|
Leonard, John, and Java |
From Coffman Cove we made our way into
Ketchikan to await the arrival of John, our Nephew, who flew in to
spend a few days with us aboard Got d' Fever. We were
delighted to have his company and planned some fun excursions despite the
clouds and rain. We motored from
Ketchikan to Thorne Bay where we toured El Capitan Cave. Cave exploration or spelunking is definitely
not the first thing that comes to mind when you think of Alaska.
|
Steep Stairs to the Top |
There are actually 500 caves on Prince of
Wales Island, the largest being El Capitan with over two miles of passageways;
El Capitan was only recently discovered by loggers in the mid-1990’s.
We rented a car in Thorne Bay and drove to
the northern end of the Island where we met our U.S. Forest Service tour guides.
It became clear why these caves had not been
discovered earlier by modern man, a steep staircase of 370 steps have been constructed
by the Forest Service in order to reach the top of a cliff where the cave
entrance is found.
|
Cave Entrance |
With our hardhats and
headlamps, we moved into the darkness, squeezing between boulders and low
ceilings before entering into a large room, and then another, and another.
Our guide pointed out mineral deposits,
generally composed of calcium carbonate that dissolved from the surrounding
limestone by water.
|
Mineral Deposits |
The water’s capacity
to hold calcite is diminished when met with air in the cave and causes the
calcite to be deposited, creating various unique formations.
At one point in the tour, we turned off our
headlamps and stood still in the blackness, listening to the drip, drip, drip
of water that has taken place over thousands of years.
|
Walking through the Caves, El Capitan |
Millions of years ago, the cave was once a reef,
but now lies 360 feet above sea level, marine fossils have been found in
several places within El Capitan Cave.
Other
discoveries include the excavation of bear skeletons found in various passageways;
carbon dating indicates the bones to be over 11,000 years old suggesting that
the El Capitan valley was free of glacier ice at that time.
|
Karst Sinkhole/Shaft |
These discoveries have spawned more research
into the prehistory of the southern portion of Southeast Alaska.
On our drive back to Thorne Bay, we stopped
at Beaver Falls Interpretive Trail, a system of boardwalks through Karst formations.
Karst is a landform shaped by the dissolving
action of water on carbonate bedrock.
|
Karst Falls |
Karsts include features like spires and pinnacles above ground as well
as sinkholes, shafts, and disappearing streams and caves below ground which develop
over many thousands of years.
On our
walk, we saw sinkholes, shafts, and a waterfall all part of this karsk area.
It was a nice day’s outing despite the
pouring rain and we kept dry in our rain gear, the official uniform of Alaska.
|
Boardwalks through the Karst Area |
No comments:
Post a Comment