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  2. List of mountains on Io - Wikipedia

    en.wikipedia.org/wiki/List_of_mountains_on_Io

    Other mountains appear to be tilted crustal blocks, with a shallow slope from the formerly flat surface and a steep slope consisting of formerly sub-surface materials uplifted by compressive stresses. Both types of mountains often have steep scarps along one or more margins. Only a handful of mountains on Io appear to have a volcanic origin.

  3. Mountains of Io - Wikipedia

    en.wikipedia.org/wiki/Mountains_of_Io

    Stress plays an important role in the origin of Io's mountains. Various kinds of stresses are considered to be responsible for the deformation of the lithosphere. Folding and faulting form all kinds of topographic features on Io. Overburden stress: on Io, the resurfacing process keeps forming new layers at the surface and pushing older layer ...

  4. Euboea Montes - Wikipedia

    en.wikipedia.org/wiki/Euboea_Montes

    Euboea Montes is rugby ball shaped (175 km by 240 km), located about 40 kilometers east of Creidne Patera caldera. It has an altitude of 10.5 km. There is a curved ridge crest which divides Euboea Montes into two sections: the steep, southern flank with an uneven surface of rounded mounds and the smoother, northern flank sloping about 6° to ...

  5. Tafel equation - Wikipedia

    en.wikipedia.org/wiki/Tafel_equation

    Tafel plot for an anodic process (oxidation) The Tafel equation is an equation in electrochemical kinetics relating the rate of an electrochemical reaction to the overpotential. [1] The Tafel equation was first deduced experimentally and was later shown to have a theoretical justification. The equation is named after Swiss chemist Julius Tafel.

  6. Zamama (volcano) - Wikipedia

    en.wikipedia.org/wiki/Zamama_(volcano)

    Zamama A (18°N, 175°W), is about 40 km (25 mi) wide, 1.5 km (0.93 mi) high, and has an average slope of 40°. Slope and height were estimated by PC. It extends about 140 km (87 mi) east and beyond the topographic margin of the observed steep-sided shield. Zamama A is the source of the Zamama flow field.

  7. Thomagata Patera - Wikipedia

    en.wikipedia.org/wiki/Thomagata_Patera

    Thomagata is located near the center of a low, 100 km (62 mi) wide mesa. The edge of the mesa rises 200 meters (660 ft) above the surrounding plains, however the slope up to the edge of Thomagata Patera is unknown. If the floor of the patera is at the same level as the surrounding plains, the western slope of the mesa would have a grade of 2°. [2]

  8. Shockley diode equation - Wikipedia

    en.wikipedia.org/wiki/Shockley_diode_equation

    n {\displaystyle n} is the ideality factor, also known as the quality factor, emission coefficient, or the material constant. The equation is called the Shockley ideal diode equation when the ideality factor equals 1, thus is sometimes omitted. The ideality factor typically varies from 1 to 2 (though can in some cases be higher), depending on ...

  9. Agar.io - Wikipedia

    en.wikipedia.org/wiki/Agar.io

    Mode (s) Multiplayer. Agar.io[a] is a massive multiplayer online action game created by Brazilian developer Matheus Valadares. Players control one or more circular cells in a map representing a Petri dish. The goal is to gain as much mass as possible by eating cells and player cells smaller than the player's cell while avoiding larger ones ...