Earth is a planet that records its own history through the accumulation of sediment at its surface. Few sedimentary basins around the globe preserve a longer or more detailed record of that history than the Umbria-Marche Basin in central Italy, where a continuous record of sedimentation from the Jurassic through the present day are exposed throughout the Apennine Mountains. Italy is the birthplace of the geological science of stratigraphy, which seeks to establish the chronology of sedimentary rock deposition.

The majority of Earth’s volume is composed of igneous and metamorphic rocks, which originate through processes that operate deep beneath earth’s surface, driven by the movement of tectonic plates. Igneous and metamorphic rocks preserve an interpretable record of the creation and modification of continents, mountain building, earthquakes, and volcanic eruptions. The formation and existence of these rocks, in turn, modulate global volatile cycles, and the evolution of life on earth.

The majority of Earth’s volume is composed of igneous and metamorphic rocks, which originate through processes that operate deep beneath earth’s surface, driven by the movement of tectonic plates. Igneous and metamorphic rocks preserve an interpretable record of the creation and modification of continents, mountain building, earthquakes, and volcanic eruptions. The formation and existence of these rocks, in turn, modulate global volatile cycles, and the evolution of life on earth.

Ours is a restless planet where plates drift, and continents rift apart and collide. The record of this is written in the deformation of the crust – manifested as faults, folds, and rock fabric. In this class we will learn to recognize and assess these and other structures, to quantify the deformation that occurred as the structures were made, and to infer the forces that were at work.

Ours is a restless planet where plates drift, and continents rift apart and collide. The record of this is written in the deformation of the crust – manifested as faults, folds, and rock fabric. In this class we will learn to recognize and assess these and other structures, to quantify the deformation that occurred as the structures were made, and to infer the forces that were at work.

For at least 3.5 billion years, Earth’s surface environments have supported some form of life. What geologic processes first created and subsequently maintained a habitable environment? How does contemporary global climate change compare to climate variations over Earth’s long history? This course looks at Earth’s climate and its surface environment from a geologist’s perspective. We will develop an understanding of the atmospheric, oceanographic, geological, and biological systems that interact to modulate the climate.

For at least 3.5 billion years, Earth’s surface environments have supported some form of life. What geologic processes first created and subsequently maintained a habitable environment? How does contemporary global climate change compare to climate variations over Earth’s long history? This course looks at Earth’s climate and its surface environment from a geologist’s perspective. We will develop an understanding of the atmospheric, oceanographic, geological, and biological systems that interact to modulate the climate.

For at least 3.5 billion years, Earth’s surface environments have supported some form of life. What geologic processes first created and subsequently maintained a habitable environment? How does contemporary global climate change compare to climate variations over Earth’s long history? This course looks at Earth’s climate and its surface environment from a geologist’s perspective. We will develop an understanding of the atmospheric, oceanographic, geological, and biological systems that interact to modulate the climate.

How well do you know the planet on which we live? In this course we will explore Earth from its core to its surface, from the mountains to the deep ocean basins, from the past and present to the future. The  earth is an evolving and dynamic system, changing on time scales that range from seconds, to millennia, to eons: volcanos erupt, earthquakes vibrate the globe, continents separate and collide, and mountains rise only to be worn away and rise again. What physical processes drive this dynamism? How does the restless nature of Earth impact our residency?

How well do you know the planet on which we live? In this course we will explore Earth from its core to its surface, from the mountains to the deep ocean basins, from the past and present to the future. The  earth is an evolving and dynamic system, changing on time scales that range from seconds, to millennia, to eons: volcanos erupt, earthquakes vibrate the globe, continents separate and collide, and mountains rise only to be worn away and rise again. What physical processes drive this dynamism? How does the restless nature of Earth impact our residency?