![]() ![]() To contact us, make sure to use our email in the about section of this channel. Any spam, insults or troll will be deleted. ![]() Please keep the comments section respectful. We publish 3 videos a week on our Youtube channel and many more articles on our website.įeel free to subscribe to not miss any of our updates and visit our website to discover additional content. Whenever you are curious or an incorrigible lover of this mysterious world, our videos are made for you ! Welcome back to the FLUCTUS channel for a discussion about the Panama Canal’s innovative lock system as well as some of the other systems in place at the biggest ports in the world.įluctus is a website and YouTube channel dedicated to sea geeks. The Genius Technologies Behind Panama Canal Locks Moving World Largest Ships We are pramote this video only for entertainment and educational perpose only. and this vIdeo is uploaded by Fluctus at. There is no discernable correlation between centers of active volcanism and topography.Hellow guys, Welcome to my website, and you are watching The Genius Technologies Behind Panama Canal Locks Moving World Largest Ships. takes time to the fluctus channel WebHow far is Sonipat from IGL CNG. 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. Sonipat, Haryana 131001, India: HP Petrol Pump - Bhagwani Filling Station the. ![]() 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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