The best running trails around Sant Vicenç De Montalt

The true epicenter of Maresme enduro. Once you reach the top, it's time to switch gears: you're at the highest point of the system, and a labyrinth of trails and tracks of all levels unfolds before you. There are no rules here: from this central hub, you can drop down towards Sant Vicenç, Llavaneres, Can Boada, Massuet, or wherever your heart desires. Every direction offers a different descent, and all connect to legendary Maresme lines. A word of advice: when you reach Turó de l’Oriola, take a deep breath… and prepare to go wild, because this is one of the few places where you can literally ride down wherever you want.

The true epicenter of Maresme enduro. Once you reach the top, it's time to switch gears: you're at the highest point of the system, and a labyrinth of trails and paths of all levels unfolds before you. There's no instruction manual here: from this central hub, you can drop down towards Sant Vicenç, Llavaneres, Can Boada, Massuet, or wherever your heart desires. Every direction offers a different descent, and all connect to legendary Maresme lines. A word of advice: when you reach Turó de l’Oriola, take a deep breath… and prepare to go wild, because this is one of the few places where you can literally ride down wherever you want. A perfect spot to get lost—but in a good way.

The peak of Turó de L'Oriola presents rock formations distributed among the trees in the area.

Very busy weekend. https://youtu.be/7Spm5VJYhcw

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It is a large granite block located between Turó de Montalt (596 m) and Turó del Mig (550 m), a hill where the municipal limits of Arenys de Munt, Dosrius and Sant Vicenç de Montalt meet. Of the two stones, the smaller one has an engraving that seems to represent a horseshoe, although the meaning is unknown. It could be, for example, a mark to delimit the old parishes. Granite is a hard rock, with a granular texture, which in the Maresme has been used for construction. Fresh granite is known as "snake's eye" as it is made up of a black mica which, in contrast to the other components, is reminiscent of a snake's eye. In this environment and during the next section of the route, we will find small accumulations of granite blocks, disordered, heterometric and rounded, which accumulate in a horizontal or slightly inclined relief. These capricious formations have their origin in weathering. Later, the rainwater dissolves the feldspar and the large initial rock cracks and gives rise to rounded shapes and a kind of sand, called "sauló" in Catalan.

El Montalt is a mountain belonging to the Catalan coastal range, within the Sierra del Corredor and the protected natural area in which it is included. A few kilometers from the coast, the top is surrounded by forest. A common point to face the final meters of ascent is the Coll de la Ferradura, a pass located to the northeast. It is a crossroads of different paths and forest tracks and, from this point, the path to the summit is narrow and has a very steep slope. The northern slope enters completely into the natural park, with different plateaus, other peaks and the Creu de Rupit, an outstanding cross in the middle of the path. To the northeast is the Sanctuary of the Corridor, with a car park and a tourist service office. From this point, through forest tracks, To the south, we find two towns, Sant Andreu de Llavaneres and Sant Vicenç de Montalt, well connected by tracks and paths. In the same way possible starting points for the ascent, to the west is the municipality of Dosrius and its population center of Canyamars, while to the east is the town of Arenys de Munt. On the other hand, the first stage of the Camino del Norte, or GR 83 long-distance path, which begins in the town of Mataró, passes very close, along its northern slope. Its top houses a geodesic vertex and a mailbox, offering magnificent views of the entire Maresme coast.

In the surroundings of the "Pedra de la Ferradura" we can find small accumulations of granite blocks, disordered, heterometric and rounded, which accumulate in a horizontal or slightly inclined relief. These capricious formations have their origin in weathering. Later, the rainwater dissolves the feldspar and the large initial rock cracks and gives rise to rounded shapes and a kind of sand, called "sauló" in Catalan.