4.6
(372)
2,499
자전거 타는 사람
166
라이딩
펠로폰네소스 산맥에서 하이킹하며 펠로폰네소스 구석 부분까지 살펴볼까요? 펠로폰네소스 산맥에 있는 모든 하이킹 및 워킹 경로 컬렉션 중 가장 멋진 하이킹 경로를 엄선하여 소개해드릴게요. 다른 하이커가 공유한 실제 팁과 사진을 살펴보고 후기를 읽으며 마음에 드는 펠로폰네소스 산맥 워킹 경로를 찾아보세요.
마지막 업데이트: 4월 13, 2026
4.8
(37)
286
자전거 타는 사람
42.2km
02:37
540m
540m
어려운 자전거 타기. 우수한 체력 필요. 대부분 포장된 지면. 실력과 관계없이 누구나 갈 수 있음.
4.0
(23)
164
자전거 타는 사람
23.8km
01:27
130m
130m
초급용 자전거 라이딩. 모든 체력 수준에 적합. 대부분 포장된 지면. 실력과 관계없이 누구나 갈 수 있음.
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4.9
(24)
143
자전거 타는 사람
28.0km
02:00
540m
540m
어려운 자전거 타기. 우수한 체력 필요. 대부분 포장된 지면. 실력과 관계없이 누구나 갈 수 있음.
4.4
(10)
93
자전거 타는 사람
32.1km
01:57
220m
220m
보통 자전거 타기. 좋은 체력 필요. 대부분 포장된 지면. 실력과 관계없이 누구나 갈 수 있음.
4.6
(12)
77
자전거 타는 사람
28.4km
01:55
430m
430m
보통 자전거 타기. 좋은 체력 필요. 대부분 포장된 지면. 실력과 관계없이 누구나 갈 수 있음.
4.0
(11)
65
자전거 타는 사람
24.3km
01:27
140m
150m
초급용 자전거 라이딩. 모든 체력 수준에 적합. 대부분 포장된 지면. 실력과 관계없이 누구나 갈 수 있음.
3.4
(11)
43
자전거 타는 사람
25.9km
01:48
360m
360m
보통 자전거 타기. 좋은 체력 필요. 대부분 포장된 지면. 실력과 관계없이 누구나 갈 수 있음.
5.0
(8)
49
자전거 타는 사람
55.9km
04:07
1,250m
1,250m
어려운 자전거 타기. 우수한 체력 필요. 대부분 포장된 지면. 실력과 관계없이 누구나 갈 수 있음.
4.4
(7)
60
자전거 타는 사람
10.5km
00:40
50m
50m
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4.3
(10)
31
자전거 타는 사람
48.9km
03:03
480m
480m
어려운 자전거 타기. 우수한 체력 필요. 대부분 포장된 지면. 실력과 관계없이 누구나 갈 수 있음.
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It goes through the water and over two or three concrete pipes above
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Neoclassical city palaces dominate the old town. These were built during the time when the city was the Greek capital from 1829 to 1834. There are also buildings from the Venetian and Ottoman periods.
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Very interesting, much more interesting to show us electric bikes than to show us the crater. When will people start giving real information?
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Don't forget to mention to those who ride power bikes that there's a pure water fountain next to the shelter. Another thing: no need for a mountain bike: all the roads are paved.
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Great island, unfortunately got stuck in the restaurant
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Methana Peninsula The Methana Peninsula was formed from the seabed by successive volcanic eruptions that began about 1,000,000 years ago and ended about 250,000 years ago. Then everything was quiet here for thousands of years and the landscape we see today was already formed. However, around 250 BC there was another small eruption. This eruption is mentioned by Pausanias, among others, in his writings. He says that there was a fertile plain that stretched from the present village of Kammeni Chora to the sea in the west. The whole area was covered by lava that accumulated over months and formed the steep mountain that you can see right behind your back. The height of the mountain is about 400 m. It was not a violent eruption. During the last phase, the viscous lava flow died out in the sea in the west. The volcanoes of Methana do not have the typical caldera shape. The lava here was so viscous that it accumulated vertically, forming high, steep mountains. The eruptions here were usually not violent and lasted a long time. In general, every mountain you see in the area is a single eruption. About 30 individual volcanic eruptions are visible on the Methana peninsula. On the summit of Kammeni Chora volcano you will find a crack that probably appeared during the last phase of the eruption, when the rich lava flow reached the sea. From the summit you can follow the lava flow with your eyes all the way to the sea. The sunset here is more beautiful than on Santorini. The lava glows red again in the last light of the setting sun. Methana volcano is active, however we cannot yet predict where and when the next eruption will be. The hike to the summit takes about 25 minutes. Text and pictures: Elias Rizos - www.volcanotrails.gr Read about the Kammeni Chora volcano on www.volcanotrails.gr SCAN ME A travel guide to Methana-topia www.volcanotrails.gr SCAN ME Map of Methe Background from 2002 Methana Peninsula The Methana peninsula was formed from the seabed by successive volcanic eruptions that began about 1,000,000 years ago and ended about 250,000 years ago. Then everything was quiet here for thousands of years and the landscape we see today was already formed. However, around 250 BC there was another small eruption. This eruption is mentioned by Pausanias, among others, in his writings. He says that there was a fertile plain that stretched from the present village of Kammeni Chora to the sea in the west. The whole area was covered by lava, which accumulated for months and formed the steep mountain that you can see right behind your back. The height of the mountain is about 400 m. It was not a violent eruption. During the last phase, the viscous lava flow died out in the sea to the west. Methana's volcanoes do not have the typical caldera shape. The lava here was so viscous that it accumulated vertically and formed high, steep mountains. The eruptions here were usually not violent and lasted a long time. In general, every mountain you see in the area is a single eruption. About 30 individual volcanic eruptions are visible on the Methana peninsula. On the summit of the Kammeni Chora volcano you will find a crack that probably appeared during the last phase of the eruption, when the rich lava flow reached the sea. From the summit you can follow the lava flow with your eyes all the way to the sea. The sunset here is more beautiful than on Santorini. The lava glows red again in the last light of the setting sun. Methana volcano is active, however we cannot yet predict where and when the next eruption will be. The hike to the top takes about 25 minutes. Text and pictures: Elias Rizos – www.volcanotrails.gr Read about Kammeni Chora volcano on www.volcanotrails.gr SCAN ME A travel guide to Methana-topia www.volcanotrails.gr SCAN ME Map of Methe Background from 2002 Με χρώματα στp
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