It illuminates each of the individual switches with one LED each.
#FLUCTUS CHANNEL SOFTWARE#
In order to be able to set this up later, Roccat makes the software called Swarm available for download on their site.Īs mentioned at the beginning, the Pyro is equipped with Roccat’s Aimo technology. As an extension to this, Roccat uses their Easy-Shift technology again, which allows the keys around WASD to be assigned two functions. In addition, the Pyro comes with macro keys, which are located at F8 to F12 and can be accessed with the FN key. The volume control can be operated precisely and very smoothly. Of course, this is nothing innovative, we can find similar things on many other keyboards. On the upper right edge of the pyro there is a small LED strip with volume control. We could not determine any optical defects or processing errors after a first inspection.
Around the brushed aluminum layer is a small plastic edge, which stands out visually with grooved stripes. In combination with the matt black keycaps, the first impression is right. The top of the keyboard case is coated with dark gray brushed aluminum. There is no discernable correlation between centers of active volcanism and topography.Stripped of its foil, the Pyro cuts a fine figure from the very first second – and there’s a clear reason for that. Although the most active volcanic centers appear to be found in structural lows (as indicated by mapping of scarps), DEMs derived from stereo images show that, with the exception of Tohil Mons, there is less than 1 km of relief in the Culann–Tohil region. From 0°–15° S the hummocky bright plains unit away from volcanic centers contains scarps, grooves, pits, graben, and channel-like features, some of which have been modified by erosion. Neighboring Radegast Patera contains a NIMS hotspot and a young lava lake of dark silicate flows, whereas the southwest portion of Tohil Patera contains white flow-like units, perhaps consisting of ‘ponds’ of effusively emplaced SO 2. Tohil Mons also contains a younger unit of mottled crustal materials that were displaced by mass wasting processes. The main massif of Tohil Mons is covered with ridges and grooves, defining a unit of tectonically disrupted crustal materials. These red–brown flows have a distinct color that is suggestive of a compositional difference, although whether this is due to surface alteration or distinct lava compositions cannot be determined. Fresh and red-mantled dark lava flows west of the Culann vent can be contrasted with unusual red–brown flows east of the vent. The Culann volcanic center has produced a range of explosive and effusive deposits, including an outer yellowish ring of enhanced sulfur dioxide (SO 2 ), an inner red ring of SO 2 with short-chain sulfur (S 3 –S 4 ) contaminants, and two irregular green diffuse deposits (one in Tohil Patera) apparently produced by the interaction of dark, silicate lava flows with sulfurous contaminants ballistically-emplaced from Culann's eruption plume(s).
Tsũi Goab Fluctus is the center of a low-temperature hotspot detected by NIMS late during the Galileo mission, and could represent the best case for active effusive sulfur volcanism detected by Galileo.
Analysis of Voyager global color and Galileo Solid-State Imaging (SSI) high-resolution, regional (50–330 m/pixel), and global color (1.4 km/pixel) images, along with available Galileo Near-Infrared Mapping Spectrometer (NIMS) data, suggests that 16 distinct geologic units can be defined and characterized in this region, including 5 types of diffuse deposits. This region includes a newly discovered shield volcano, Tsũi Goab Tholus and a neighboring bright flow field, Tsũi Goab Fluctus, the active Culann Patera and the enigmatic Tohil Mons-Radegast Patera–Tohil Patera complex. We have used Galileo spacecraft data to produce a geomorphologic map of the Culann–Tohil region of Io's antijovian hemisphere.
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