At the start of the trail, some shelf-style fungi on a tree trunk:
Glacial boulders adorned the landscape - this one was specifically labeled as such:
A covered bridge over the Pemi.
A first glimpse of the Slide:
The surface was not worn smooth and flat, but smooth and rippled, as if from eons of waves:
Important warning for visitors:
In the Flume itself, an 800-foot long gorge formed where basalt dikes have worn away faster than the Conway granite, trees have sprung up in the (seemingly inhospitable) long horizontal cracks in the walls. It makes the roots look kind of espaliered:
And even some of the branches have a similarly artificial feeling:
It was slow going, as the boardwalk was clogged with people stopping for photos. (Unnecessarily, I might add, since the path is actually wide enough for a passing lane if only people would keep to the right when they are not moving!) A view up the Flume:
This natural archway to nowhere (it's very shallow) is labeled "The Pulpit":
The Avalanche Falls toward the top of the gorge were cool because the water kept ricocheting back and forth like a pinball machine:
As we exited at the top of the gorge, the temperature rose noticeably. The Flume must be great on a hot summer's day (natural air conditioning).
Unfortunately, in a crowd this large, it's inevitable that not everyone will actually obey the signs:
A picture postcard of tenacity - tree roots gripping a rock:
(I found myself wondering at times whether the trees maybe hoped to crush the rocks over time until they give forth all their nutrients - what a bonanza, if they pull it off! Cue the Far Side cartoon with a spider web strung across the bottom of a playground slide: "If we pull this off, we'll eat like kings!")
Here, the water flows down through an arch to create a second waterfall:
A nice NH mountain stream view:
A close-up of water rushing through rocks:
The Sentinel Pine Bridge takes visitors across to a prime viewing spot for the Pool. From the NHDPR website:
The Pool is a deep basin in the Pemigewasset River. It was formed at the end of the Ice Age, 14,000 years ago, by a silt-laden stream flowing from the glacier. The Pool is 40 feet (12m) deep and 150 feet (45m) in diameter, and is surrounded by cliffs 130 feet (39m) high. A cascade rushes into it over fragments of granite that have fallen from the cliffs above.
On the high cliff above the Pool, the Sentinel Pine stood for centuries. It was one of the largest in the state, nearly 175 feet (53m) high, with a circumference of 16 feet (4.8m). The hurricane of September, 1938 uprooted the giant pine whose trunk bridges the river above the Pool and forms the base for the covered bridge. The bridge offers a fine view of the Pool.
Was this the scene after the Ents smashed up Isengard?
As we soaked in a view of Mts. Liberty, Flume, and Osseo, occasional gusts of wind would fill the air with leaves, fluttering and even glinting as they caught the sun:
The top of Mt. Liberty (4460') is supposed to look like a profile of George Washington's face. Imagine that he is lying face up, and the top of his head on the right. It's really just the nose and a hint of the forehead. Kinda almost works:
I couldn't get enough of tree roots gripping rocks. There's something so compelling about the imagery. It really makes the trees look human - in a chilling, inhuman way. It's like fingers, or arms, or tentacles. Oooh, that gives me the shivers!
It was a lovely walk, very fun. We had some lunch outdoors (including birthday cake - thanks, Ruth!!!) and then prepared for Round II.
No comments:
Post a Comment