Sabine & Ritter: [NE/J11] About 60 miles west of the Apollo 11 landing site you will see two curious craters: Sabine and Ritter. They are unusual because they should be deeper than they are. Look closely at Sabine (the easternmost) and you will see that its shallow floor looks like it has been cut out by a giant cookie cutter. Both Sabine and Ritter are floor-fractured craters (FFC’s).
A floor-fractured crater is a special type of crater that has been modified by later volcanism, uplift, and consequent fracturing. Some of the common characteristics of FFC’s are that they are large, they have rilles (both arcuate and linear), they occur near the borders of maria, and (most significantly) they are very shallow for their size.
Floor-fractured craters have a fascinating genesis. Sometime after the crater was formed and had settled in, magma rising up from underneath the basin actually pushed the crater floors upward (hence their shallowness). It was not an effortless process and the resulting strain caused radial and concentric fractures to appear on the floor. At times, lava would also flow upward through these fractures and spill out onto the crater floor.
It is highly recommended that you get a copy of Sky and Telescope’s Field Map of the Moon, the very finest Moon map available for use at the telescope. It is available for $10.95 at www.skyandtelescope.com and on Amazon. All features mentioned in this blog will be keyed to the grid on the Field Map and will look like this: Plato: [NW/D9]
Courtesy of Gray Photography of Corpus Christi, Texas
Lunar photos: NASA / USGS / BMDO / LROC / ASU / DLR / LOLA / Moon Globe. Used by permission
Latest posts by Andrew Planck (see all)
- Geminus and Burckhardt: Two Unique Moon Craters - January 17, 2022
- Most Spectacular Example of Subsidence on the Moon: Sinus Iridum - January 10, 2022
- Peirce and Picard: Two Largest Intact Moon Craters on Mare Crisium - January 3, 2022