Avalanche Defensemen Erik Johnson on Life Without His Three Front Teeth

Avalanche Defensemen Erik Johnson on Life Without His Three Front Teeth

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“You would think it’s the opposite”: The average age of fatal avalanche victims is on the rise

Sidney Crosby will miss at least one more Pittsburgh Penguins but the return date is growing closer. Crosby has yet to face contact in practice and so Sunday is also looking shaky, but the Penguins have an astonishing record in the 26 games that Crosby missed due to injury this season. Those 16 wins are tied for fourth in the NHL.

Sullivan indicated Crosby was scheduled to practice on Tuesday but coaches delayed the timeline as best for the team. The Penguins will conclude their season series with Colorado as they play the middle game of their current three-game road trip. Earlier this season, the Penguins took down Colorado, , in overtime when Brandon Tanev scored a shorthanded goal.

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Eckert, N. Baya, and M. Snow avalanches are natural hazards strongly controlled by the mountain winter climate, but their recent response to climate change has thus far been poorly documented. In this paper, hierarchical modeling is used to obtain robust indexes of the annual fluctuations of runout altitudes. The proposed model includes a possible level shift, and distinguishes common large-scale signals in both mean- and high-magnitude events from the interannual variability.

Application to the data available in France over the last 61 winters shows that the mean runout altitude is not different now than it was 60 yr ago, but that snow avalanches have been retreating since This trend is of particular note for high-magnitude events, which have seen their probability rates halved, a crucial result in terms of hazard assessment.

Avalanche control measures, observation errors, and model limitations are insufficient explanations for these trends. On the other hand, strong similarities in the pattern of behavior of the proposed runout indexes and several climate datasets are shown, as well as a consistent evolution of the preferred flow regime.

The proposed runout indexes may therefore be usable as indicators of climate change at high altitudes. Recent changes in snow precipitation patterns and snow cover regimes have been investigated in depth e. These changes challenge the assumption of the stationarity of snow avalanche activity Paul ; Seiler , which is defined by McClung b as the stationarity of the weather conditions that generate snow stability.

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Nathan MacKinnon and Seth Jones. Jonathan Drouin and Aleksander Barkov. They are the top candidates to go first Sunday at the Prudential Center. Colorado won the draft lottery and has flirted with the idea of picking a puck-moving defenseman in Jones. But it appears the Avalanche are leaning toward choosing a forward, perhaps the year-old MacKinnon.

This article deals with recent avalanche events dated by the dendrogeomorphic method and their verification. The research was focused on two active.

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Recode Daily: Amazon’s Alexa avalanche

Noel Potter, Jr. Schumm, William C. Tree-ring dating in several avalanche tracks in Galena Creek valley, northern Absaroka Mountains, Wyoming, is used to determine the frequency of large snow avalanches that pass below the forest line. The following criteria are used: 1 datable scars on the trees, 2 changes in growth-ring pattern from concentric to eccentric, caused by tilting, 3 changes in growth rate due to increase in photosynthesis when adjacent trees are destroyed, and 4 age of trees within a given reforested avalanche track.

The first two of these criteria are most reliable. Many young trees within the avalanche tracks are protected by snow during avalanches, and they thus survive to reforest the track immediately following destruction of the larger trees.

Moderate-large earthquakes usually trigger a large number of landslides. The prehistoric large landslides can be analyzed to determine the.

The Center for Snow and Avalanche Studies serves the international mountain science community and regional water resource managers by hosting and conducting mountain system research and collecting integrative, real time, year-round mountain system observations. Mountain system research includes monitoring regional climate trends influential to snow melt, remote sensing of snowpack, snow and ice microstructure, and The Colorado Dust on Snow Program. Data includes information about weather, snowpack, radiation, soil, and hydrologic signals.

By incorporating this research and information we are able to contribute to the understanding of water resource availability, from mountain snow, on a regional and global scale. CSAS does not forecast for avalanche hazard nor do we provide avalanche instruction. However, our resources and research do support avalanche science, forecasting, and education. Researching snow microstructure, and impacts of dust on snow, is valuable for the science of slab and weak layer formation.

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Large rock-slope failures are among the primary geohazards in high mountain areas. This study focuses on the formation and geomorphological activity of the Akdag landslide complex located on the southern slope of Mount Akdag, SW Turkey. We employed detailed mapping in the field, spatial and morphometric analysis using GIS and remote sensing technologies, and surface exposure dating with cosmogenic 36 Cl to reconstruct the chronology of the landslide complex.

For the analysis of cosmogenic 36 Cl, we collected 18 surface samples from calcareous boulders within the landslide deposit. Our field mapping shows that the Akdag rock avalanche is a large and active slope failure developed between carbonates and flysch. The rock-avalanche deposits cover an area of 9.

Nobody in the history of dating has ever screwed up THIS badly A man at a Colorado Avalanche game elbowed his girlfriend in the head.

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Colorado Avalanche

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Trees are most often used as subjects for study but there are some possibilities for using shrubs to date events over short intervals. The methodology of ring-dating is based on the growth behavior of woody plants in cold and temperate climates with marked differences between summer and winter temperature regimes. The winter conditions cause the plants to slow or stop their growth so that there is a discernible difference between the cell size and structure at the end of a growing season compared with that at the beginning of a new growing season.

The numbers of rings in cross-sections of selected stems can provide a means of dating and reconstructing events of the past such as glacier fluctuations Lawrence , Sigafoos and Hendricks , timberline changes La Marche and Mooney , lake level fluctuations Cameron , Lawrence , landslides Heath , , floods Grant , , fires Spurr , and other natural and man-made changes.

For the purposes of this handbook, the methodology will be referred to as tree-ring analysis, rather than dendrochronology. The latter term has come to be applied, more narrowly, to the somewhat more specialized methodology of use, for dating, cross-dating to extend chronologies and climatic analysis of sequences of wide and narrow growth layers in sensitive species in arid or cold climates Glock , Fritts , , Ferguson , Suess , La Marche and Fritts , Fritts and Blasing Nevertheless, both methodologies make much the same use of knowledge of the characteristics of tree growth and wood structures.

In certain rare circumstances, mentioned later, dendrochronological techniques might be applied to the dating of snow avalanches. Techniques most useful in tree ring analysis are described by Lawrence , Potter , and Stokes and Smiley

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In the Obernberg valley, the Eastern Alps, landforms recently interpreted as moraines are re-interpreted as rock avalanche deposits. For a wide altitude range the avalanche deposit is preserved, and the event age of mass-wasting precludes both runout over glacial ice and subsequent glacial overprint. The regularly arrayed transverse ridges thus were formed during freezing of the rock avalanche deposits.

Most rock avalanches post-dating the Last Glacial Maximum LGM in the Alps are readily recognized by their shape and size as well as by an extremely poorly sorted composition ranging from cataclastic gouge to megablocks Pollet and Schneider, ; Crosta et al. At a few locations, however, the interpretation of landforms composed of very poorly sorted deposits remains controversial. For instance, transverse and lateral ridges of rock avalanches may appear similar to terminal and lateral moraines of glaciers.

Using this process, they constructed an avalanche history dating back over years. “By doing this, we are sure that the frequency and.

Nathan MacKinnon had a goal and three assists before sitting out the third with an upper-body injury. Cale Makar and Ryan Graves each added a goal and two assists for the Avalanche, who snapped an eight-game home losing streak to Nashville dating back to Jan. Nashville led after Filip Forsberg and Matt Duchene scored in the first of the second period but Colorado took over with six goals in eight minutes. Donskoi and Graves scored 20 seconds apart and Andre Burakovsky got another later to make it and chase Predators goalie Pekka Rinne.

Rinne, who came into the game with a 2. Juuse Saros came on and allowed a short-handed goal to Matt Nieto 50 seconds later. Matt Calvert scored at and Donskoi’s second of the night at made it Craig Smith scored in the third period for Nashville, and Donskoi completed the hat trick with his eighth goal of the season at Pavel Francouz made 20 saves for the win in place of Philipp Grubauer. Colorado coach Jared Bednar said Grubauer will miss two games with a lower-body injury.

Makar scored his second of the season 50 seconds into the game. Ryan Ellis tied it midway through the first and MacKinnon got his ninth during a 5-on-3 power play late in the first. Colorado D Nikita Zadorov sat out the third period with an upper-body injury.

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N2 – A tongue of very coarse rockslide debris that extends 1. Calculations based on frictional considerations imply that the feature is an excess-runout rock avalanche sturzstrom deposit. The morphological characteristics of the deposit appear consistent with movement by grainflow or fragmental flow. Failure is inferred to reflect time-dependent paraglacial stress release and consequent propagation of an internal joint network. The late-Holocene age of failure implies persistence of the effects of paraglacial stress release over a time-scale of several millennia.

Abstract. Counts of tree rings were employed to date a major avalanche deposit. This technique required the evaluation of assumptions as to delays in seeding.

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Donskoi scores 3 goals as Avalanche beat Predators 9-4

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