1/5/2023 0 Comments Rift dustwind hills![]() ![]() Average erosion rates reach as high as 2–4 mm/a, which is explained by the frequency of catastrophic mass-transport events able to mobilize in one single episode between 106 and 107 tons of detritus, corresponding to 10–50 mm of erosion distributed across the catchment upstream. River channels here display extreme steepness (ksn up to 200–300) and low concavity indices (θ 0.15 - 0.35) typical of thalwegs shaped by debris flows. Results clearly indicate that volcanic and basement rocks supply a disproportionate amount of sand relatively to their outcrop area, testifying to strongly focused erosion in the high-relief axial part of the range. The accurate definition of mineralogical signatures characterizing detritus derived from six end-member volcanic, metamorphic basement, and sedimentary/metasedimentary rock units allowed us to calculate the relative contribution of each to the sand load, with particular precision for the Baksan River draining Mt. Also presented is an extensive review of sediment-transport data available in the Russian literature on glacial-lake outburst floods and rainfall-triggered debris flows, which owing to global warming and glacier retreat have afflicted the Greater Caucasus with increasing frequency in the last 50 years. In this rugged mountain region, we have investigated sand generation and erosion patterns by using high-resolution petrographic and heavy-mineral data on river sands complemented by detailed morphometric analysis of 9 major mountain branches of the Terek River. more Abstract The highest peaks in Europe are found in the central Greater Caucasus, an orogenic belt characterized by extremely active tectonic and sedimentary processes. In the mid-Miocene Nataraja Slide (the second-largest mass-transport deposit reported from passive margins worldwide), dominant carbonate detritus and depleted heavy-mineral suites (including apatite, garnet, and locally augite or rare aegirine) reveal gravitational failure and sliding of the entire s.Ībstract The highest peaks in Europe are found in the central Greater Caucasus, an orogenic belt. Occurrence of euhedral aegirine and apatite in lower Paleocene mudrocks can be tied to alkaline volcanism affecting the adjacent western Indian margin during the late stage of Deccan activity. In the cored Laxmi Basin succession, heavy minerals are far less affected by selective diagenetic dissolution than in foreland-basin sandstones exposed along the Himalayan front. more Provenance analysis of IODP Expedition 355 cores in the Laxmi Basin sheds new light on the erosional evolution of the Himalayan belt and its western syntaxis during the Neogene and on large-scale mass-wasting and magmatic events that affected the western continental margin of India in the mid-Miocene and early Paleocene. On PvP servers these areas are considered contested, even though the zone it is contained in is a Horde/Alliance territory.Provenance analysis of IODP Expedition 355 cores in the Laxmi Basin sheds new light on the erosio. Pvp objective area? (Death's Door also has this flag although it's no pvp object area) ![]() Not used now (no area/zones with this flag set in 3.0.3)Įxpansion zones? (only Circle of Blood Arena not have this flag, but have 0x00000400 flag) Only Netherwing Ledge, Socrethar's Seat, Tempest Keep, The Arcatraz, The Botanica, The Mechanar, Sorrow Wing Point, Dragonspine Ridge, Netherwing Mines, Dragonmaw Base Camp, Dragonmaw Skyway Only for one zone named "City" (where it located?)Įxpansion zones? (only Eye of the Storm not have this flag, but have 0x00004000 flag) Only used for areas on map 571 (development before) Snow (only Dun Morogh, Naxxramas, Razorfen Downs and Winterspring) Reference to what zone intro music to play when entering area ![]() Reference to what Ambiance to use during day and night For the purposes of this wiki article, the zone IDs, names, mapID and AreaID will be included. This DBC contains the zone and subzone lists.
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