Snowbird ski area to replace its aerial tram


New cabins with glass panels within the ground anticipated to hold passengers by June

(Rick Egan | The Salt Lake Tribune) A tram filled with sightseers head to the highest of the mountain, as skiers head again down, on the final ski day of the season, at Snowbird Ski resort, Thursday, July 4, 2019. The resort plans to interchange the tram automobiles and drive system this summer season.

The barrels shipped from Switzerland bore the label “Cable Grease.” And their contents seemingly did assist easy the constructing of Snowbird Resort’s huge aerial tram through the spring and fall of 1971 — when a collection of unseasonable blizzards beleaguered Little Cottonwood Canyon, together with a Halloween dumping of 8.5 inches.

However due to perseverance and loads of schnapps — the precise contents of these barrels, in accordance with Walt McConnell’s e-book “The Snowbird Tram” — the resort’s iconic blue and crimson carriages made their maiden voyage on Dec. 23, 1971.

Because the resort celebrates its fiftieth season, nevertheless, the time has come for the tram to get replaced. Snowbird introduced Tuesday it has ordered a brand new drive system and carriages from The Doppelmayr Group in Switzerland. The outdated automobiles will make their final journeys between the bottom and Hidden Peak on April 3 and the brand new ones are anticipated to be prepared to hold passengers by the beginning of the summer season season in late June.

“The Tram and Snowbird have supplied year-round pleasure for 5 a long time,” resort basic supervisor Dave Fields mentioned in a press launch, “however the brand new tram cabins promise to take this pleasure to an entire new degree.”

The tram carriages have traveled almost 800,000 miles — sufficient to permit it to go to the moon and again 1.5 instances. And although Snowbird changed all 4 observe ropes in 2016, the expertise had superior such that it was time to interchange it, resort spokesperson Sarah Sherman mentioned.

“The present trams are 50 years outdated. We completely love them, they’re a traditional, but it surely was time for an improve,” Sherman mentioned. “Even trying on the management system and the way they drive the tram, there’s simply been a lot up to now 50 years that has modified and been upgraded that we felt it was time to actually embrace the newer expertise, not just for this upcoming season however for the following 50 years.”

Some perks include the upgrades.

In the summertime, the 2 automobiles — certainly one of which can nonetheless be crimson and the opposite blue — could have glass ground panels, permitting passengers to see the surroundings instantly under them. Every of the three panels measure 3 toes by 3 toes and will probably be positioned in a single part of the tram. So, there will probably be protected areas for individuals who are squeamish concerning the thought of seeing the treetops cross far under their toes.

For these wanting a fair much less obstructed view, nevertheless, another choice exists. The brand new automobiles will probably be outfitted with a 15-person open-air balcony that may be accessed within the summers for an extra payment. Sherman mentioned it’s the solely open-air tram balcony within the U.S.

“We’re actually, actually excited to have this,” she mentioned, “and let individuals arise there on the summer season days and see the 360-degree views of Mount Superior and Salt Lake and take every little thing in.”

Neither choice is obtainable within the winter, when the automobiles will return to delivering skiers and snowboarders to the snow 2,900 toes up the mountain. The outdated cabins carried a most of 125 passengers, essentially the most of any aerial tram in the USA as of 2016, in accordance with liftblog.com. Sherman mentioned the uphill capability, which the resort usually limits to 100, and the velocity, about 10 minutes per journey, won’t change.

Some alterations will probably be made to the tram automobile docks. Sherman mentioned she shouldn’t be conscious of any further modifications that can should be made to the constructing that housed the just lately closed Tram Membership, a bar positioned underneath the tram’s loading station and in view of its bull wheels, and different adjoining buildings. The Tram Membership is already present process renovations and its standing needs to be up to date “quickly,” Sherman mentioned.

Whereas it hopes to have the brand new tram up and working by mid-June for its summer season season, that doesn’t imply it will likely be closed for snowboarding by then. Snowbird is historically one of many final ski areas within the nation to shut, typically staying open into July. Sherman mentioned the resort will attempt to discover methods to maintain the areas historically accessed by the tram open nicely previous April 3 utilizing their Peruvian, Little Cloud and Mineral Basin lifts.

So what’s going to turn into of the 2 tram automobiles as soon as they’re retired?

“That’s the million greenback query,” Sherman mentioned. “And the not thrilling reply is: We don’t know but. We need to do one thing actually cool with them. We need to proceed to honor them.”

The 200 gallons of schnapps that greased their set up says a bar is perhaps a great resolution.



New model may improve San Francisco Bay Area, U.S., seismic hazard maps — ScienceDaily


The Santa Cruz Mountains outline the geography of the Bay Space south of San Francisco, defending the peninsula from the Pacific Ocean’s chilly marine layer and forming the area’s infamous microclimates. The vary additionally represents the perils of dwelling in Silicon Valley: earthquakes alongside the San Andreas fault.

In bursts that final seconds to minutes, earthquakes have moved the area’s floor meters at a time. However researchers have by no means been in a position to reconcile the fast launch of the Earth’s stress and the bending of the Earth’s crust over years with the formation of mountain ranges over thousands and thousands of years. Now, by combining geological, geophysical, geochemical and satellite tv for pc knowledge, geologists have created a 3D tectonic mannequin that resolves these timescales.

The analysis, which seems in Science Advances Feb. 25, reveals that extra mountain constructing occurs within the interval between giant earthquakes alongside the San Andreas Fault, quite than throughout the quakes themselves. The findings could also be used to enhance native seismic hazard maps.

“This mission targeted on linking floor motions related to earthquakes with the uplift of mountain ranges over thousands and thousands of years to color a full image of what the hazard may truly appear to be within the Bay Space,” mentioned lead research creator Curtis Baden, a PhD pupil in geological sciences at Stanford College’s College of Earth, Vitality & Environmental Sciences (Stanford Earth).

Bending and breaking

Geologists estimate the Santa Cruz Mountains began to uplift from sea stage about 4 million years in the past, forming as the results of compression round a bend within the San Andreas fault. The fault marks the boundary between the Pacific Plate and the North American Plate, which shift previous one another horizontally in a strike-slip movement.

Measurements of deformation — adjustments within the shapes of the rocks — have proven that Earth’s floor warps and stretches across the San Andreas fault throughout and in between earthquakes, and behaves very similar to an elastic band over seconds, years and even a long time. However that basic method can’t align with geologic observational knowledge as a result of it would not enable the rocks to yield or break from the stress of the warping and stretching, as they finally would in nature — an impact that has been noticed in Earth’s mountain ranges.

“For those who attempt to deal with the Earth like an elastic band and drive it ahead too far, you are going to exceed its power and it isn’t going to behave like an elastic anymore — it may begin to yield, it may begin to break,” mentioned senior research creator George Hilley, a professor of geological sciences at Stanford Earth. “That impact of breaking is widespread to nearly each plate boundary, however it’s seldom addressed in a constant manner that permits you to get from earthquakes to the long-term results.”

By merely permitting the rocks to interrupt of their mannequin, the research authors have illuminated how earthquake-related floor motions and floor motions in between earthquakes construct mountains over thousands and thousands of years. The outcomes had been stunning: Whereas the geosciences neighborhood conceives of earthquakes as the first drivers of mountain-building processes, the simulation confirmed most uplift has occurred within the interval between earthquakes.

“The traditional knowledge is that everlasting uplift of the rock truly occurs as the results of the immense pressure of the earthquake,” Hilley mentioned. “This argues that the earthquake itself is definitely relieving the stress that’s constructed up, to some extent.”

A neighborhood laboratory

As a result of the Santa Cruz Mountains neighbor a number of analysis establishments, together with Stanford, the College of California, Berkeley, and the USA Geological Survey (USGS), scientists have gathered an immense quantity of details about the mountain vary over the course of greater than 100 years.

Efforts to gather geological and geophysical knowledge had been particularly spurred by main current occasions just like the 1989 Loma Prieta earthquake and the 1906 San Francisco earthquake, however the formation of the Santa Cruz Mountains seemingly spanned a whole lot of hundreds of smaller earthquakes over thousands and thousands of years, in accordance with the researchers.

The research authors compiled the prevailing suite of observations, and in addition collected new geochemical knowledge by measuring Helium gasoline trapped inside crystals contained in rocks of the mountains to estimate how briskly these rocks are coming to the floor from hundreds of toes beneath. They then in contrast these datasets with mannequin predictions to determine how earthquakes relate to uplift and erosion of the mountain vary. The method took years of specifying materials properties to mirror the complexity that nature requires.

Seismic implications

The researchers ran their simulation from when the Santa Cruz Mountains began to uplift 4 million years in the past till current day to grasp how the evolution of topography close to the San Andreas fault by means of time influences current and potential future earthquakes.

“At present, seismic hazard assessments within the San Francisco Bay space are largely primarily based on the timing of earthquakes spanning the previous few hundred years and up to date crustal motions,” Baden mentioned. “This work exhibits that cautious geologic research, which measure mountain-building processes over for much longer timescales than particular person earthquakes, also can inform these assessments.”

The scientists are at present engaged on a companion paper detailing how hazard threat maps could possibly be improved utilizing this new mannequin.

“We now have a manner ahead when it comes to truly having a viable set of mechanisms for explaining the variations between estimates at completely different time scales,” Hilley mentioned. “The extra we will get all the pieces to suit collectively, the extra defensible our hazard assessments might be.”

Examine co-authors embody David Shuster and Roland Bürgmann of UC Berkeley; Felipe Aron of the Analysis Heart for Built-in Catastrophe Threat Administration (CIGIDEN) and Pontificia Universidad Cato?lica de Chile; and Julie Fosdick of the College of Connecticut. Aron and Fosdick had been affiliated with Stanford once they performed analysis for the research.

This research was supported by NSF Profession Grant EAR-TECT-1108 105581, Fondo de Financiamiento de Centros de Investigación en Áreas Prioritarias ANID/FONDAP/15110017-Chile (CIGIDEN) and the Ann and Gordon Getty Basis.