"Settsas" roundtour

Category
Hiking trail
Difficulty
Medium
Duration
4.1
Duration in hours
Distance
10.4
Distance in km
Region
Arabba

Details

The "Settsas" massif is a milestone in the history of geology, as it is one of the first explored areas in the Dolomites and is also called the "Richthofen" reef.

The name derives from Baron "Richthofen" who, interested in the geology of the Dolomites, discovered in 1800 that the "Settsas" is nothing other than a coral reef. This mountain is very important from a geological point of view because it preserves the geometry of two reefs from the Triassic period (23 m.a.) with the fossil underwater ramps and the connection with the deep sea deposits that surrounded them, the " S.Cassiano" formation.

At that time they were in tropical latitudes and thanks to plate tectonics they have moved to where we see them now.

The researches of Baron "Richthofen" had fundamental importance, as much as they allowed to give bodies to the tectonics of the plates, according to which the parts of the rocky crust that cover the planet can move, in the geological ages, even of thousands of kilometres from the place where they are formed.

MORE INFO :   

  • "Settsas" became a UNESCO patrimony in 2009 and is part of system n.5   
  • "Settsas" consists of two ancient atolls, "Settsas" and "small Settsas".

Rating

Stamina
Experience
Landscape

Best time of year

JAN
FEB
MAR
APR
MAY
JUN
JUL
AUG
SEP
OCT
NOV
DEC

The tour in numbers

10.4
Distance in km
4.1
Duration in hours
550
Ascent
569
Descent
2055
Lowest point
2385
Highest point

Description

The "Settsas" massif is a milestone in the history of geology, as it is one of the first explored areas in the Dolomites and is also called the "Richthofen" reef.

The name derives from Baron "Richthofen" who, interested in the geology of the Dolomites, discovered in 1800 that the "Settsas" is nothing other than a coral reef. This mountain is very important from a geological point of view because it preserves the geometry of two reefs from the Triassic period (23 m.a.) with the fossil underwater ramps and the connection with the deep sea deposits that surrounded them, the " S.Cassiano" formation.

At that time they were in tropical latitudes and thanks to plate tectonics they have moved to where we see them now.

The researches of Baron "Richthofen" had fundamental importance, as much as they allowed to give bodies to the tectonics of the plates, according to which the parts of the rocky crust that cover the planet can move, in the geological ages, even of thousands of kilometres from the place where they are formed.

MORE INFO :   

  • "Settsas" became a UNESCO patrimony in 2009 and is part of system n.5   
  • "Settsas" consists of two ancient atolls, "Settsas" and "small Settsas".

Similar routes nearby

These tours would be interesting for you
Valparola - Setsas - Palongiá - San Cassiano
Panoramic Tour
Medium
4.3
Duration in hours
13.8
Distance in km
Sass de Stria
Panoramic Tour
Medium
2
Duration in hours
2.5
Distance in km
Lagazuoi Kaiserjäger
Panoramic Tour
Difficult
2.8
Duration in hours
5.4
Distance in km
Panoramic Tour
Easy
2
Duration in hours
2.1
Distance in km