Nathan Hills
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During the VI Italian Antarctic expedition (1990/91), 394 rocks have been sampled within the aim of the project "Regional and structural geology, stratigraphy, geological mapping and remote sensing" in northern Victoria Land. They include intrusive, subvolcanic, volcanic, metamorphic and sedimentary rocks. The investigated regions are within Cape Hallett SS 58-60/2, Coulman Island SS 58-60/6, Franklin Island ST 57-60/2*, Freyberg Mountains SS 58-60/1, Mount Joyce SS 55-57/16, Mount Melbourne SS 58-60/9, Mount Murchison SS 58-60/5, Reeves Névé SS 55-57/12, Ross Island ST 57-60/6*, Sequence Hills SS 55-57/8 and Welcome Mountain SS 55-57/4 USGS sheets.
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Rocks from the project “Cenozoic geodynamics in the Ross Sea area: magmatism and tectonic evolution"
During the IX Italian Antarctic expedition (1993/94), 376 rocks have been sampled within the aim of the project "Cenozoic geodynamics in the Ross Sea area: magmatism and tectonic evolution" in northern Victoria Land. They include intrusive, subvolcanic, volcanic and metamorphic rocks. The investigated regions are within Cape Hallett SS 58-60/2, Coulman Island SS 58-60/6, Mount Melbourne SS 58-60/9, Mount Murchison SS 58-60/5, Reeves Névé SS 55-57/12 and Relief Inlet SS 58-60/13 USGS sheets.
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During the XXVI and XXVII Italian Antarctic expeditions (2010/11, 2011/12), 668 rocks have been sampled within the aim of the project "Geological continental markers of Cenozoic climate changes in Victoria Land, Antarctica" in northern Victoria Land. They include intrusive, subvolcanic, volcanic, metamorphic and sedimentary rocks. The investigated regions are within Cape Hallett SS 58-60/2, Coulman Island SS 58-60/6, Mount Joyce SS 55-57/16, Mount Melbourne SS 58-60/9, Mount Murchison SS 58-60/5 and Relief Inlet SS 58-60/13 USGS sheets.
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During the II Italian Antarctic expedition (1986/87), 885 rocks have been sampled within the aim of the project "Earth Sciences. Structural geology" in northern Victoria Land. They include intrusive, subvolcanic, volcanic, metamorphic and sedimentary rocks. The Bowers Terrane is reached for the first time. The investigated regions are within Coulman Island SS 58-60/6, Mount Melbourne SS 58-60/9, Mount Murchison SS 58-60/5, Reeves Nevé SS 55-57/12, Relief Inlet SS 58-60/13 and Sequence Hills SS 55-57/8 USGS sheets.