[136394] in SIPB IPv6
Your Future Partner Could Be in Ukraine!
daemon@ATHENA.MIT.EDU (Match Now)
Mon Jan 6 11:15:39 2025
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Date: Mon, 6 Jan 2025 17:13:29 +0100
From: "Match Now" <UkrainianLove@pianoforall.za.com>
Reply-To: "Match Now" <DreamMatch@pianoforall.za.com>
To: <sipbv6-mtg@charon2.mit.edu>
Message-ID: <35x2jbnc48ru5q0e-09f0bu56jzjyuxo5-71-254b8@pianoforall.za.com>
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Your Future Partner Could Be in Ukraine!
http://pianoforall.za.com/XGnPevnKFB_BszwkC8AILP3Xs-OXlwqh6bknJ_RcmNwyk3E
http://pianoforall.za.com/atVUnkDixUbb4p7xj3GERQFj56FAkNoUnHLjJGLZC8u5sAI
orsal of Pedro Gil covers the area from the start at Mount La Esperanza, at a height of about 750 m (2,461 ft), to the center of the island, near the Caldera de Las Cañadas, with Izaña, as its highest point at 2,390 m (7,841 ft) (MSLP). These mountains have been created due to basaltic fissural volcanism through one of the axis that gave birth to the vulcanism of this area.
The Abeque Dorsal was formed by a chain of volcanoes that join the Teno with the central insular peak of Teide-Pico Viejo starting from another of the three axis of Tenerife's geological structures. On this dorsal we find the historic volcano of Chinyero whose last eruption happened in 1909.
The South Dorsal or Dorsal of Adeje is part of the last of the structural axis. The remains of this massive rock show the primordial land, also showing the alignment of small volcanic cones and rocks around this are in Tenerife's South.
Valleys and ravines
Valleys are another of the island's features. The most important are Valle de La Orotava and Valle de Güímar, both formed by the mass sliding of great quantities of material towards the sea, creating a depression of the land. Other valleys tend to be between hills formed by deposits of sediments from nearby slopes, or simply wide ravines which in their evolution have become typical valleys.
Tenerife has a large number of ravines, which are a characteristic element of the landscape, caused by erosion from surface runoff over a long period. Notable ravines include Ruiz, Fasni
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<div style="color:#fefefe; font-size:8px;visibility:hidden;">orsal of Pedro Gil covers the area from the start at Mount La Esperanza, at a height of about 750 m (2,461 ft), to the center of the island, near the Caldera de Las Cañadas, with Izaña, as its highest point at 2,390 m (7,841 ft) (MSLP). These mountains have been created due to basaltic fissural volcanism through one of the axis that gave birth to the vulcanism of this area. The Abeque Dorsal was formed by a chain of volcanoes that join the Teno with the central insular peak of Teide-Pico Viejo starting from another of the three axis of Tenerife's geological structures. On this dorsal we find the historic volcano of Chinyero whose last eruption happened in 1909. The South Dorsal or Dorsal of Adeje is part of the last of the structural axis. The remains of this massive rock show the primordial land, also showing the alignment of small volcanic cones and rocks around this are in Tenerife's South. Valleys and ravines Valleys are another of the island's features. The most important are Valle de La Orotava and Valle de Güímar, both formed by the mass sliding of great quantities of material towards the sea, creating a depression of the land. Other valleys tend to be between hills formed by deposits of sediments from nearby slopes, or simply wide ravines which in their evolution have become typical valleys. Tenerife has a large number of ravines, which are a characteristic element of the landscape, caused by erosion from surface runoff over a long period. Notable ravines include Ruiz, Fasni</div>
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