We took off to view Mt. Shasta as close as possible. It reaches the height of 14,179’ and is by
far the youngest geologic feature in the area.
It is volcanic, forming in episodes beginning 530,000 years ago and last
erupting in 1786. It is now considered
dormant. It is figured that it will
become active again in the future. It
was very devoid of snow.
We then checked out the City of Mt. Shasta. We lucked out as it was their afternoon to
have a Farmer’s Market. We made
purchases there, walked around downtown and then headed back to the campground.
Sleeping until almost nine o’clock we showered and
dressed and went to the #1 restaurant in Dunsmuir only to find that they are
closed on Tuesdays. Arriving at Yak’s, the
#2 restaurant we ordered our breakfasts.
We split French toast with Bailey’s Irish Cream and Bourbon as the
sauce. They are known for that!!!! Neither one of us really would ever order
that again. We split a tomato, bacon,
spinach omelet, which was good. Going
through the small town we decided we could never live in such a small town with
not much to do.
Our next destination was the Castle Crags. We drove up a single-lane curvy road with an edge that dropped straight down the mountain we climbed with the truck. From the parking area we hiked about a quarter mile with a 4% incline, to the view point. The crags are made of granite that cooled slowly deep with the earth. Over time this granite was uplifted and the rock above it worn away. Once the granite was exposed to the elements, water and ice have taken over as the main sculpting forces, breaking fractures in the rock, creating the castle-like features.
|
No comments:
Post a Comment