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Gravity, Topography, and Early Evolution of the Moon - Shoemaker Lecture

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Overview

Explore the early evolution of the Moon through gravity and topography data in this AGU Fall Meeting Shoemaker Lecture. Delve into findings from the Lunar Orbiter Laser Altimeter (LOLA) and Gravity Recovery and Interior Laboratory (GRAIL) mission, examining lunar topography, crustal thickness, density, and porosity. Investigate the role of impact bombardment in shaping the Moon's surface and interior, including the size-frequency distribution of craters and their effects on crustal melting and redistribution. Analyze case studies such as the Shackleton crater, examining its age, floor composition, and reflectance properties. Compare lunar observations with data from other terrestrial planets to gain a comprehensive understanding of early planetary evolution. Learn about advanced measurement techniques, including multibeam laser altimetry and gravity mapping, and their applications in planetary science.

Syllabus

Introduction
Introducing Maria Zuber
Awards and Honors
Harry Hess Medal
Welcome
Lunar Reconnaissance Orbiter
Multibeam Laser Altimeter
Multibeam System
Roughness Measurement
Laser Tracking
Lunar Topography
Smaller Smaller Crater Sizes
Lunar Global Data Sets
Case Study Shackleton
How old was Shackleton
The floor of Shackleton
Laser backscatter measurement
Shackleton reflectance
Gravity data
Grail mission
Nominal mapping
Measurements
Frequency Domain
Gravity and Topography
Terrestrial Planetary Bodies
Clementine Mission
Free Air Gravity
Lunar Highlands
Porosity
Crust thickness
Aluminum abundance
Giant impact
Gravity
Lavafilled Dykes

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AGU

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