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Chaotic Descriptor Table
Castle Oldskull Supplement CDT1: Chaotic Descriptor Table These ideas would require a few hours’ the players back to the temple of the more development to become truly useful, serpent people, I decide that she has some but I like the direction that things are going backstory. She’s an old jester-bard so I’d probably run with it. Maybe I’d even treasure hunter who got to the island by redesign dungeon level 4 to feature some magical means. This is simply because old gnome vaults and some deep gnome she’s so far from land and trade routes that lore too. I might even tie the whole it’s hard to justify any other reason for her situation to the gnome caves of C. S. Lewis, to be marooned here. She was captured by or the Nome King from L. Frank Baum’s the serpent people, who treated her as Ozma of Oz. Who knows? chattel, but she barely escaped. She’s delirious, trying to keep herself fed while she struggles to remember the command Example #13: word for her magical carpet. Malamhin of the Smooth Brow has some NPC in the Wilderness magical treasures, including a carpet of flying, a sword, some protection from serpents thingies (scrolls, amulets?) and a The PCs land on a deadly magical island of few other cool things. Talking to the PCs the serpent people, which they were meant and seeing their map will slowly bring her to explore years ago and the GM promptly back to her senses … and she wants forgot about it. -
Sample File ACCURSED DEFILER CR 4 (1,100 XP) CHECKLIST M Undead, NE Speed 30' 1
Sample file ACCURSED DEFILER CR 4 (1,100 XP) CHECKLIST M undead, NE Speed 30' 1. Accursed Defiler 33. Forest Marauder 66. Ratatosk 2. Amphiptere 34. Frostveil 67. Ravenala AC 12 HP 75 (10d8+30) 3. Angel, Fidele 35. Ghoul, Darakhul 68. Rift Swine S 19|+4 D 14|+2 C 17|+3 I 6|–2 W 15|+2 Ch 14|+2 4. Angler Worm 36. Ghoul, Imperial 69. Sandman Skills Percept +4, Stealth +4 5. Arboreal Grappler 37. Ghoul, Iron 70. Sap Demon 6. Aridni 38. Giant, Flab 71. Sarcophagus Slime Dmg Resist necrotic; nonmagic bludg/pierc/slash 7. Asanbosam 39. Giant, Thursir 72. Scorpion, Night weapons 8. Bagiennik 40. Gnoll Havoc & Stygian Fat-tail Dmg Imm poison 9. Bearfolk Runner 73. Selang Cond Imm charmed, exhaustion, frightened, poisoned 10. Bereginyas 41. Goat-man 74. Serpopard Senses darkvision 60', #14 11. Bouda 42. Harpy, Owl 75. Skitterhaunt 12. Cactid 43. Hound Of The 76. Spider, J'ba Fofi Languages knows ancient language, can’t speak 13. Carrion Beetle Night 77. Spire Walker Cursed Existence At 0 hp in desert terrain, its body 14. Cavelight Moss 44. Hulking Whelp 78. Subek disintegrates into sand & a sudden dry breeze. But 15. Dau 45. Imy-ut Ushabti 79. Swarm, Beetle unless killed in a hallowed location, w/radiant dmg, or 16. Death Butterfly 46. Jaculus Prismatic Swarm & Greater 47. Kikimora 80. Swarm, Scarab by a blessed creature, it reforms at next sundown 17. Deep One & Deep 48. Kongamato Manabane 1d100 miles away in a random direction. One Hybrid Priest 49. Lich Hound 81. -
Korean Direct
AAC Publications Korean Direct The First Ascent Of Gasherbrum V Insignificant against the blinding white backdrop of Gasherbrum V’s south face, we stood like silhouettes atop a moraine, the wall before us in full view. The complex glacier leading up to the face reminded me of scaly dragon’s tail. We had spotted a snaking line that would lead us to the jagged bergschrund at the foot of the wall. Once on the face, we would have to keep left to avoid a menacing serac, then move right in the upper mixed section before finishing with a direct line to the top. Seong Nak-jong and I had never really considered a route on the south side of unclimbed Gasherbrum V until we were denied passage up the northeast face. We had started our first attempt on the 7,147- meter peak from Camp 1 on the South Gasherbrum Glacier, along the normal routes to Gasherbrums I and II. We trudged through thigh-deep snow to reach the northeast face, which was covered in loose ice and snow, and was nearly impossible to protect. Falling ice and spindrift poured down from above. We finally had no choice but to evacuate from our high point of 6,400 meters. This unsuccessful attempt quashed our desire to climb. As the leader of our small team, the quandaries of a second attempt weighed heavily on my mind. Not only were we physically weakened and our confidence shot, it was already mid-July and more snow was laying siege to the camps. We had been away from home for more than a month. -
Reconciling Drivers of Seasonal Terminus Advance and Retreat at 13
Journal of Geophysical Research: Earth Surface RESEARCH ARTICLE Reconciling Drivers of Seasonal Terminus Advance 10.1029/2018JF004628 and Retreat at 13 Central West Greenland Key Points: Tidewater Glaciers • We evaluate the correlation of seasonal terminus advance/retreat to M. J. Fried1,2 , G. A. Catania1,2 , L. A. Stearns3 , D. A. Sutherland4 , T. C. Bartholomaus5 , glacial runoff, ice mélange, and 6 6 ocean temperature E. Shroyer , and J. Nash • Runoff is the strongest predictor at 1 2 glaciers that calve via serac failures Institute for Geophysics, University of Texas at Austin, Austin, TX, USA, Department of Geosciences, University of Texas at where subglacial melt plumes locally Austin, Austin, TX, USA, 3Department of Geology, University of Kansas, Lawrence, KS, USA, 4Department of Earth Sciences, enhance retreat University of Oregon, Eugene, OR, USA, 5Department of Geology, University of Idaho, Moscow, ID, USA, 6College of Earth, • Glaciers with sporadic, Ocean, and Atmospheric Sciences, Oregon State University, Corvallis, OR, USA buoyancy-induced full-thickness calving and the largest ice fluxes are less sensitive to environmental forcings Abstract The majority of Greenland tidewater glaciers undergo a seasonal cycle in terminus position, characterized by wintertime advance and summertime retreat. Understanding mechanisms that control seasonal cycles can help elucidate how tidewater glaciers regulate dynamic ice loss on longer timescales. Supporting Information: • Supporting Information S1 However, controls on terminus position are numerous and complex. To address this, we compare time series • Movie S1 of satellite-derived terminus positions for tidewater glaciers in central west Greenland with observations of • Movie S2 environmental forcings, including runoff at the grounding line, mélange presence, and, where available, • Movie S3 ocean temperature in the proglacial fjord. -
Energy and Air Pollution
Copyright © 2006, United Nations Environment Programme ISBN: 92-807-2668-4 UNEP/GCSS.IX/INF/2 UNEP Job No. DEW/0773/NA Disclaimers The content and views expressed in this publication do not necessarily reflect the views or policies of the contributory organizations or the United Nations Environment Programme (UNEP) and neither do they imply any endorsement. The designations employed and the presentation of material in this publication do not imply the expression of any opinion whatsoever on the part of UNEP concerning the legal status of any country, territory or city or its authorities, or concerning the delimitation of its frontiers and boundaries. Mention of a commercial company or product in this publication does not imply the endorsement of UNEP. © Maps, photos and illustrations as specified. Reproduction This publication may be reproduced in whole or in part and in any form for educational or non-profit purposes without special permission from the copyright holder, provided acknowledgement of the source is made. UNEP would appreciate receiving a copy of any publication that uses this publication as a source. No use of this publication may be made for resale or any other commercial purpose whatsoever without prior permission in writing from UNEP. Applications for such permission, with a statement of purpose and intent of the reproduction, should be addressed to the Division of Communications and Public Information (DCPI), UNEP, P.O. Box 30552, Nairobi 00100, Kenya. The use of information from this publication concerning proprietary products for publicity or advertising is not permitted. Produced by Division of Early Warning and Assessment (DEWA) United Nations Environment Programme P.O. -
1976 Bicentennial Mckinley South Buttress Expedition
THE MOUNTAINEER • Cover:Mowich Glacier Art Wolfe The Mountaineer EDITORIAL COMMITTEE Verna Ness, Editor; Herb Belanger, Don Brooks, Garth Ferber. Trudi Ferber, Bill French, Jr., Christa Lewis, Mariann Schmitt, Paul Seeman, Loretta Slater, Roseanne Stukel, Mary Jane Ware. Writing, graphics and photographs should be submitted to the Annual Editor, The Mountaineer, at the address below, before January 15, 1978 for consideration. Photographs should be black and white prints, at least 5 x 7 inches, with caption and photo grapher's name on back. Manuscripts should be typed double· spaced, with at least 1 Y:z inch margins, and include writer's name, address and phone number. Graphics should have caption and artist's name on back. Manuscripts cannot be returned. Properly identified photographs and graphics will be returnedabout June. Copyright © 1977, The Mountaineers. Entered as second·class matter April8, 1922, at Post Office, Seattle, Washington, under the act of March 3, 1879. Published monthly, except July, when semi-monthly, by The Mountaineers, 719 Pike Street,Seattle, Washington 98101. Subscription price, monthly bulletin and annual, $6.00 per year. ISBN 0-916890-52-X 2 THE MOUNTAINEERS PURPOSES To explore and study the mountains, forests, and watercourses of the Northwest; To gather into permanentform the history and tra ditions of thisregion; To preserve by the encouragement of protective legislation or otherwise the natural beauty of NorthwestAmerica; To make expeditions into these regions in fulfill ment of the above purposes; To encourage a spirit of good fellowship among all loversof outdoor life. 0 � . �·' ' :···_I·:_ Red Heather ' J BJ. Packard 3 The Mountaineer At FerryBasin B. -
Glaciers of Grandes Jorasses: an Open-Air Laboratory for Glacier Monitoring Systems Development
EGU2020-9814 https://doi.org/10.5194/egusphere-egu2020-9814 EGU General Assembly 2020 © Author(s) 2021. This work is distributed under the Creative Commons Attribution 4.0 License. Glaciers of Grandes Jorasses: an open-air laboratory for glacier monitoring systems development Niccolò Dematteis1, Daniele Giordan1, and Fabrizio Troilo2 1Research Institute for Geo-Hydrological Protection, National Reasearch Council of Italy, Torino, Italy ([email protected]) 2Safe Mountain Foundation, Courmayeur, Italy Glaciological phenomena can have a strong impact on human activities in terms of hazards and freshwater supply. Therefore, a scientific observation is fundamental to investigate their current state and recent evolution. To this aim, experimenting innovative scientific survey methodologies and equipment is of primary importance. Strong efforts in this field have been spent in the glacial complex of the Grandes Jorasses massif (Mont Blanc area), where several ice break-offs glacial outburst triggered from the Planpincieux Glacier snout and the Whymper Serac and threatened the underling Planpincieux valley in the past. From 2009, the glacial complex has become an open filed laboratory where a wide set of close-range remote sensing survey systems have been developed and applied to investigate the glacial state and dynamics. Two continuous monoscopic time-lapse cameras observe the Planpincieux Glacier since 2013. Digital image correlation is applied to the photographs to measure the surface kinematics at different level of detail. During the monitoring, image analysis techniques allowed at classifying the instability processes of the terminus and at estimating the volume of the break-off events. Such investigation revealed the presence of possible break-off precursors and a monotonic relationship between glacier velocity and break-off volume, which might help for risk evaluation. -
T He M C N Eill
T he M cN eill-N ott M emorial R oute A new line on the south face of Mt. Foraker. W il l M ayo as the sky falling? The serac had avalanched with a vicious cacophony. The moment was surreal: the mind trying to recognize the cause of the roar, the delay between sight and sound too difficult for the brain to assimilate immediately. We had Wdescended merely hours before, and now we watched a serac pummel our route, filling the entire cirque at the base of Mt. Foraker’s south face with a cloud of powder blown up by debris. Thirty minutes earlier, Max and I had stood chatting with Karen McNeill and Sue Nott at the very spot where the debris had landed. After the cloud subsided, we could once again see Karen and Sue, unharmed, two dots at the bergschrund at the base of the Infinite Spur. After much swearing and exclamation, and then silence, we continued up to the shoulder, headed back to base camp. It was 8 a.m. on May 14, 2006. Maxime and I rested on the shoulder for over an hour. I sat in the blazing sun, nause ated by the irony of our mad descent in fear of a storm that hadn’t yet materialized, only to barely miss being pulverized by a serac avalanche. I was relieved to be safely off the south face; I felt like we had made the wrong decision; Maxime was disappointed, saying it was like the “Magnificent Failure.” I apologized—we had descended due to my ambivalence about the weather. -
Various Expeditions
• 322 Various Expeditions. party to a small saddle on the subsidiary ridge, which was crossed at this point into the head of an easy, grassy gully. Ascending this they shortly reached the long summit ridge. Turning now to the left, a short rocky wall of some difficulty led the party to easy, grassy slopes which led up the summit in about 5! hrs. from camp. A cairn was built, as no traces of a previous ascent could be found. The height of the peak is estimated at approximately 9900 ft., and that of the main' berg' in its vicinity would appear to vary between 9000 and 11,000 ft. Owing to the position of the peak between Mont aux Sources including the Towers and the Sentinel on the one hand, and the peaks to the S.E. on the other it possesses a unique view in both directions, including Cathkin, Champagne Castle, the Saddle, as well as the Cathedral, the 'M weni Needles and Rockeries, whilst beyond the main Drakensberg ridge, which · falls away from the Sentinel, the higher peaks of the Maluti range are also visible. The party was confident that there was no other route of ascent. After a joyous half-hour spent on the summit the descent of the actual peak was accomplished by the route of ascent. From this point a more direct route than that taken during the ascent was followed to camp, the latter being reached at nightfall, in about 3! hrs. from the time of leaving the summit. 0. K. W. VARIOUS• EXPEDITIONS . -
A Collection of First Tier Creatures from Heraldry and Beyond
Ye Olde Physiologus A Collection of First Tier Creatures from Heraldry and Beyond DUNGEONS & DRAGONS, D&D, Wizards of the Coast, Forgotten Realms, the dragon ampersand, Player’s Handbook, Monster Manual, Dungeon Master’s Guide, D&D Adventurers League, all other Wizards of the Coast product names, and their respective logos are trademarks of Wizards of the Coast in the USA and other countries. All characters and their Sampledistinctive likenesses are property of Wizards of the Coast. This material is protected underfile the copyright laws of the United States of America. Any reproduction or unauthorized use of the material or artwork contained herein is prohibited without the express written permission of Wizards of the Coast. ©2016 Wizards of the Coast LLC, PO Box 707, Renton, WA 98057-0707, USA. Manufactured by Hasbro SA, Rue Emile-Boéchat 31, 2800 Delémont, CH. Represented by Hasbro Europe, 4 The Square, Stockley Park, Uxbridge, Middlesex, UB11 1ET, UK. Ye Olde Physiologus Author: K. David Ladage Alphyn......................................................5 Hellion....................................................21 Amphisbaena............................................6 Kopoacinth..............................................22 Antalope....................................................7 Lava Bear................................................23 Bonnacon..................................................8 Leucrocotta.............................................23 Boreyne.....................................................9 Mahr.......................................................24 -
Mt. Everest Not Safe from Climate Change 15 June 2015, by Christine Evans, Earth Institute, Columbia University
Mt. Everest not safe from climate change 15 June 2015, by Christine Evans, Earth Institute, Columbia University The Khumbu Icefall can move up to six feet a day, making this half-mile stretch one of the most treacherous of the climb. One veteran guide recently told the Associated Press, "If it wasn't the tallest mountain in the world, you would never put yourself on a glacier this active." The number of climbers on Everest has skyrocketed in recent years, and improvements in weather forecasting have made it all the more dangerous when bottlenecks of climbers attempting to summit in favorable conditions occur. A widely circulated photo by German mountaineer Ralf The north face of Mount Everest, as seen From Bhutan. Dujmovits shows hundreds of people following the Credit: Wikimedia Creative Commons same rope line up the mountain in 2012. A year later, mountaineers reported waiting two and a half hours to summit due to crowding and inexperienced climbers. One day in 2012 saw 234 climbers The last two years have witnessed the two summit, while in 1983, the highest daily number deadliest disasters in Everest climbing history, and was 8. As recently as 2009 it was barely over 100. many say climate change is to blame. On the whole, climbing Everest has become much Earlier this year, two earthquakes hit Nepal within more safe, but anecdotal evidence suggests that weeks of each other, first on April 25 and another the mountains are changing, and rapidly, becoming on May 12. The first earthquake triggered several less packed with snow and ice and experiencing avalanches on Mount Everest, resulting in at least more volatile conditions. -
Table of Contents
.........................................Table Of Contents............................................................... 0. About Dominions KB (Knowledge Base) <URL:#tn=0. About Dominions KB (Knowledge Base)> 0.1 Author <URL:#tn= 0.1 Author> 0.2 Description <URL:#tn= 0.2 Description> 0.3 Credits <URL:#tn= 0.3 Credits> 0.4 Version <URL:#tn= 0.4 Version> 1. Best tricks learned from MP games <URL:#tn=1. Best tricks learned from MP games> 1.1 Sneaky snipers <URL:#tn= 1.1 Sneaky snipers> 1.2 Wrathers <URL:#tn= 1.2 Wrathers> 1.3 Rain of stones <URL:#tn= 1.3 Rain of stones> 1.4 Black servant sneakers <URL:#tn= 1.4 Black servant sneakers> 1.5 Get upkeep free undead commanders <URL:#tn= 1.5 Get upkeep free undead commanders> 1.6 Beware the visiting heroes <URL:#tn= 1.6 Beware the visiting heroes> 2. Buffs in dominions III <URL:#tn=2. Buffs in dominions III> 2.1 (F)ire <URL:#tn= 2.1 (F)ire> 2.2 (A)ir <URL:#tn= 2.2 (A)ir> 2.3 (W)ater <URL:#tn= 2.3 (W)ater> 2.4 (E)arth <URL:#tn= 2.4 (E)arth> 2.5 A(S)tral <URL:#tn= 2.5 A(S)tral> 2.6 (D)eath <URL:#tn= 2.6 (D)eath> 2.7 (N)ature, <URL:#tn= 2.7 (N)ature,> 2.8 (B)lood <URL:#tn= 2.8 (B)lood> 3. Lessons learned from MP games <URL:#tn=3. Lessons learned from MP games> 3.1 Research <URL:#tn= 3.1 Research> 3.2 Raiding <URL:#tn= 3.2 Raiding> 3.3 Blood <URL:#tn= 3.3 Blood> 3.4 Assassination.