Martin Hill
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During the XVII Italian Antarctic expedition (2001/02), 61 rocks have been sampled within the aim of the project "Role of Cenozoic tectonic and glacial events in the landscape evolution of the Victoria Land region" in northern Victoria Land. They include subvolcanic and metamorphic rocks. The investigated regions are within Cape Adare SR 59-60/13*, Cape Hallett SS 58-60/2, Coulman Island SS 58-60/6, Freyberg Mountains SS 58-60/1 and Mount Murchison SS 58-60/5 USGS sheets.
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During the XXVII Italian Antarctic expedition (2011/12), 143 rocks have been sampled within the aim of the project "Xenoliths and basic lavas for the knowledge of the C-O-H system in the lithospheric mantle of the polar regions" 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 and Mount Murchison SS 58-60/5 USGS sheets.
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During the XV, XVI and XVII Italian Antarctic expeditions (1999/2000, 2000/01, 2001/02), 259 rocks have been sampled within the aim of the project "Cenozoic magmatism in the area north of Tucker Glacier, northern Victoria Land, Antarctica" in northern Victoria Land. They include intrusive, subvolcanic, volcanic, metamorphic and sedimentary rocks. The investigated regions are within Cape Adare SR 59-60/13*, Cape Hallett SS 58-60/2, Coulman Island SS 58-60/6, Freyberg Mountains SS 58-60/1 and Mount Melbourne SS 58-60/9 USGS sheets.
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During the IV Italian Antarctic expedition (1988/89), 819 rocks have been sampled within the aim of the project "Regional geology, tectonics, 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 Adare SR 59-60/13*, Cape Hallett SS 58-60/2, Coulman Island SS 58-60/6, Freyberg Mountains SS 58-60/1, Mount Melbourne SS 58-60/9, Mount Murchison SS 58-60/5 and Reeves Névé SS 55-57/12 USGS sheets.