Entrance Stations Now Accept Credit Cards
Visitors coming to Yosemite National Park will now have another means to pay for entrance into the park.
Previously, visitors had to pay the $20 entrance fee by cash or check. Yosemite National Park management recognized that providing another option to cover the entrance fee would be a beneficial service for park visitors. With the availability of other payment methods, many travelers today carry very little money. The option to pay by credit card provides additional flexibility to visitors to the park.
Visa, MasterCard, American Express, Discover, and Diners Club cards have been accepted at park entrance stations since December 10.
"We are very excited to provide this service to visitors of the park," said Mike Tollefson, Superintendent of Yosemite National Park. "It gives them a choice and helps make their trip planning simpler."
Tuolumne Meadows in Winter: Population 2
Have you ever wondered what it would be like to spend a winter snowed in at 8,600 feet in Yosemite’s high country, with the nearest plowed road 15 miles to the east?
When the Tioga Road closes in late fall, winter rangers Bruce & Tracey Wiese get busy! They assist cross-country skiers, observe wildlife activity, regularly assess avalanche conditions, survey the Sierra snow pack, and when needed, assist in search & rescues. They get around only on cross-country skis and can log up to 1,000 miles in a season!
Periodically, the winter rangers send in reports from their Tuolumne Meadows base. What follows is their latest installment.
Report from Tuolumne Meadows
December 19, 2003
WEATHER/SNOW (from Dec. 11 to Dec. 18)
High temp: 59 (Dec. 18)
Low temp: -10 (Dec. 15)
New Snow: 19” (Dec. 11, 12, 13, 15)
Total settled snow depth: 24” (Dec. 19)
We have been enjoying an abundance of maritime powder, which has gotten heavier the last few warm days. The snow level on the east side is near the gate at 7,000’ a few miles from Lee Vining.
AVALANCHE/SNOW CONDITIONS (above 8,000’)
Avalanche potential is generally Moderate with higher potential on granite domes and steep rock slabs.
We noticed that a few small avalanches had occurred early in the week, mostly involving last Sunday morning’s new snowfall. Sunday’s storm had strong SW winds and several slides had started from wind deposited snow off of steep rocky starting zones. We have also seen evidence in some steeper, rocky areas of other small slides, which appear to be sloughing after every storm exposing the gray colored old, November snow surface.
Our snow pit tests on Unicorn Peak (near last week’s test area) showed weaknesses about 6” down (bottom of freshest snow) and another weakness several feet down on top of the old November ice crust. Both a stuffblock test (dropping a ten-pound bag on an isolated shovel size snow column) and a rutschblock test showed moderate instabilities at both these depths. The bottom layer of faceted snow had been somewhat compressed and generally more compacted than a week ago. The overlying snow may have helped compact this layer, but having facets at this depth is always a red flag, one we will have to consider throughout this winter.
Flying Squirrels? Actually they are “falling squirrels.” After a new snowfall we’ve noticed that chickarees (also known as Douglas squirrels) will jump from branches—sometimes 10’-20’ high—into the snow, then “swim” their way through the snow looking like wound-up rubber band toys with much effort and little forward motion. Then they will climb another tree and launch again. Actually it is a good strategy for newly fallen snow and appears to have a strong element of fun.
Although flying squirrels live in the Sierra, it is not common to see these much more secretive critters. But we see a fair amount of falling squirrels and even more of their tracks. One day just as a snow storm had subsided and the trees were falling with squirrels, we saw a goshawk perched in a tree next to the Tioga Road; it looked like a good time and place to catch a meal as it floundered in the snow trying to cross the open road.
The falling squirrel prints look similar to snowball impressions in the snow, since their landing is in a tight four-point stance. While working one winter in Glacier National Park, we would use a much more revealing impression left by pine martens and fishers when they leaped from a tree, indicating body length and width, even head and tail impressions in favorable conditions. The dimensions would often help determine which species made the track.
Note: The Tuolumne Meadows Winter Conditions Update is posted every week at https://www.nps.gov/yose/now/tm.htm.