Grants Pass to Crescent City Highway 199 Road Guide -
Oregon & California Redwood Highway
Mantle Rock
ZERO ODOMETER at the driveway into Patrick Creek Lodge
0.0 Patrick Creek Lodge:
In this part of the tour you will be driving through an
exposure of rocks that were uplifted from the earth’s upper mantle.
This is the largest exposure of this type of rock in North America.
The poor nutrients in these rocks, along with the presence of chrome
and nickel, retards the growth of plants. Some plants such as the
California pitcher plant growing at mile 4.0 are adapted to growing
in these harsh regions. You saw
portions of these mantle rock exposures at Eight Dollar Mountain near
Selma and again at the Rough and Ready Forest State Park south of
Cave Junction, both of which were located in exposures that
paralleled Highway 199. In this area, this exposure of rocks turns
to the south and you are now going to be driving through them.
0.6 Turnout: Use turnouts to allow faster moving traffic to
pass.
1.6 Turnout
1.9 Bridge
2.0 Road becomes four lanes
2.3 Land slides are common in these mantle rock exposures
and you are likely to see a number of new and very old landslides
along the river through this area. Land slides provide good evidence
of the instability of mantle rock and the reason for this occurred
in the very early history of when these rocks were formed. In the
mantle, very little water is able to penetrate from the surface to
the mantle rock but as the rock is uplifted and still under high
pressure and temperatures, water begins to mingle with these rocks,
usually working its way through cracks. When water is added to
mantle rock, it changes to a type of rock called serpentine. One of
the common serpentine minerals is talc and this tends to make the
cracks in the rock slippery and prone to land slides. New land
slides have a white color. Older landslides appear to be more
brick-red in color caused by staining from the iron in the rock. The
older the landslide, the more reddish the rock. The process of serpentinization occurred only in the earliest history of these
rocks when they were under high pressure and temperature. Water from
rain does not appear to cause further development of serpentine.
2.7 Bridge
3.0 Grassy Flat Campground (left):
A section of the old highway and part of the old bridge
that was washed out in the 1964 flood can be seen by turning left
into Grassy Flat. The campground is closed in the winter but the
road is open to the old bridge.
3.4 Slide area - watch for rocks. Rocks often roll onto the
road from the cut on the right.
4.0 Botanical Trail (right):
This is a must-see stop for anyone driving through the
unusual mantle rock exposures of Smith River National Recreation
Area. The trail is
wheelchair accessible and has interpretive signs that tell you about
the botany and mining history in this area. The hallmark feature is
the colony of insectivorous pitcher plants, known in this area as
the Darlingtonia. They are well adapted to survive in the nutrient
poor soils of the mantle rock and are generally found growing around
springs and seeps in the mantle outcrops of this region
4.3 Slide area watch for rocks
4.7 The road to right is another small section of the old
highway. The bridge that crossed the river was washed out in the
1964 flood. There is a smaller bridge just before the cul-de-sac
that is one of the original bridges installed when Highway 199 was
constructed in 1922.
4.8 Bridge
5.2 Panther Flat Campground (right) has a day use area next to
the river that is open for public use. A day use fee can be paid at
the self-serve station near the campground entrance. Rocks from a
landslide have created a nice swimming hole at this location.
6.4 Lado Del Rio road on the right was the site of the
community of Darlingtonia, a town you may see shown on some maps.
There was a lodging facility located here.
5.4 French Hill:
The flat-topped hill in front of you is called French
Hill and was the site of gold mining in the 1800s. Gold was mined in
gravel beds of ancient rivers that are believed to have flowed over
a wide, flat region not much higher than sea level. The gravels of
French Hill were deposited on these flatlands about 30 million years
ago and since that time regional uplift raised the gravel beds, with
erosion carving out river canyons around them. This is a good
example of the uplift this entire region has experienced; bringing
rocks up from deep in the ground to the surface such as the roots of
the ancient volcano that was pointed out in the first part of the
tour at Grants Pass. You will see another terrace that has been
recently uplifted out of the sea when you get to the end of the tour
and drop down on to the flat lands of Crescent City and Tolowa Dunes
State Park. The picture above was taken from French Hill looking at
other hills in the area.
7.2 Four lane ends. Reduce your speed.
7.5 French Hill Trail and USFS Ranger Station:
The historic pack trail used by miners to bring supplies
from the Gasquet Store to the mines on French Hill is on the left.
Gasquet Ranger Station in on the right and has inside
and outside displays as well as books and maps pertaining to Smith
River National Recreation Area. The buildings and rock work at this
station were constructed by crews at the Gasquet Civilian
Conservation Corps (CCC) camp in the 1930s, the same crews that did
the rock work at the Patrick Creek Campground.
7.7 SET ODOMETER TO ZERO at the Gasquet Store. Toll Road
(right),
The Old Redwood Highway Road Tour returns to Highway 199
on the road next to the Gasquet Store.
During the past few miles, you have been following the
Middle Fork of the Smith River. At Gasquet, the north fork merges
with the middle fork.
The community of Gasquet was established in 1856 by
Horace Gasquet and his wife, both from France. His original store
and station was located between the north and middle forks of the
Smith River, probably because this is where the 1852 Cold Springs
Mountain Pack Trail crossed the North Fork of the Smith River. This
site was located near the present-day Gasquet cemetery. In the
following year, 1857, the Turnpike and Puncheon Road was completed,
which allowed for much less expensive shipping by freight wagon. No
doubt, the completion of this road caused a dramatic drop in the
number of pack trains going over the Cold Springs Mountain Pack
Trail. He later purchased property across the river, the side you
are on, and set up what was to become the town of Gasquet. The town
included a vineyard (foreground of picture above) that Gasquet used
to make wine for his customers.
By 1877, the Turnpike and Puncheon Road had gone defunct
and Gasquet was forced to use pack animals to ship supplies to
stores he had set up at Happy Camp, California and Waldo, Oregon. He
decided to build his own road to Waldo, which was completed in 1887
and became known as the Gasquet Toll Road. You can drive through the
redwood forest on a portion of this road by following the Old
Redwood Highway Road Guide. This section of the tour begins at South
Fork Road about seven miles from here.
The
road through the forest is named Howland Hill Road and has a graded,
gravel surface with more hiking opportunities than you will find on
the Highway 199 tour route. A picture of the road is shown to the
right. The turnoff for the old road is pointed out in
the next section of the Highway 199 Road Guide. To pick up the tour,
follow the Highway 199 Road Guide to South Fork Road. Follow safety
suggestions as you make the left turn on to this road. Tour
information for the
Old Redwood Highway Road Guide can be obtained by following the link titled
Redwood Forest at the bottom of the page.
NEXT...
Intro |
Cavemen |
Hays Hill |
Eight
Dollar |
Gold Country |
Elk Valley |
Ocean Crust |
Mantle
Rock |
Canyon |
Redwoods
|