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Glen H. Fountain

Researcher at Johns Hopkins University Applied Physics Laboratory

Publications -  14
Citations -  663

Glen H. Fountain is an academic researcher from Johns Hopkins University Applied Physics Laboratory. The author has contributed to research in topics: Solar System & Interstellar probe. The author has an hindex of 5, co-authored 13 publications receiving 567 citations.

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The Pluto system: Initial results from its exploration by New Horizons.

S. A. Stern, +150 more
- 16 Oct 2015 - 
TL;DR: The New Horizons encounter revealed that Pluto displays a surprisingly wide variety of geological landforms, including those resulting from glaciological and surface-atmosphere interactions as well as impact, tectonic, possible cryovolcanic, and mass-wasting processes.
Journal ArticleDOI

Initial results from the New Horizons exploration of 2014 MU69, a small Kuiper Belt object

S. A. Stern, +215 more
- 17 May 2019 - 
TL;DR: Stern et al. as mentioned in this paper presented the initial results from the New Horizons flyby of MU_(69) on 1 January 2019, which consists of two lobes that appear to have merged at low speed, producing a contact binary.
Journal ArticleDOI

Initial results from the New Horizons exploration of 2014 MU69, a small Kuiper Belt Object

S. A. Stern, +204 more
TL;DR: The New Horizons spacecraft completed its MU69 flyby on 1 January 2019, with a closest approach distance of 3538 km—less than one-third of its closest distance to Pluto.
Journal ArticleDOI

MERLIN: Mars-Moon Exploration, Reconnaissance and Landed Investigation

TL;DR: The Mars-Moon Exploration, Reconnaissance and Landed Investigation (MERLIN) mission as mentioned in this paper was designed to obtain in situ measurements from Deimos to test models for the moon's origin.

WITTEX: A Constellation of Three Small Satellite Radar Altimeters

TL;DR: WITTEX as discussed by the authors consists of three co-planar small satellite radar altimeters launched on the same vehicle into a GEOSAT-class orbit, which can support measurement of both orthogonal components of the ocean's surface slope, rather than the single component seen by conventional instruments.