fliš

Flysch – term, characteristics, weathering…

Flysch is a term for sedimentary rock sequence, deposited in a deep basin formed on the continental edge of mountain mass. Flysch sequence is characterized by progressive deposition of deep-water turbidite sediments up to shallow-water shales (claystones and siltstones) and sandstones.

Considering the area of Croatia, flysch sediments are deposited within alpine orogenesis, which formed existing mountain masses within European and Asian continents, from the Pyrenees to the west all the way to Himalaya to the east, including Alps and Dinarides. Continental edges of newly formed mountain masses are characterized by flysch deposits, which in Croatian area can be tracked along narrow strips from northern Istria all the way to Dubrovnik towards the southeast.

fliš alpidski pojas
Figure 1. Stretching of „alpine belt“ as a result of alpine orogenesis, characterized by the appearance of flysch deposits

Flysch deposits mostly consist of a continuous alteration of sandstone and shale layers, while turbidite breccia and conglomerates are often found at the bottom of flysch sequence. Flysch shales and sandstones consist mostly of quartz or calcite grains. Calcitic shales are commonly known as marls. Limestones and carbonate breccias are often inlayed within the flysch sequence, as a result of local sedimentation environment changes.

Geomechanical characteristics of flysch rock mass

Flysch rock mass is characterized by extreme lithological heterogeneity, as a result of frequent vertical and lateral lithological differentiation, which makes the flysch rock mass unevenly weathered. This occurs due to shales susceptibility to weathering, while sandstones and carbonates are highly resistant to weathering. Individual lithological members of flysch rock mass belong to poor to wellpetrified rocks.

Intensive weathering of flysch rock mass causes shales to relatively quickly disintegrates into clay and silt sediments, making the rock mass itself geomechanically interchange between extremely weak rock and cohesive soil. This process is common in the upper flysch layers due to surface weathering, while in the lower layers it is caused by underground water flow.

Opposed to shales, sandstones represent hard rocks, resistant to weathering and erosion and are often found as fragments in the muddy matrix due to more intensive weathering of surrounding shales.  

Hydrogeologically, flysch rock mass as a whole represents impermeable medium, with the possibility of forming smaller aquifers and springs within cracked sandstones or carbonate inlays.

Civil-engineering in flysch

Along lithological composition, stability of flysch rock mass is also influenced by its layers orientation and thickness, alteration rate of shales and sandstones, tectonical disturbance, weathering and underground waterflow intensity.

While performing excavations (open pit, cutting) within flysch rock mass, layers orientation and thickness, as well as alteration rate of shales and sandstones greatly influence structural instabilities due to differential weathering and erosion, which causes degradation of geomechanical characteristics of shales and destabilization of sandstones and carbonates. Tectonical disturbance has most impact on shales, often forming so called „milonite“ zones with foliations following the orientation of tectonic movements.

Underground water flow has a tendency to travel through semipermeable sandstone layers, and at the same time weathering and eroding bordering shale layers. Due to intensive weathering and/or underground water flow, flysch deposits consisting mostly of shales have a tendency to gradually degrade to muddy soil, which is susceptible to differential ground settlement, or sliding on the steeper ground as well as excavation edges.

pokos u ritmičkim izmjenama suhhorizontalnih slojeva lapora
Figure 2. Slope formed in thin subhorizontal marl and sandstone layers in quick alteration rate, next to railroad section Buzet – Lupoglav; locality Raspadalica
zasjek u laporima i mjere zaštite Roxanich
Figure 3. Open excavation in massive marls with rare sandstone layers (left picture) and open pit protection within flysch rock mass (right picture); locality: wine cellar Roxanich, Motovun
Zasjek u strmo nagnutim naslagama pješčenjaka
Figure 4. Open excavation in steeply oriented sandstone layers with rare marl layers: locality: Miškovići, island of Rab
Primjer nestabilnosti fliških pokosa
Figure 5. Flysch rock mass instability example – rockfall and sliding of massive sandstone blocks due to differential weathering and erosion of surrounding marls; locality: spring of Rječina
 fliš primjer nestabilnosti
Figure 6. Flysch rock mass instability example – the toppling of thin-layered marls within lower-unprotected part of open pit excavation, leaving the upper sandstones (on picture protected with concrete and anchors) in serious overhang; locality: island of Rab

Differential weathering of alternating lithological members within flysch rock mass forms a complex geological environment, which often causes problems in civil-engineering, especially regarding foundations and excavations. To avoid the aforementioned negative outcomes, special care is needed when building on flysch built terrains.

Read more: How to determine the age of a rock?

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