(I): international value
(N): national value
(R): regional value

1) CHURCH OF ALBO (I): metamorphic rocks of the Ivrea Verbano Area, a geological area famous among scientists from all over the world.

2- CANDOGLIA (I): quarries for the pink marble used in Milan Cathedral.

3- PREMOSELLO (I): contact between rocks of the deep continental crust and rocks of the continental mantle, in an exceptionally rare occurrence at the Earth’s surface.

4- FINERO (I): Quarry of peridotites, rocks of the Earth's mantle: they form the mafic-ultramafic body of Finero, one of the most studied in the world.

5- SAN BERNARDINO RIVER (N): metamorphic rocks of the so-called “Scisti dei Laghi”, shaped by glacial action.

6- CADORNA ROAD: PIAN D’ARLA (I): Scisti dei Laghi and a good view-point for the Monte Zeda group.

7- PONTE NIVIA (I):  Banded amphibolites, metamorphic rocks of the Strona-Ceneri area, much studied by European scientists.

8- CADORNA ROAD: P. FOLUNGO - MT. BAVARIONE (I): around Mount Bavarione are exposed all types of rocks of the so-called “Strona-Ceneri area”, studied by many European scientists.

9- PONTE CASLETTO (I): outcrop of "Cenerigneiss", rocks derived from the metamorphism of a sedimentary rock; their complex history is still strongly debated.

10- SPOCCIA ORASSO (I): mylonites which formed along the Cossato-Mergozzo-Brissago Line, a fault developed at great depth and high temperatures.

11- SPOCCIA (I): mylonites of the Cossato-Mergozzo-Brissago Line and their relationship with the rocks of the basic intrusion (Basic Complex of the Ivrea Verbano area).

12- POGALLO VALLEY (I): mylonites formed at the Pogallo Line, a fault whose role is crucial in the interpretation of the geological history of the “Serie dei Laghi” area.

13- CASTLE OF VOGOGNA (I): mylonites here are related to the most important fault system in the Alps, the Insubric Line.

14- PREMOSELLO – VOGOGNA (I): exposed here are the so-called “fossil earthquakes”: products of instantaneous melting along fault planes triggering an earthquake.

15- SCOPETTA - old bridge over the Sesia river (I):  mylonite of the Insubric Line, the most important fault system  in the Alps.

16- BALMUCCIA (I): one of the best preserved mantle peridotites in the world.

17- VOCCA near the village of Isola (I): basic rocks deformed at high temperatures.

18- VOCCA near the bridge on the Gavala stream (I): crustal rocks incorporated in the Mafic Complex.

19 - ANICETI - VARALLO (I): the magma chamber of the Mafic Complex, where igneous structures are best preserved.

20- BOCCIOLARO (I): the magma chamber of the Mafic Complex; here the magmatic structures are stretched because they were at a greater depth.

21 - CREVOLA (I): contact between different rocks of the Ivrea Verbano area: the Basic Complex and the Kinzigitic Formation.

22- VALSESSERA - LA FRERA (R): faults that cut the rocks of the Basic Complex and other high temperature deformation structures.

23- AGNONA BRIDGE (I): mingling  of basic and acidic rocks, which were at only a few kilometers deep in the upper crust.

24 - PRATO SESIA (I): megabreccia of a caldera. It is a chaotic association of rocks, formed during the collapse of a caldera: gigantic blocks of different rocks, in a compacted tuff.

25 - PIANCONE (I): crustal rocks incorporated in the Basic Complex; inside them it is possible to find thin corundum bands.

26 - GARGALLO (I): caldera fill and caldera wall.

27 - MONTE ROSA massif and its glaciers (N): granitic massif, glaciers and related landforms.

28 - MONTE ROSA GOLD MINES (I): gold veins and ancient mining structures.

29 - STOFFUL (R): talc-bearing serpentinites,  the “soapstone” used to make pots and stoves.

30 - CIMALEGNA (N): high mountain geological-pedological track.

31 - WOLD – FUN D’EKKU (R): glaciological track. 

32 - BOCCIOLETO (R): peculiar landform and genesis of the Giavine rock Tower.

33 - UNIPIANO (R): Varallo: a glacial terrace, the remains of the valley bottom during the last glaciation.

34 - SAMBUGHETTO (N): complex of caves in the "Valley of Strona marble" and geo-paleontological museum "Bertolani", devoted to rocks, minerals and fossils of the valley.