On April 24, Ben Kiessel (27), Chris Scharf (38) and Chris Lackey (39) landed on the Root Canal Glacier below the South Face of the Moose’s Tooth with the intention of climbing the “Ham and Eggs” route. On April 27, they had climbed up to the eighth pitch and turned around due to thin ice conditions. Upon returning to camp, they met two guides, Kevin Mahoney and Larry Cote, who had set up camp immediately next to theirs.
About 0115 on April 18, the climbers heard the crack of a serac wall collapsing and moments later were engulfed in the blast of an avalanche while in their
The rescue was not able to launch until 0650. By that time, Lackey had succumbed as a result of traumatic injuries.
Ice avalanches (serac falls) result from tensile failure within the ice due to ice flow (creep) within the ice mass and/or glide at the bed surface. It is inherently difficult to predict the timing of this type of failure. Unlike the situation with snow avalanches, there is very little correlation to time of day, aspect, elevation or weather. This leaves few tools available to the practitioner for use in the field. Avoidance and limiting the time of exposure
The run-out distance for an avalanche is the farthest point to which debris can reach. Currently, the best methods for determining runout distance are “...by long-term observations of avalanche deposits; (2) observations of damage to vegetation, ground or structures; or (3) searches of the historical record as preserved in newspapers, old aerial photos, or other written material” (McClung and Schaerer, 2006). Unfortunately very few of these are available for the mountains of the Alaska Range, so we must use other methods.
The debris from this event traveled 1,920 feet out from the point of impact on an average slope angle of six degrees. This is a substantial distance on a shallow slope angle, and thus it retained enough energy to hit the camp with impressive force. Similar to water, the main flow channel followed the path of least resistance. A subtle depression channeled the majority of the debris (up to feet deep) and deposited it directly through the area of the campsite.
Another significant terrain feature that contributed to this event is the nearly vertical avalanche path. The vertical fall of approximately 743 feet allowed for an almost “free fall” environment for the ice to travel, increasing the speed at which it fell. This appears to have created an explosive impact that broke ice into small pieces allowing them to travel greater distances, also resulting in a substantial air blast that traveled in front of the debris. The air blast hit with such force that it ejected all five climbers from their tents, hurling them into the air ahead of the debris, accounting for their position mostly above or shallowly buried in the debris.
The timing of large avalanche events are sometimes described in terms of “100-year events”, indicating that events this large only happen once every 100 years much like a 100-year flood. They are in effect rare events. This is a dangerous assumption in this case. The hanging glacier that produced this event is capable of producing a much larger one and this size event seems to happen on a more regular basis. Based on interviews, a Google Earth image that captured a similar debris zone and this event, it appears that the return period for this size event is much more frequent than 100 years. It may have a return period as frequent as every five to ten years or less.
An additional component was the guides’ decision to place their camps in this location. Historically, camps on the Root Canal have been used on both sides, up and down the entire airstrip. The approximate campsite location where the accident occurred is a popular area often used by many climbers each year for its view of the entire “Ham and Eggs” climbing route and proximity to plane access. Interviews indicate that there were previous campsites from this season in this location and none in other locations. Choosing camping locations in this area is difficult due to the large scale of terrain and multiple potential hazards (rockfall, snow avalanches, weather, and serac fall) that threaten the basin. At times one may trade one for the other, making decisions difficult, even for experienced guides.
Professionals often rely on experience to help guide their decision making process. However, experience-based decisions are not always flawless. Studies have shown that novices and professionals make decisions using “heuristics” or mental shortcuts (Tremper, 2008). These shortcuts allow for quick decisions during complex tasks and are based on limited information. Two heuristics that professionals are especially prone to are “social proof” and “familiarity” (McCammon, 2002). In this case the existing campsites and historical use of this area may fall into McCammon’s “social proof” category. “The social proof heuristic is the tendency to believe that a behavior is correct to the extent that other people are engaged in it” (McCammon, 2002). One of the two guides had also been to the area many times and camped in a similar location on seven previous trips without incident. His decision may fall into the “familiarity” category. “The familiarity heuristic is the tendency to believe that our behavior is correct to the extent that we have done it before” (McCammon, 2002). An additional heuristic that I will add is potentially a calibration problem regarding snow avalanches and ice avalanches resulting from the possible assumption that they behave like the same animal when they do not.
Complex terrain in the Alaska Range demands attention to detail every step of the way, and timing will always be a part of it. Using all of our tools to avoid and reduce exposure will help to reduce the risk but cannot take away all of the risk. The decision to camp in this location worked for many people for many seasons, but not this time. (Source: John Leonard, South District Ranger, and Peter Armington, Investigating Officer.)
(Editor’s Note: Request bibliography from Denali National Park.)