaeomagnetism - determining the absolute strength of the Earth's magnetic field during the last seven thousand years.
- Using paleomagnetism methods to reconstruct past tectonic activity in a wide range of geological settings including: Cyprus, North America, and Israel.
- Incorporating paleomagnetism and rock magnetism in interrelated fields of research like ancient and recent earthquakes, by combining archaeological and geological observations.
- Dating rock sections in prehistoric sites, which include tools, using the magnetism in the rock, and cosmogenic isotopes.