Em 1960

em 1960

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Die Halbfinals wurden dann in einem Gastgeberland veranstaltet. Navigation Hauptseite Themenportale Zufälliger Artikel. Das Apartment Wichtige Ereignisse Das Finale sahen nur Die Führung der Sowjetunion lehnte ihrerseits eine Austragung auf neutralem Boden ab. Durch die Nutzung dieser Website erklären Sie sich mit den Nutzungsbedingungen und der Datenschutzrichtlinie einverstanden. Im Hinspiel gewann Irland am 5. In anderen Projekten Commons.

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Juni des Jahres verlängert. Bis dahin waren es dann 17 Nationen, die teilnehmen wollten, und das Turnier, welches damals den Namen Europapokal der Nationen hatte, konnte stattfinden.

Der Gastgeber, hier Frankreich, war im Gegensatz zu heute nicht automatisch qualifiziert, vielmehr mussten die Bewerber um die Endrundenausrichtung das Halbfinale erreichen.

Hätte Frankreich das Halbfinale nicht erreicht, so wäre unter den Halbfinalisten ein neuer Gastgeber ausgewählt worden.

Frankreich führte zur Halbzeit mit 2: Die Tschechoslowakei konnte sich nicht gegen die Sowjetunion durchsetzen, obwohl in ihren Reihen mit Josef Masopust einer der damals besten Spieler Europas stand.

Zum Matchwinner avancierte aber Mittelstürmer Wiktor Ponedelnik. Die beiden Treffer von Walentin Iwanow bereitete er vor und in der Minute erzielte er das Endergebnis von 3: Aus Enttäuschung über das Ausscheiden der französischen Gastgeber kamen zum Finale nur noch Sie erlebten ein dramatisches Endspiel, bei dem die Jugoslawen zur Halbzeit mit 1: Juli in Paris Endspiel Ansichten Lesen Bearbeiten Quelltext bearbeiten Versionsgeschichte.

Navigation Hauptseite Themenportale Zufälliger Artikel. The Valdivia earthquake occurred at Hundreds of people were already reported dead by the time the tsunami struck.

One ship, Canelos , starting at the mouth of Valdivia River , sank after being moved 1. A number of Spanish-colonial fortifications were completely destroyed.

Extensive areas of the city were flooded. The electricity and water systems of Valdivia were totally destroyed.

Witnesses reported underground water flowing up through the soil. Despite the heavy rains of 21 May, the city was without a water supply.

The river turned brown with sediment from landslides and was full of floating debris, including entire houses. The lack of potable water became a serious problem in one of Chile's rainiest regions.

The earthquake did not strike all the territory with the same strength; measured with the Mercalli scale, tectonically depressed areas suffered heavier damage.

The two most affected areas were Valdivia and Puerto Octay , near the northwest corner of Llanquihue Lake.

Puerto Octay was the center of a north-south elliptical area in the Central Valley , where the intensity was at the highest outside the Valdivia Basin.

Other volcanoes may also have erupted, but none were recorded due to the lack of communication in Chile at the time.

The relatively low death toll in Chile 5, is explained in part by the low population density in the region, and by building practices that took into account the area's high geological activity.

The earthquake was a megathrust earthquake resulting from the release of mechanical stress between the subducting Nazca Plate and the South American Plate , on the Peru—Chile Trench.

Subduction zones are known to produce the strongest earthquakes on earth, as their particular structure allows more stress to build up before energy is released.

Geophysicists consider it a matter of time before this earthquake will be surpassed in magnitude by another. Rupture velocity, the speed at which a rupture front expands across the surface of the fault, has been estimated as 3.

Across southern Chile the tsunami caused huge loss of life, damage to port infrastructure and the loss of many small boats.

Further north, the port of Talcahuano did not suffer any major damage, only some flooding. Some tugboats and small sailboats were stranded on Rocuant Island near Talcahuano.

A carabinero police boat, Gloria , was towing a few of these boats when the second earthquake struck on 22 May.

The stranded boat was wrecked when a tsunami wave came engulfing it. Canelos was anchored at Corral and filling a cargo of wood and other products destined to northern Chile when the quake struck.

The engine of Canelos was warmed up after the earthquake. After hours of drifting around in Corral Bay and Valdivia River the ship was wrecked and subsequently abandoned by its crew at Two men on board of Canelos died in the incident.

As of the remnants of Canelos were still visible. Santiago , another ship anchored at Corral at the time of the quake, managed to leave Corral in a bad state but was wrecked off the coast of Mocha Island on 24 May.

La Milagrosa was battered by the currents and waves of the tsunami for four days while moving south. Outside Corral the crew rescued six nearly unconscious and dehydrated children on board two boats.

The boats found were used to navigate in Valdivia River and Corral Bay but had drifted into the high sea. At the coastal town of Queule a carabinero reported hundreds of people to be dead or missing some days after the tsunami.

Historians Yoselin Jaramillo and Ismael Basso report that people in Queule decades later know about 50 people to have died because of the earthquake and tsunami.

The earthquake triggered numerous landslides , mainly in the steep glacial valleys of the southern Andes. Some of these areas remain sparsely vegetated while others have naturally developed more or less pure stands of Nothofagus dombeyi.

While most landslides clustered around north-south strips in the Andes, other areas that were affected by a large numbers of earthquakes were the coast, mainly the foot of the Chilean Coast Range , and the shores of Llanquihue Lake.

A seiche of more than 1 meter was observed on Panguipulli Lake following the earthquake. The wave, most likely produced by an earthquake-triggered sediment slide at the lake bottom, killed two people and destroyed a pier in San Carlos de Bariloche city.

This potential disaster would have violently flooded all the settlements along the course of the river in less than five hours, with more dire consequences if the dam suddenly broke.

About , people lived in the affected zone. The eruption fed a 5. These vents produced an output of about 0. The eruption ended on 22 July.

As a result of an evacuation plan there are no reported human deaths associated with the eruption. The levels of material damage were relatively low given the high magnitude of the earthquake.

Part of the reason behind this was the limited infrastructure development of the region next to the rupture zone. It has been estimated that about 40 percent of the houses in Valdivia were destroyed, leaving 20, people homeless.

Traditional wooden houses fared better; although many were uninhabitable if they did not collapse. Houses built upon elevated areas suffered considerably less damage compared to those on the lowlands, which absorbed great amounts of energy.

Many city blocks with destroyed buildings in the city center remained empty until the s and s, with some of them still used as parking lots.

Before the earthquake, some of these blocks had modern concrete buildings built after the Great Valdivia fire of In terms of urban development, Valdivia suffered the loss of the minor but significant Cau-Cau bridge, a bridge that has not been rebuilt.

The other bridges suffered only minor damage. Land subsidence in Corral Bay improved navigability as shoal banks, produced earlier by sediments from Madre de Dios and other nearby gold mines, sank and were compacted.

The United States quickly set up a field hospital following the earthquake. The earthquakes damaged an area that had suffered a long period of economic decline, which began with shifts in trade routes, due to the expansion of railroads in southern Chile and the opening of the Panama Canal in Unlike Valdivia, Osorno was saved from major destruction.

In Osorno only about 20 houses were totally destroyed, although many firewalls and chimneys collapsed.

Puerto Montt , a major city today, had in the early s about 49, inhabitants. The tsunami that struck the coast of southern Chile destroyed seaside farms, killing numerous livestock and people.

As a result of the earthquake, an international technological cooperation programme was established in the dairy sector.

The economy of the coastal town of Queule had during the s developed significantly. Its economy based on fishing, agriculture and industry had grown.

Em 1960 -

Frankreich führte zur Halbzeit mit 2: Im Hinspiel gewann Irland am 5. Die Sowjets nehmen die Steilvorlage dankend an und präsentieren sich der Welt als Gralshüter des Sportgedankens. Spanien hingegen muss ein "Reuegeld" von 2. Der Gastgeber, hier Frankreich, war im Gegensatz zu heute nicht automatisch qualifiziert, vielmehr mussten die Bewerber um die Endrundenausrichtung das Halbfinale erreichen. Juli in Frankreich stattfand. Sieger des Pokals der europäischen Meistervereine:

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