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  2. Voronoi diagram - Wikipedia

    en.wikipedia.org/wiki/Voronoi_diagram

    When two cells in the Voronoi diagram share a boundary, it is a line segment, ray, or line, consisting of all the points in the plane that are equidistant to their two nearest sites. The vertices of the diagram, where three or more of these boundaries meet, are the points that have three or more equally distant nearest sites.

  3. Tycho (lunar crater) - Wikipedia

    en.wikipedia.org/wiki/Tycho_(lunar_crater)

    Tycho is a relatively young crater, with an estimated age of 108 million years , based on analysis of samples of the crater ray recovered during the Apollo 17 mission. [3] This age initially suggested that the impactor may have been a member of the Baptistina family of asteroids, but as the composition of the impactor is unknown this remained ...

  4. String diagram - Wikipedia

    en.wikipedia.org/wiki/String_diagram

    One such definition is to define string diagrams as equivalence classes of well-typed formulae generated by the signature, identity, composition and tensor. In practice, it is more convenient to encode string diagrams as formulae in generic form, which are in bijection with the labeled generic progressive plane graphs defined above.

  5. File:Topographic model of Gale crater.stl - Wikipedia

    en.wikipedia.org/wiki/File:Topographic_model_of...

    Use of NASA logos, insignia and emblems is restricted per U.S. law 14 CFR 1221.; The NASA website hosts a large number of images from the Soviet/Russian space agency, and other non-American space agencies.

  6. File:Crater-depth-diagram.svg - Wikipedia

    en.wikipedia.org/wiki/File:Crater-depth-diagram.svg

    English: How crater-depth is measured, using the side-view of a typical crater. Depth "A" measures from the surface to the bottom of the crater. Depth "B" measures from the mean height of the rim to the bottom of the crater.

  7. Complex crater - Wikipedia

    en.wikipedia.org/wiki/Complex_crater

    A central-peak crater is the most basic form of complex crater. A central-peak crater can have a tightly spaced, ring-like arrangement of peaks, thus be a peak ring crater, though the peak is often single. [3] Central-peak craters can occur in impact craters via meteorites. An Earthly example is Mistastin crater, in Canada. [1]

  8. Tsiolkovskiy (crater) - Wikipedia

    en.wikipedia.org/wiki/Tsiolkovskiy_(crater)

    The crater protrudes into the neighbouring Fermi, an older crater of comparable size that does not have a lava-flooded floor. Tsiolkovskiy has been considered one of the largest craters of the Upper (Late) Imbrian age, [4] [5] although that dating was revised to the Imbrian/Eratosthenian boundary in 2013. [6]

  9. Mathematical formulation of the Standard Model - Wikipedia

    en.wikipedia.org/wiki/Mathematical_formulation...

    Interactions in the Standard Model. All Feynman diagrams in the model are built from combinations of these vertices. q is any quark, g is a gluon, X is any charged particle, γ is a photon, f is any fermion, m is any particle with mass (with the possible exception of the neutrinos), m B is any boson with mass. In diagrams with multiple particle ...