Isthmus of Corinth

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Isthmus of Corinth

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Isthmus of Corinth, Natural land bridge near Corinth, Greece

The Isthmus of Corinth forms a 6.3-kilometer-wide connection between mainland Greece and the Peloponnese peninsula, rising 90 meters above sea level.

The Romans attempted to construct a canal through the isthmus in 67 CE, with Emperor Nero deploying 6,000 slaves before the project ceased upon his death.

The southern section of the isthmus contained the sanctuary where athletes gathered every two years to participate in the Isthmian Games competitions.

Two road bridges, two railway bridges, and two submersible bridges currently traverse the Corinth Canal, which cuts through the center of the isthmus.

The ancient Diolkos path allowed vessels to be transported across the isthmus on rolling logs, reducing the journey around the Peloponnese by 320 kilometers.

Location: Corinthia Regional Unit

Elevation above the sea: 94 m

GPS coordinates: 37.93293,22.98374

Latest update: May 28, 2025 18:37

Natural stone arches and rock holes

Geological forces have carved openings, arches, and caves into rock formations across continents through millions of years of erosion. Water, wind, and weathering have shaped these natural structures from various rock types, creating landmarks that reveal the Earth's ongoing transformation. The formations appear in diverse environments, from coastlines where ocean waves carve passages through limestone cliffs to desert regions where wind erosion creates openings in sandstone walls. This collection spans locations such as Durdle Door along England's Jurassic Coast, where a 200-foot (60-meter) arch rises from layers dating to the Mesozoic era. The Faraglioni Rocks off Capri reach heights of 360 feet (109 meters) and include a natural passage navigable by boat. In landlocked regions, formations like the Eyes of God in Bulgaria's Prohodna Cave display symmetrical ceiling openings where sunlight penetrates the rock. Desert sites such as Las Ventanas in Argentina's Andes showcase wind-carved arches in remote sandstone landscapes. Each location offers direct evidence of erosion processes that continue shaping these geological features, from readily accessible coastal points to isolated areas requiring significant travel to reach.

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