Red Rocks Climbing sample topo Black Orpheus III 5.10a, Solar Slab Gully, Red Rocks Black Orpheus ascends a huge overhung headwall via a cleanly fractured dihedral and has some of the best moderate crack climbing at Red Rocks. We have provided a FREE topo of Black Orpheus to whet your appetite to purchase our Red Rocks Climbing guidebook.
High Sierra Climbing sample topo Red Dihedral IV 5.10b, Incredible Hulk, High Sierra Red Dihedral is one of the best 5.10 route in the High Sierra. The routes splitter cracks, incredible Yosemite-like rock lead to a great summit with big exposure on all sizes. We have provided a FREE topo of Red Dihedral to whet your appetite to purchase our High Sierra Climbing guidebook.
Tuolumne Free Climbs sample topo Regular Route 5.9, Fairview Dome, Tuolumne Meadows The Regular Route of Fairview Dome is listed in Fifty Classic Climbs of North America—“routes which ambitious climbers dream of doing”—and there is no doubt it is one of the climbs to dream about in Tuolumne Meadows. The route follows the longest steep line in Tuolumne and contains pitch after pitch of sustained and rewarding cracks. We have provided a FREE topo of Fairview Dome to whet your appetite to purchase our Tuolumne Free Climbs guidebook.
The annual list of popular torrent sites features well-known brands, and this year there are some notable additions. The new entrants are a pair of gaming-focused sites; skidrowreloaded.com and igg-games.com.
We have limited the list to English-language torrent sites, which means that sites such as Rutracker.org, Rutor.info, Dytt8.net and Etoland.co.kr are not included, despite the fact that they have substantial traffic numbers.
Below is the full list of the top ten most-visited torrent site domains at the start of the new year. The list is based on various traffic reports. Please note that this list is created as a historical record, to keep track of the popularity of these sites over time.
NYAA.si is a popular resurrection of the anime torrent site NYAA. While there is fierce competition from alternative pirate streaming sites, the torrent portal continues to do well, climbing two positions compared to last year.
Skidrow and RELOADED are two iconic game-cracking groups. This likely served as inspiration for the people running Skidrowreloaded.com, which is a blog-style release site featuring popular game releases.
Launched a little over four years ago, TorrentGalaxy is a relatively new torrent site. It has a dedicated group of uploaders and an active community. In addition to torrents, TorrentGalaxy also makes some releases available for streaming.
Disclaimer: Proxies and clear copycats are excluded. Please keep in mind that many sites have mirrors or alternative domains, which are often not taken into account here. The yearly list is published as an informational / news resource. The 2022 torrent site list is archived.
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Thousands of supraglacial lakes form each spring and summer on top of the Greenland Ice Sheet as sunlight returns to the region. Many lakes disappear within hours when large cracks form below them, draining the lakes and sending torrents of water to the base of the ice sheet. To learn what triggers this phenomenon, a team of scientists installed a network of GPS units around a lake.
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Overflow water on the top of Khanh waterfall flowed into the cracks and underground caves of the limestone layer (Fig. 17A, B). The water in cracks and underground caves increased the uplift water force and driving water force (Fig. 13). The increasing of destabilizing forces caused the slope to fail. The collapsed surface was the fault between the limestone layer and the shale layer (Fig. 18). The limestone blocks at the top of slope moved together with the talus deposit at the toe of slope. This mixture crossed the river and passed over the opposite hill. The large and fast moving mass destroyed five houses and killed eighteen people at the opposite hill. The collapse process was simulated based on Coulomb mixture theory (Denlinger and Iverson 2001). This method assumes that grain-fluid flows behave as mixtures limestone layer at the top and the talus deposit at the toe of slope. The simulation results show that the range of moving mass is similar to the actual phenomena at Khanh waterfall landslide.
Another nearby areas are P1 and P2 areas on the right bank downstream of Khanh waterfall. Since the topography of the P1 and P2 areas is similar to the old landslide site, it was feared that landslides would continue to occur in the future. However, the survey results show that the geology at areas P1 and P2 is different from the geology at Khanh waterfall (Fig. 19). The geology at areas P1 and P2 is mainly limestone interspersed with a thin shale layer. In addition, the surface and groundwater in areas P1 and P2 and the Khanh waterfall landslide area are considered to have different water supply channels due to differences in water quality. It suggests that areas P1 and P2 may have a different phenomena compared with Khanh waterfall landslide.
The collapse of Khanh waterfall was different from some previous collapses of waterfalls due to erosion at the toe of the slope. Due to the torrent rain continuing for 48 h, a large amount of water flowing from the upper stream network channel concentrated in the Khanh waterfall area. It resulted in a large amount of groundwater flowed in the cracks and karsts in Khanh waterfall slope. The water in cracks and karsts increased the uplift water force and driving force causing slope failure. The increasing of destabilizing forces caused the slope to collapse. The sliding surface was the small fault between the limestone layer and the shale layer.
There are many possible approaches to regulation of grading through the subdivision ordinance. In a discussion of how to avoid grading problems, the Home Builders Manual says: "Contour intervals should vary with the type of property encountered. Where the site contains grades which average 3 per cent or less, use contours with a one-foot interval. A greater interval will be of little value on flat topography. Where slopes are up to 15 per cent, a two-foot contour interval should be used with a five-foot interval for slopes of 15 per cent and over." 2b1af7f3a8