Sunday, November 28, 2021

Corona walks number 8, Goederede

A good shelter


Goederede in Dutch means “good shelter”. The medieval sailing ships were more or less forced to sail before the wind. The prevailing winds in the English Channel and the North sea are south-west to North-west. To sail out of the Rhine Delta or up the river after coming into the Delta, ships had to wait for favourable winds. This was done in the little shelter which the flat muddy island of Goeree south of Rotterdam could provide for the anchoring ships. A settlement was found to cater to the anchoring ships and it was aptly named Goedereede.


The market square in Goedereede


For that time the port was big and convenient. The place became important quite quickly and already in 1312 it was rewarded city rights which included the right to catch herring. A gate tower was built to protect the entrance to the port. In case of enemies approaching, chains could be spun between the towers of the gate to prevent them from sailing into the port. This gate still is the coat of arms of the town.




In 1453 the little town started to replace their little chapel with a representative church dedicated to St. Catharina, which in the subsequent years was successively enlarged. The nave of two aisles was attached to an enormous steeple which at the same time served as a lighthouse. It took from 1467 to 1512 to finish the steeple, however, the top was never put on.


Between 1492 and 1507 the pastor of the church was Adriaan Floriszoon Boeyens (Utrecht, 2.3.1459 – Rome, 14.9.1523). A statue next to the steeple announces that he was the only Dutch pope, Hadrianus VI, from 1522-1523. However, the future pope never lived in Goedereede. At the time he was part of the community of the Church of St.Pieter in Leuven in Belgium and taught at the university there. One of his disciples at the university was Erasmus of Rotterdam, and he also became one of the teachers of young prince Karl, son of Habsburg emperor Maximilian I, who later became emperor Karl V, the guy whose sun never set.


Statue in memory of Paus Hadrianus in Geodereede

The life of Adrian is quite fascinating. He was born in Utrecht as son of a carpenter who died when he was only 10 years old. His birthplace in Utrecht, which was later turned into a school for girls, still exists. The boy was intelligent and eager to learn and against all odds passed through different schools in the Netherlands until he begun to study in Leuven in 1476.


Entrance to the Paushuis in Utrecht

His friendship to Karl V. determined his career. He was entrusted with the sale of indulgences. One third of the money which people donated to save their souls was given to the pope in Rome, two thirds were to be used by Karl V to improve the dikes in the Netherlands. In 1515 Hadrianus was sent on a diplomatic mission to Spain, where he successively became bishop, cardinal and the head of the government after Karl was crowned emperor and moved to Belgium. In 1518 he also became the head inquisitor of Castilia and Leon. After the departure of Karl he stayed back in Spain alone. He had no experience in government and, as a foreigner, was not able to deal with the local politics. When an uprising started, he was not able to suppress it. Only after several pleas he was replaced by two Spanish rulers in 1520 but had to stay in Spain to fulfil his task as inquisitor.


The Paushuis in which the pope never lived

After 1517 and while in Spain Hadrianus had ordered to get a house built in Utrecht. He intended to move in there for his old days. However, he never even got to see his house. In 1521 he was nominated to become pope in Rome. He took more than half a year to decide whether to accept the nomination but eventually he sailed to Rome and was crowned in 1522. 


Statue in memory of pope Hadrianus in Utrecht

In Rome he had to cope with a hostile population, corruption and chaos in the church, opposing political fractions backed by the French king Francois I on one side and emperor Karl V on the other side, the Turks in the east and the rise of Protestantism and Martin Luther in the North. In addition, the kitty of the papal state was empty since Hadrianus’ Medici predecessor had spent all the reserves on the splendid luxury of his court. One solution to earn money was the trade in indulgences, where Hadrianus already had some experience. That was exactly what Luther was opposed to. Luther said about the new pope:

“The Pope is a magister noster of Leuven, where even donkeys have the chance to acquire the doctorate. His words and actions are inspired by Satan.”


Statue in Goedereede

Hadrianus stayed pope for only a little more than one year. At age 64 he probably died from a kidney infection, and not, as frequently has happened, from poison. In spite of his short rule he already had aquired a nickname: “videbimus“, or “we shall see”. Hadrianus was the last non-Italian pope until the election of Polish Karol Józef Wojtyla in 1978.


The Gouden Leeuw at the market place to the right and the southern entrance to the port where a big port building used to stand

At the market in Goedereede, the “Gouden Leeuw”, built in 1482, after a big fire destroyed the town, is one of the oldest buildings in town. The building always served as a inn, originally for travelling salesmen and merchants. Today it is one of the oldest surviving hotels in the Netherlands. One of the hotel rooms is named after Adrianus Floriszoon Boeyens, the later pope, who was never here.


The gouden leeuw


The interior has preserved a lot of the original features and is at the same time stylish in a modern way. Like in many traditional old inns and merchant houses in the Netherlands there is a wooden balcony above the bar in the back of the guest room. On the walls, tasteful art and in the air, subtle and appropriate music. I arrive wearing a face mask shortly after the opening time at 10 am and I am the only guest. The friendly owner prepares my coffee and a piece of the typical apple pie. His regular coughs bring me back from medieval times into the age of a pandemic. He does not wear a mask. After a while his young help arrives. He had been at a boozing with his soccer club last night. Because everything has to close at 8 pm the 60 of them had to meet in a different room which had no windows open to the street. There had been around 25.000 daily positive tests in the Netherlands for the last week and the health care is at the brink of collapse.


The interior of the gouden leeuw

In the 16th century the tide turned in Goedereede. The entrances to the port started to silt up. Although as early as 1540 some measures were taken to prevent the silting of the harbour, by 1560, half of the population of the town had left. In addition, a series of floods covered the land around town. In 1570 a flood caused the collapse of a part of the gate tower protecting the entrance to the port. Eventually polders were created by building dykes. However, the consequence was that the canal linking the town to the sea became longer and longer. Goedereede lost its importance as a merchant port. Only fishing boats remained. But also merchants and artisans left. Their abandoned houses fell into disrepair and were demolished. The inhabitants turned to agriculture. The gaps in the city were filled with barns and sheds.


The backyards of the rich houses in Goedereede


The wooden barns


With the decline of the town also the big church went into dereliction. By 1706 the nave was in such a desolate state that it was demolished and replaced by a much smaller, free standing neo-gothic nave. The steeple remained and still towers above the town. The location of the former columns supporting the roof are indicated in the space between steeple and the baroque nave. The lower part of the northern wall of the nave is also preserved.


The new and old parts of the church


The wall remembering the former nave


In the second half of the seventeenth and in the eighteenth century the United Netherlands and England clashed in four Anglo Dutch wars over the supremacy of trade and rule over the oceans of the world. Fortifications were built to protect the many entrances of the river delta. Close to Goedereede an earthen defence structure was built in the seventeenth century to block passage of enemy ships into the Grevelingen part of the delta. The original structureof the so-called Schans was largely demolished in 1673. In 1795 it was rebuilt, now in a modern style. The earthen fortifications are still there today while the buildings which used to house the soldiers in the central courtyard are gone. A couple of old cannons decorate the bastions and remind of the former use. In the distance the steeple of the church of St. Catharine in Goedereede towers above the flat countryside.


The fortress guarding the entrance to the Grevelingenmeer


When the entrance for ships into the town became too difficult in the second half of the 19th century, the fishers of Goedereede decided to move to a new port at the seaside end of the canal. A new hamlet called Havenhoofd was found. The port in the town centre was only used occasionally by cargo ships.


The last windmill of Goedereede is also the last one in the Netherlands with an outside staircase to gain space for living quarters inside


Remainders of the medieval wall around Goedereede with a statue symbolizing the disposal of garbage across the walls  

But the town was still close enough to the sea to harvest what was available. In 1918 a cargo ship was sunk by a torpedo of a submarine. In the middle of the great war, the ships precious cargo were barrels of port wine. The fishers of Goedereede succeeded in recovering 436 barrels. The wine was auctioned at the town’s market and gained 300.000 guilders. A third went to the fishermen, the rest into the treasury of the town. When two argue, the third laughs. The Netherlands were neutral in the first world war.


The canal linking Goedereede and Havenhoofd

In the second world war the Netherlands were quickly overrun by a German invasion in 1940. Despite its remote location a detachment of the German coast guard was deployed in Havenhoofd. Now the activities of the fishers were closely supervised. The fishermen had to be back at sunset and afterwards the entrance to the port was closed with a chain. The fish caught went to the German troops.


Havenhoofd

But it would get worse. With the threat of an allied invasion becoming more real, the fishing boats were confiscated. The attempt of building a defensive structure called the Atlantic wall along the entire coast from France to Denmark started with the deployment of an artillery detachment in Havenhoofd. For the construction of the Atlantic wall all the fishermens’ cottages were raised in 1943. The inhabitants had to find a refuge elsewhere. Only in 1947 the building of new replacement homes started. That is why there are no historic buildings in Havenhoofd.


Statue memorizing the discharge of fishing boats with baskets in Havenhoofd 

However, with the construction of the Delta works, the flood gates protecting the southern Netherlands from the North sea, the port of Goedereede was finally closed and a thousand years of marine tradition came to an end.


The construction of the flood gates at the Haringvliet were the end of Havenhoofd-Goedereede as a seaport 

When I come to Goedereede next time the corona regulations have been tightened. This time I enter the other cafe at the market square. Again I am the only one wearing a mask. They have not bothered to increase the distance between the tables to 1.5 m as required by the tightened regulations and the place is much smaller and lower than the Gouden Leeuw. Nobody wears a mask. They ask for the QR code certifying to be tested, recovered or vacinated but do ask any proof of identity as required by the regulations. The next guests who enter admit openly that they have no QR code. That is also OK for the staff, who will loose a big part of their income by the tightened regulations and therefore are grateful for any guest. Nobody asks me, the only other guest, whether I agree to sit close to somebody who might be infected.


The inner harbor in Stellendam

Today the seaport of the island of Goeree-Overflakkee, on which Goedereede is located, is closeby in Stellendam. The town has an outer harbour open to the tides and an inner harbour protected by the flood gates and accessible by locks. In the outer harbour, fishing boats moor in front of the “visafslag”, a huge building where the arriving fish is auctioned. A big part of the inner harbour is used for ship building.


Ships in the inner port of Stellendam

The entrance into the inner port is guarded by cameras which register license plates. A police car warily inspects the jetties. Since the big container ports are closely observed the drug smugglers have changed their tactics. Now the drugs are thrown overboard the big ships off the coast and small boats or fishing vessels pick up the contraband and bring it into minor ports where they attract less attention. It is a profitable but dangerous business for fishermen who suffer from reduced quota and overfished seas.


Fishing boats in the inner port...


...and the fish auction in the outer port

In some places history is so dynamic that it is surprising that anything from the past survives. Or, on the other hand, since economic and military attention turn away, old structures remain because nobody bothers or has the money to remove them.


The entrance to the ports of Stellendam

Another town with the name of Goede Reede was found on an island in a complete different part of the world. Dutch slave traders found a settlement on an island in the bay off Dakar in Senegal. Later the name was turned into French Goerée. This is part of a previous story:


Sources


"non omne quod minatur ferit"
("not everything that threatens strikes")
Relief in the courtyard of the Paushuis in Utrecht

Saturday, November 20, 2021

Number 75 Spain 2005, La Palma


How to live with volcanoes?


Most volcanic activity is caused by the tectonic plates pushing against each other. But there are also so called hot spots, areas of overheated magma which weaken the crust above and cause thinning and melting and break through which results in volcanic activity above the hot spot. Since the tectonic plates move above the hot spot a chain of volcanoes is created. While older ones are left behind extinct on one end of the chain, new ones are formed at the other end. Hot spots can be under the oceans or under the surface of the continents. Supposedly there are more than 40. The most famous visible manifestations are the Hawaiian islands, Yellowstone, the Galapagos islands, Cabo Verdean islands, Madeira, the Azores and the Canary islands. But also very close by, the presently dormant Eifel volcanoes were caused by a hotspot. There seems to be an eruption every 60.000 years. The last one 60.000 years ago threw ash as far as the south of France...


In Tazacorte...


...the main town on the west coast of La Palma


Of the seven major islands of the Canarias, four are volcanically active: Tenerife, El Hierro, La Palma and Lanzarote. The Teide volcano on Tenerife is the third tallest volcano on Earth on a volcanic ocean island. In the summer of 2011 a series of low-magnitude earthquakes occurred beneath El Hierro followed by a submarine eruption producing gases and pumice.


Ruin of a windmill

However, together with Tenerife the most volcanically active of the Canary islands is La Palma. Since the Spanish have kept records, there have been eight eruptions which all have occurred in the area of Cumbre Vieja:
1470–1492 Montaña Quemada
1585 Tajuya near El Paso
1646 Volcán San Martin
1677 Volcán San Antonio
1712 El Charco
1949 Volcán Nambroque at the Duraznero, Hoyo Negro and Llano del Banco vents
1971 Volcán Teneguía
As everybody meanwhile knows the latest eruptions started on 19th September 2021 after earthquakes at Volcán Tajogaite.


Our little house in Tijarafe

In 2001, with a little baby of 18 month we decided that we needed a break. We were fortunate enough that my mother was willing to come along as a babysitter. As accommodation we rented a beautiful little house with a big view in Tijarafe in the northwest of the island. In the morning the house was just high enough up on the slope above the coastal cliffs that the mist stayed in a layer above the sea below us. The slopes had some orchards, but there was no village close by. A few old houses looked abandoned. A narrow access road led to the house. For today’s standards it was rather simple, a couple of sparsely furnished bedrooms, a kitchen and living room and a big terrace overlooking the sea. No swimming pool which only would have caused paranoia about the danger for a mobile baby.


Houses along the old country road near Tijarafe


La Palma is a drop shaped island. The base lies almost 4,000 m below sea level and reaches a height of 2,426 m above sea level. Most of the coast is formed by steep ocean cliffs. The northern part of the island is formed by the caldera de Taburiente. About a half a million years ago, the Taburiente volcano collapsed with a giant landslide, forming a caldera with a diameter of 10 km and in parts a depth of 2000 m. From the caldera running south a chain of more recent volcanic craters forms the crest of the island. The caldera of the Taburiente volcano was designated a national park in 1954.


The caldera of Taburiente


Exit of the caldera

The presence of my mother as a babysitter allowed us to do some hiking without need to carry around the baby in a backpack. The caldera of the volcan Taburiente was close by. The caldera is open on the western side and allows a lively stream of water leaving the volcano via the Barranco de las Angustias. Because of the height the upper slopes of the crater are covered by a shady forest of pines. There is a trail along the water into the caldera with nice spots to have a refreshing dip. Other trails follow the rim of the enormous crater.


Hiking along the rim of the crater


The collapse of the Taburiente volcano must have been an enormous event with far reaching consequences although the crater itself probably was formed by erosion. Basaltic ocean islands such as the Canary Islands tend to experience catastrophic landslides every few hundred thousand years. For example, the 1883 eruption of Krakatau, Indonesia, caused a tsunami killing tens of thousands. Scientists have calculated the flood resulting from the collapse of a significant portion of an island with a potential to displace vast amounts of seawater. A simulation by Ward and Day made in 2001 describes a doom scenario which seems to have been taken right out of the plot of a Hollywood movie. The landslide would instantaneously create a water dome of 900 m high above La Palma. A flood wave more than 50 m high would reach the African coast in less than 60 min, a tsunami of 25 m high would reach the Florida coast after 9 hours. Spain, and even France would be affected by flood waves of 5-7 m high. The study later was criticized and it is improbable that a landslide causing such an enormous tsunami ever happened.


While the huge Taburiente volcano is dormant or extinct now, a chain of more recent volcanoes extends from there south. A 23.70 km long hiking trail, the ruta de los volcanes, links the Refugio del Pilar at the caldera de Taburiente with the Faro de Fuencaliente at the southern tip of the island. It is one of the most spectacular hikes I know. The route follows a crest along a moon like landscape of a chain of volcanic craters with only little recent vegetation. We walked in two day hikes. The first day from the Refugio El Pilar via the Mirador de Birigoyo, Hoyo Negro (1 h 47 min, 4,80 km), El Duraznero (Volcán de San Juan, 2 h 17 min, 5,83 km), Las Deseadas (3 h 10 min, 7 km), Volcán de Martín (4 h 30 min, 10,5 km) reaches the little town of Los Canarios after 17,2 km and 6.5 h. The highest point is at 1933 meters in Las Deseadas. In total there is a descent of 1207 meters. From Los Canarios it is necessary to take a bus and taxi back to the starting point at the refugio.


Main street of Los Canarios

This route passes the area of the more recent volcanic activity on La Palma. The 1949 eruption in the Duraznero, Hoyo Negro and Llano del Banco vents caused a lava flow which ended up forming a lava delta, a peninsula stretching out into the Atlantic ocean to the west. It can be seen from the hiking trail at the crest of the chain of craters. After 50 years much of these deposits is covered in green houses and recent buildings.


The peninsula ....


.... and the old vent of the previous eruption ....


..... are also the site of the current activity


Volcan Duraznero

Starting on September 19th, 2021, the Cumbre Vieja area of the La Palma volcano started erupting again. Following the collapse of part of the interior cone the size of the lava lake increased and lava flows spilled down the side of the mountain. With the lava, ash was ejected and on September 25th La Palma Airport suspended all flights due to ash accumulation. Sometimes dense and billowing ash-and-gas plumes rose up to 2.8-4 km above sea level. Up to 53.600 tons of Sulfur dioxide were emitted per day. Some lava fountains rose up to 600 m above the vent. Big junks of rock were spat out, which sometimes drifted downhill like boats on the sea of lava.


The craters of Las Deseadas along the ...


... ruta de los volcanes.


The Hoyo Negro crater


Volcan de Martin


The lava flows reached the sea and a lava delta reached to 120 m water depth. The thickness of the flow at the delta was 10-30 m and covered an area of about 0.11 square kilometers. The new lava delta is not far from the one formed in the eruption of 1949.


At the horizon to the right the Island of La Gomera and to the left ...


.... el Teide volcano on Tenerife


The eruptions were accompanied by seismic activity. Some of the shocks were not only felt by the local residents, but also on La Gomera and Tenerife.


Volcan San Antonio


The eruption has caused the evacuation of around 7,000 people, and by october 29th the lava flow had covered 946 hectares. At that point 2532 buildings had been destroyed, including the entire town of Todoque. What was not destroyed was covered by a thick layer of ash. In brief interruptions of the lava flows and ash rains desperate homeowners returned to retrieve stuff. Since the area flooded by the recent lava flows was so close to the previous flows from not even 100 years ago a certain risk of new volcanic activity could have been expected. Apparently there were no volcano related building restrictions in this area. It will be interesting to wait how long it will take until development will start anew after the present activity has ceased.


The lighthouse of Fuencaliente

In a second day we walked from Los Canarios to the lighthouse Faro de Fuencaliente (6,7 km one way) at the southern tip of the island. On the way Volcán de San Antonio and Volcán de Teneguía are passed. This is the area which was most affected by the eruptions of the Teneguia volcano in 1971. In 2001 these activities were only 30 years ago and the area looked even more like a moonscape that the Cumbre vieja area the other day. A black landscape of desolation with, as backdrop, the blue sea.


The salt pans at Fuencaliente

Next to the lighthouse rock pools are used to evaporate sea water to produce salt. On the other side is a beach. Like most beaches in La Palma it is black. Swimming on these beaches is dangerous and most wave the red flag throughout the year. 


The port and beach of Tazacorte

When we had a rest on one of the beaches at Tazacorte, my mother had disappeared. Not realising the red flag she had still tried to have a dip. In one of the big waves she had lost her foothold and was turned upside down. We got alarmed when we saw legs and feet briefly appear above the water and then disappear. I started to run and together with another helpful soul we dragged her out of the water. She had almost fainted and her sense of up and down had disappeared. After we had safely returned to solid ground one of the beach’s bay watch heroes appeared and reproached her angrily about entering the water. He should have made his reproaches when he saw her going in and not afterwards.


The beach of Tazacorte

At points where the bottom of the steep cliffs can be reached the islanders have built boat houses which also seem to have a second life as vacation homes. Frequently there are concrete pools which provide safer spots for a dip. But even there, with high surf, a big wave can flood a pool in a wink.


The fishing coves of Puntagorda ....



.... and Playa Jurada 


In the time of corona with tourists staying away and lockdowns blocking tourism for entire months an economy like the one of the canary islands is in despair. Nevertheless the official tourist board for La Palma tries to market the 'Isla Bonita'. Tourists come in big numbers to watch the volcanic activity. They neither seem to be scared away by the many quakes registering up to 5 on the Richter scale (such as on sunday 30.10.) nor the risk of cancelled flights after airport closures due to ash clouds. La Palma's local council even launched a transportation plan with free shuttle buses for all those who wish to visit the volcanic area. The volcano is not seen as a threat but as a chance….


Endemic plants of the Canarian islands


Dracena draco


euphorbia canariensis


Sources:


The port of Tazacorte

Previous post about volcanism:


Puntagorda


Tazacorte