EGU25-21276, updated on 15 Mar 2025
https://doi.org/10.5194/egusphere-egu25-21276
EGU General Assembly 2025
© Author(s) 2025. This work is distributed under
the Creative Commons Attribution 4.0 License.
  Identification of a lunar volcanic dome termed L1 in Promontorium Laplace and mineralogy
Maximilian Teodorescu1 and Raffaello Lena2
Maximilian Teodorescu and Raffaello Lena
  • 1Institute of Space Science, 409, Atomistilor Street 077125 Bucharest-Magurele, Romania
  • 2ALPO and BAA coordinator for lunar domes program via Cartesio144 D 00137 Rome, Italy

In recent years, with the advancements in digital sensors technology and access to space probes data, more and more lunar features are discovered using ground-based images. Mostly, these features are lunar domes, with tens of such structures being discovered using medium-sized telescopes.

In the following study we examine a lunar dome, termed Laplace 1 (L1), identified using telescopic images, Lunar Reconnaissance Orbiter (LRO) Wide Area Camera (WAC) images, the Laser Altimeter Digital Elevation Model (LOLA DEM), and the LRO WAC-based GLD100 Digital Terrain Model (DTM) along with data from the Chandrayaan-1 Moon Mineralogy Mapper, Diviner dataset and Kaguya Multiband Imager. The dome lies at coordinates of 48.57°N and 26.37°W, at about 36 km south east of the crater Maupertuis, and has a base diameter of 7.6 km ± 0.3 km, a maximum height of 230 ± 20 m, resulting in a slope angle of 3.4° ± 0.3°. We also infer the mineralogical composition of the dome.

 

How to cite: Teodorescu, M. and Lena, R.:   Identification of a lunar volcanic dome termed L1 in Promontorium Laplace and mineralogy, EGU General Assembly 2025, Vienna, Austria, 27 Apr–2 May 2025, EGU25-21276, https://doi.org/10.5194/egusphere-egu25-21276, 2025.