It seems that just about everyone is going to Portugal these days. Part of the attraction is the generous process for obtaining citizenship there (see this link to learn about the Golden Visa program). And as the USA drifts ever closely toward authoritarianism, a sunny beach-rich and laid back environment looks quite attractive. For me, the attraction was hiking with my wife Helen and two other couples for 14 days along a beautiful and exhilarating coastline. Some people's idea of a vacation may not include a 100-mile walk but it is exactly what we love to do. As an added "attraction", I purposely did not study any of the geology we might encounter while there. - I wanted to be surprised and boy, was I ever!
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| What's not to like about Latin countries? |
There are quaint, seaside villages, great food including locally caught seafood, opportunities learn a foreign languages, and as always, interesting landscapes and friendly people. As Mark Twain wrote in
Innocents Abroad, "Travel is fatal to prejudice, bigotry and narrow-mindedness...". How true!
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| Our course on the Fisherman's Trail took us from Porto Covo in Alentejo to Lagos in the Algarve |
The Fisherman's Trail was designated in 2013 and cobbled together from various pre-existing trails into a long, 140 mile coastal route. It is one of the newest of Europe's long hiking routes. An association of interested parties (hotels, villages, and transport service companies has formed called
Rota Vicentina. See that web site for great information on how to hike the trail.
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Stages of the Fisherman's Trail from Porto Covo to Lagos
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Some of the 13 stages were longer than I wanted to do (up to 15 miles a day). I requested a bit more user friendly itinerary that would allow us to arrive in villages earlier in the day and more fully experience their charms. It turned out to be a wonderful and enjoyable hike! That's how I answer folks who think walking 100 miles in 14 days cannot be considered a vacation.
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| The official colors of the trail are green and blue - other nearby trails have other colors |
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| These are the symbols we would follow to stay on course |
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| The owner of Vicentina Travel is Ricardo Estêvão, who came to see us at the start of our trek |
We used Ricardo's company, called
Vicentina Travel and he was great to work with. He reserved all of the accommodations for us, set up luggage transfers, provided excellent maps of the area, and was always available via
What'sApp to provide guidance when needed. I highly recommend this company. Ricardo also serves on the board of the Rota Vicentina Association.
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| On occasion, the trail left the coast and through the nearby forest |
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| This view is just north of Cavaleiro - note the upturned sedimentary rocks |
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| The lighthouse at Cabo Sardão near Cavaleiro |
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| Deformed sedimentary strata south of Cavaleiro |
These sedimentary rocks were deposited in a narrow seaway about 312 Ma and are known to geologists as
flysch. The term was first applied to similar sedimentary sequences exposed in the Alps. Flysch is sediment that is shed off of ancient mountains and initially deposited in deep water but as the sediment fills in the marine trough it slowly grades upwards to shallow water sandstone. What you will notice in the photo here is that the layers are at various angles that are bounded by thrust faults. Soon after the flysch was deposited it became caught up in a continental collision associated with the amalgamation of the supercontinent Pangaea.
This is the paleogeography when Pangaea began to take shape. Land that is colored lightest gray is part of
Laurussia also known as
Laurasia. It includes North America (upper left), southern Greenland and Scandinavia (all in light gray). The dark gray at the bottom is the southern continents of Gondwana, (South America, Africa, and the Iberian peninsula - located to the left of the small "b". Yes, at this time Iberia was attached to Gondwana! You will notice that in between Laurussia and Gondwana is an intermediate gray color and is a microcontinent called
Amorica that was caught in a vice-like manner between the two larger landmasses. This is how and when the folds we were to see on our trek were formed. The collision of these three landmasses created the supercontinent of Pangaea, approximately 300 to 260 Ma. This mountain building event is called the
Variscan orogeny (aka as the Hercynian orogeny). Eventually, the Rheic Ocean closed when South America (lower left) would drift into North America to create the Ouachita folds in Oklahoma and Texas, and the Ancestral Rocky Mountains in the American Southwest. Such interesting (and large) considerations in Earth history!
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| On day 10, we made our approach to the southwestern most point in Europe, Cabo São Vicente |
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| Getting closer to Cabo São Vicente! |
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| This is the outcrop at Telheiro Beach, just to the north of Cabo São Vicente |
Telheiro Beach hosts an iconic angular unconformity and is listed as an International Geoheritage Site by the International Commission on Geoheritage.
Check out this link to learn more. And
here is another useful link. In the view above, red-colored Triassic rocks (about 210 Ma) sit on top of the Late Carboniferous flysch deposits (far left). A 3-D model of the unconformity can be viewed
here. A cap of Cenozoic marine limestone is in turn capping the Triassic rocks. This was one of the detractions for me by NOT learning about the geology ahead of the trip - I had no idea of the worldwide significance of this unconformity while I was there. Overall however, being surprised most of the trip was a plus!
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| A fort near this point (south of Sagres) is thought to be the location of the Sagres School |
Our layover day in Sagres was wonderful! If you do decide to do this trail, I can highly recommend going slow and arranging for layover days. It is a time to rest up, do laundry and enjoy the surroundings!
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| Mesolithic monument called Menhir do Padrão between Sagres and Luz |
This limestone rock is the last one standing at this location. It was pointed out to us by a taxi driver. He told me that when he was a boy, the farmers used to knock these down in plowing their fields - no one knew what they were! He said he used to ride his moto-cross bicycle over them to 'pop wheelies'. Then it became known that these were part of a Mesolithic culture that lived here some 7500 to 6500 years ago. You can read or about the Menhir do Padr
ão at this link.
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| Helen had the idea to take a photo of the feet that had carried us over 100 miles! |
That's my feet in the Chaco sandals. I had heard of the sand along the trail and decided that rather than emptying my shoes of sand every so often, I would just negate that need. It worked out fine as I usually do all of my Grand Canyon river trip hikes in these sandals.
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| After a lovely night in Luz, we looked back to the west at the village |
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| We ultimately came upon the black rock mass and indeed it was an intrusive plug! |
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| We finally made it to Lagos and Ponta da Piedade - Pity Point |
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| The rock formations are wonderful at Ponta da Piedade |
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| One of the many fine beaches in Lagos |
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| Walking to our hotel in Lagos |
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| Wayne and Helen at the end of the trail in Lagos Portugal |
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| Inspired by the trail! |
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| Thank you for reading this far! Hip, hip hooray to my hiking companions! |
Thanks to Joe, Judy, Don, Anne and especially Helen for being such wonderful trail mates! I would travel anywhere in the world with you all! Obrigado.