In honor of the 50th Earth Day, Joe and Rob talk about...the earth! That is, the rock we call planet earth. They discuss some amazing experiments, done in the 1700s, that told us the mass of the earth and that calculated the gravitational constant. This is a big deal for us today, because there would be no space travel without these foundational experiments.

In honor of the 50th Earth Day, Joe and Rob talk about...the earth! That is, the rock we call planet earth. They discuss some amazing experiments, done in the 1700s, that told us the mass of the earth and that calculated the gravitational constant. This is a big deal for us today, because there would be no space travel without these foundational experiments.


Kenyan top-bar hives, Warre beehives, Layens beehives (Rob’s choice)


What’s inside the earth? Solid rock. Not lava. 80% melt temperature. The core might be solid


The Oklo ‘natural reactor’, deep under Gabon, Africa


Mass of the earth: 5.972 × 10^24 kg


Density of granite


Schiehallion experiment, 1774


Nautical miles


Minutes and seconds of arc


Mass vs weight


Newton’s Second Law of Motion, F = ma


The law of gravity


Satellite laser range finding


Cavendish experiment, 1798


The history of the Cavendish Laboratory


The Schweinfurt raid, 1943


Types of earthquake waves


Acoustic shadows


Seismic tomography and deep crustal rocks


The Gulf of Corinth


The San Andreas Fault


The Emperor Seamount chain


Is plate tectonic happening today?


Baumgardner’s TERRA model