Moons of Uranus and Neptune, Part 2 Codexery

Gertrude (crater)

Largest known crater on Uranus's moon Titania.

Gertrude (crater)

Gertrude is the largest crater on Titania, a moon of Uranus. This impact basin features a peak ring and measures between 326 and 400 kilometers in diameter, which is roughly one-fifth to one-quarter of Titania’s own size. The crater was first spotted by the Voyager 2 spacecraft as it flew past the Uranian system in January 1986. Its name comes from Gertrude, the mother of Prince Hamlet in Shakespeare’s *Hamlet*, following the convention of naming Titania’s features after female Shakespearean characters. The International Astronomical Union officially adopted the name in 1988.

The crater is surprisingly shallow. In 1989, planetary scientist P. M. Schenk estimated its depth at only 1 to 3 kilometers. Its rim rises about 2 kilometers above the crater floor, and at the center sits a large dome roughly 150 kilometers wide and 2 to 3 kilometers high—formed when the surface uplifted right after the impact. For a crater this size, both the rim and dome are low, suggesting the terrain has relaxed over time. The dome itself has few smaller craters on it, indicating it was reshaped later. Linear ridges cut across Gertrude and the nearby Messina Chasmata. Surrounding the crater are plains that are less heavily cratered than most of Titania’s surface, likely the remains of Gertrude’s ancient ejecta blanket.

Based on depth-to-diameter ratios of smaller Titania craters, Gertrude’s original depth may have been around 6 to 6.5 kilometers. Its current shallowness implies a period of relaxation, during which the crust slowly crept and smoothed out extreme topography. The central dome is a telltale sign of this process, and the crater’s floor resembles that of Tirawa, a large relaxed crater on Saturn’s moon Rhea.

Quick Facts

Location
Titania
Diameter
~326 km / (GPN) · 400 ± / (Moore et al.)
Depth
~1 –
Discoverer
Voyager 2
Eponym
Gertrude, mother of Prince Hamlet

Facts from the source article.

Lore & Background

Gertrude's depth was estimated to be roughly 1–3 kilometers by planetary scientist P. M. Schenk in 1989. The crater rim is elevated by 2 km over the crater floor. In the center of the crater there is a large dome, which resulted from the uplift of the surface immediately after the impact. The dome has a diameter of about 150 km and is 2–3 km high. The rim and dome are low for a crater with such a large diameter, indicating that the relief has relaxed since the impact. The surface of the dome has only few superimposed smaller craters, meaning it was modified later. Linear ridges cut across Gertrude and the nearby Messina Chasmata. Gertrude is additionally surrounded by plains with less cratering compared to much of Titania's surface, likely representing Gertrude's ancient ejecta blanket.

Reader's Guide

Gertrude is unusually shallow; extrapolating from depth-to-diameter ratios of smaller craters on Titania, its original depth may have been ~6–6.5 km. This implies that Gertrude underwent a period of relaxation, where the crust slowly creeps and gradually mutes topographical extremes. The central doming of Gertrude's floor is indicative of relaxation; its floor appears similar to the central domed floor of a large relaxed crater on Saturn's moon Rhea, Tirawa. The name Gertrude was officially adopted by the International Astronomical Union (IAU) in 1988. Features on Titania are named after female Shakespearean characters.

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