Fluvial geomorphology is affected by physical conditions which allow its adaptation due to high dynamics and environmental influences. Fluvial morphological changes are manifested as a result of tendency of the river system to maintain its physical balance. Our study area is the upper and middle flow part of Vouraikos river and surrounding area, near the NW border of Chelmos mountain in Northern Peloponnese, near the town of Kalavrita, at an altitude of 800 m. The area is part of the Skepasto basin, constituting of a graben with a general E-W direction that was developed NW of Kalavrita. The area comprises of Mesozoic, Upper Triassic-Jurassic limestone and dolomite of the Tripolitsa unit External Hellenides and Plio-Pleistocene fluvio-lacustrine sequences, while its tectonic structure is characterized mainly by normal faults. The geomorphological landscape is characterized by alluvial deposits and important geomorphological features including fluvial terraces, alluvial fans, fluvial scarps and their main rill washes. This area has been a place of major human activity as shown by the findings of many uncovered artifacts and a settlement. Through a paleographic reconstruction, detailed field investigations, in combination with the compilation of geomorphological maps using GIS software and archaeological evidence found in the area, we attempted to reconstruct the fluvial evolution of Vouraikos river and identify the major geomorphological factors that led to, and influenced it. Finally, the link between cultural activities and sedimentary processes is also studied. The recorded environmental variations had a great impact on the geomorphological shaping and instability of Kalavrita plain and Vouraikos river and are being reflected on the buried settlement. Sediment fluxes were high enough to form strath terraces, while local tectonics aided in the strath and fill terrace creation. Smaller and younger strath terraces, formed during increased sediment supply periods, when the valley was at a higher level.
Fluvial systems are characterized by a notable variety of physical conditions that enable their adaptation to the morphological changes, due to their high dynamics combined with environmental, especially climatic, influences. Therefore, river systems that are being affected by environmental factors, reflect this influence by adjusting their channels. These adjustments are representative of the state of equilibrium of the fluvial systems and their adaptation to their changing environment [
During the middle (and part of late early) Pleistocene, the Hellenic region has undergone some major palaeogeographical alterations that had as a result the formation of intermountain basins and of the recent coastal plains and capes that we see today. The geomorphological and palaeogeographical evolution of this kind, was closely connected to the tectonic condition and geodynamics of the Mediterranean region.
The continental and marine environment in this area has evolved while affected by these palaeogeographical alterations and synchronously was also affected by the periodical Quaternary climatic oscillations in the Mediterranean [
Our study area is located approximately at N331000-E4210000 of the GGRS87 coordinate system and constitutes the upper and middle flow part of the Vouraikos river and the surrounding area, located near the NW border of Chelmos (Aroania) mountain (2341 m) in Northern Peloponnese (
The Skepasto basin constitutes a graben with a general E-W direction which was developed NW of Kalavrita town [
The aim of this paper is to reconstruct the fluvial evolution of Vouraikos river in the study area and identify the major geomorphological factors that led to, and influenced this evolution. Also, a secondary aim is to collect evidence on the environmental conditions that governed the study area and discover how the studied fluvial system was affected by the geomorphological changes that led to
channel adjustments and how these changes affected human activity. These environmental conditions reflect wider environmental and climatic changes that took place in the Mediterranean during the investigated period and as such, it can be a topic of wider interest. These tasks will be carried out with the assistance of field investigations, geomorphological mapping, archaeological evidence found in the study area and GIS analysis.
The most obvious way in which geoarchaeology may be used as tool in geomorphology is by dating the erosional and depositional events and also by identifying and reconstructing the climatic factors which influenced the study area. The study focuses especially on the period of the archaeological evidence of the 10th and the 7th century B.C. That is translated to be between Early Protogeometric Period and Early Archaic Period and coincides with the climatic changes observed during the Holocene period.
A landscape in general, is being distinguished by the characteristic morphologies that govern its’ shape. These morphologies are mainly caused by tectonic forces such as tectonic uplift, sedimentary processes like erosion and sediment transport and climate conditions. These processes formed distinctive topographic signatures [
This work focuses on the land-surface and fluvial development of the study area while taking into account the local geology and the major climatic changes that occurred during Holocene period. A paleographic reconstruction was carried out aiming at recognizing the submerged and emerged areas and at describing and interpreting the major morphological features and environmental alterations regarding the study area and especially of Vouraikos river channel. That was achieved with on the field geomorphological and geoarchaeological mapping and geoarchaeological prospecting, as we were able to take advantage of the archaeological excavations, taking place at an area of approximately 1.5 Km2.
Finally, detailed field investigations of the Holocene stratigraphy and sedimentological study in combination with map and aerial photo interpretations and the compilation of Geomorphological maps using GIS software, provided valuable information about the geomorphological evolution and features of the study area and an insight of the evolution of the Vouraikos’ river channel. The latter was achieved by using DEMs (GDEM V2) with 30-meter postings and 1 × 1 degree tiles, produced by NASA’s ASTER (Advanced Spaceborne Thermal Emission and Reflection Radiometer)-EOSIDS (Earth Observing System-Data and Information System) program.
The DEMs were checked and corrected in order to be further processed. A hydrological model in the studied area was produced using ESRI’S software package, ArcGIS and all the relevant data produced by the study were then overlain on the final map. The overlaid geology of the area was produced by field study, while taking into account the works of Poulimenos [
The study area is situated at an altitude of 800 m as a part of the Corinth Rift. It comprises of Mesozoic, Upper Triassic-Jurassic limestone and dolomite of the Tripolitsa unit of the External Hellenides and Plio-Pleistocene fluvio-lacustrine sequences. Alongside the south margin of the Corinth Rift, the intensely fragmented mountains of northern Peloponnese expose extensional half-grabens, which are bound by WNW/ESE and NNE/SSW normal faults [
The tectonic structure of Peloponnese is characterized by thrust nappes and normal faults [
The main fluvial system in the area is the Vouraikos river with its tributaries and a drain-age pattern in the study area runs SW-NE.
The area around of Skepasto village consists of Plio-Quaternary and Holocene sediments. It is believed by Poulimenos [
The geomorphological landscape is mainly characterized by alluvial deposits (
The alluvial plains in the area are becoming wider as we move towards the east. One of the important features of the Xerocampos valley (
The geomorphology of the area is directly influenced by structures formed on the bedrock and we are trying to assess how they were impacted by the changes of the climate during the Quaternary and the general tectonics of the area.
Mediterranean climate characterizes the area under study. Specifically, the period of limited precipitation, i.e. dry period, is during the summer months. Furthermore, the minimum mean temperature recording for January has a value of 4˚C and the maximum mean temperature recording for July has a value of 22˚C. The repetitiveness of numerous Holocene major scale climate change events and the important role they play to the shaping of the environment and to humans has been previously pointed out by scientists [
River terraces are landforms underlain by alluvial deposits and linked to climate change and tectonics [
This difficulty may be a result of a major change in the climate in the area [
The fluvial evolution in our study area is one important aspect in our effort to understand the background of the human settlement that was uncovered. Numerous attempts have been made, in order to cross date geomorphological, tectonic and generally geological evidence with archaeological data.
During Holocene, the study area was almost uninterruptedly inhabited where the alluvial fan is located, along the riversides of the stream. Cyclic flooding events as observed during fieldwork (
These cyclic events are also supported by the findings of Stamatopoulos & Evelpidou [
The deposits are generally very poorly sorted with an indistinctive bedding (
At present time, human activity such as the creation of irrigation channels in Xerocambos, near Skepasto village, 2 Km NW of Kalavrita town, had as a result, archaeological artefacts to be unearthed. Between the years 2001 and 2008 archaeological excavations were carried-out in an area of approximately 1.5 Km2 on the NE higher fluvial terrace of Vouraikos River. Buried archaeological artifacts such as in situ pottery and traces of a constructed settlement, which was protected by a wall, were discovered by Alexopoulou in 2009 [
The protective wall has a height of 0.80 m and a width of 2 m. The artefacts were found 1.25 - 1.8 m (
silty gravels, fluvial sediments and about 4 m higher than the present river flow bed (thalweg). According to Alexopoulou [
Knowledge of the morphochronological evolution of a study area is often difficult to assess, in view of the lack of accurate geological constraints. The presence of Plio-Pleistocene tectonic and stratigraphic products in combination with the existence of Geoarcheological data in the Kalavryta plain allows us to reconstruct the geomorphological processes.
Cyclic flooding events, triggered by climate change in the Mediterranean region and consequently in the study area, have been studied in this paper. Archaeological artifacts and findings in general, assisted to connect and analyze them chronologically with these flooding events and this relation will be analyzed in the following chapter.
Additionally, the findings have been located under a sedimentary cover with particle size, orientation, bedding, sorting, thickness and general characteristics that correspond to more than one incidents of debris flow. This deduction is being verified by numerous particles of large size (up to boulder size) that were found to be present in a matrix of smaller particles up to the size of gravel. These flooding events characterized the area geomorphologically as they were crucial to its formation and evolution. The findings also verified the age of the terraces creation.
The study area in and near Skepasto basin appeared to be full of human activity during ancient times.
That is an indication that the burial has happened as a result of flooding that forced the population to abandon the settlement [
The aforementioned settlement is situated on a preexisting alluvial fan of a probably Early Holocene age, cut by linear erosion and transformed in a terrace. The altered environmental and climatic conditions from glacial to eventually warm humid drastically reduced slope degradation processes and induced related aggradations of riverbeds. This fan was the result of post-glacial stream sedimentation due to the abundance of clastic material of glacial origin present in the valleys floor and distributed by the stream. Probably climatic variations during middle Holocene allow the stream to cut a small erosional valley in the alluvial fan and alluvial plane: the main order of terrace was formed.
The recent findings are shown in
The river bank is currently moving to the SE, affected by the local geology as shown in the reconstruction and the geomorphological and sedimentary processes of the alluvial fan, coming from a left slope direction towards the right side of the valley.
Also, the local geology of the study area is being shown as a result of map interpretation and fieldwork investigations. The former as well as the latter also revealed the existence of two large normal faults in the area. The northwest one, having a NW-SE orientation extending at a distance of 2 km. The south one, with a general direction of W-E extends at a distance of 3.2 km and cuts through Vouraikos river channel.
The area of main interest is covered with braided river and alluvial fan deposits.
The degree of the impact and the importance of the climate in relation with the geomorphological and sedimentological processes, has been under debate for quite some time [
Both aggradational (fill) and bedrock (strath) terraces occur in the study areas river network of Vouraikos. The greatest obstacle to reconstruct the timeline and extract conclusions about the creation of these terraces is that of chronology and
climate fluctuations. A terrace’s creation can be defined by its age and its position into the glacial and interglacial climatic record and by the tectonic environment into which they are being formed. Also, time and age enable age-related comparisons between strath and fill terraces and facilitates links to already documented tectonic and climatic events. It is a deciding factor to identify whether or not the terraces formed when these events took place. Strath terraces are usually maintained in better condition at higher altitudes. On the other hand, fill terraces are usually best maintained at lower altitudes [
In spite of the wide use of strath terraces in geomorphology (both fluvial and tectonic), it’s still not clear the conditions in which the planation of a strath terrace takes place. There is a difficulty to deduce the rules that govern the mechanisms of the strath terraces formation along with the duration of such processes and their exact age based solely on field investigation and observations. That is because terrace sequences are difficult to date as they constitute fragmented and incomplete records that were created in climatic, morphological and fluvial conditions that are different from the current ones.
Strath and fill terraces have been linked to peak glacial advances [
The large-scale uplift which has occurred during the Plio-Quaternary in Northern Peloponnese [
Phases of Holocene valley alluviation for many countries around the Mediterranean have been described and ascribed either to human activity and climatic change [
The climatic change in the area is directly connected to the glacial fluctuations and the topographic position of Vouraikos river in correlation with the glacial morphology.
The climatic and therefore the glacial fluctuations are recorded as advances and retreats of the ice line which in this case is rather useful as a result of the high altitude (800 m.a.s.l.) and the topography of the Kalavrita plane positioned 14 km NE of Helmos mountain.
Helmosmountain, is characterized by Tymphian [
The altered climatic conditions from glacial and periglacial to warm and humid, drastically reduced slope degradation processes and induced related aggradations of riverbeds [
It is evident that between 3000 and 2700 yrs B.P. the climate conditions in the study area were cold and humid and subsequently to this interval, the climate was rapidly warming till a warm peak around 2200 yrs B.P.
Additionally, the uplift-induced valley incision [
Successively, the study area underwent a climate change resulting to flooding events commonly present in dry warm climate conditions and intense concentrated rainfall. As consequence, high amount of sediments was deposited in episodes of concentrated rainfall and related flash flood events. Events that had as a result the burial of the human settlement.
Strath terraces are created when sediment fluxes are high enough to cover the channel bed. Additionally, discharge has to be low enough in order for the sediment not to be able to move and expose the bed to be eroded. Finally, lateral erosion has to be greater than vertical incision [
High sediment flow that was present during deglaciation period [
As it was already mentioned, the study area consists of Plio-Quaternary and Holocene sediments (braided river sedimentary sequences) and uncomfortably resting Plio-Quaternary sediments that are being covered by stream Holocene sequences. Local tectonics have an effect on the sediment supply which fluctuates along the rivers channel length along with the creation of strath terraces which are carved into the bedrock and also fill terraces. The former are created during a process that takes place as sediment flow values become lower than the ones of the transports capacity. Then, the bed is re-exposed and fluvial incision restarts, converting the strath to a strath terrace. Locally, a thin veneer of alluvium on the top of them is observed.
The bedrocks lateral erosion is the governing process and could have such a duration that is enough to produce sloping surfaces under active channels.
Given enough time, there is a possibility for pediments to form. These major strath terraces constitute the landform of the fundamental stream-terrace. Smaller strath terraces, which are more recent, formed when the river overflowed its banks and beveled the bedrock, during the aforementioned increase of the supplied sediment, while the valley was at a higher altitude.
The climatic reconstruction attempted, is also backed up by the findings of Heymann et al. [
The wet conditions, with small interruptions, continue during Mid-Holocene (8 - 5 ka B.P.) while climate conditions in area became similar to the present day after 7 kacal B.P. Human impact on sedimentary processes and dynamics in the study area becomes important during the Bronze age (after 5 ka B.P.) [
Comparing the geomorphological and archaeological data enabled us to comparatively date the fluvial forms of the study area and also enabled the stages of geomorphological evolution to be defined. Xerocambos plain in Northern Peloponnese was geomorphologically active between 10th and 7th century B.C. and was buried beneath 1.5 m thick fluvial sediments.
Before the 10th and the 7th century B.C. (Early Protogeometric Period - Early Archaic Period), the study area was generally affected by cold humid climatic conditions, like numerous other parts of Greece and the Mediterranean.
The recorded environmental variations in the general study area had a great impact on the geomorphological shaping of Kalavrita plain and especially Vouraikos river channel. The analysis identified and confirmed a shift from glacial and periglacial dry conditions to warm and humid conditions.
As a result, reduced slope degradation processes and induced related aggradations of riverbeds are the main geological processes that characterized the area. Additionally, due to the uplift-induced valley incision in combination with the climate shift, fluvial terraces were created in the area.
Subsequent widespread flooding events deposited high amount of sediments, in episodes of concentrated rainfall and related flash flood events, shaping the present-day fluvial system along with alluvial fans and terraces. This climate shift is reflected on the burying of the settlement and the findings of human activity in the alluvial deposits.
The Xerocambos settlement was surrounded by a flood-protection wall in order for structures to be protected in the case of these events [
Sediment fluxes were high enough to form strath terraces as they covered the channel bed of Vouraikos river while discharge was low enough having as a result lateral erosion being greater than vertical incision and promoted strath formation.
We also have to take the local tectonics under consideration that also affect the sediment supply and aid the strath and fill terrace creation.
The connection of cultural activities with tectonic and sedimentary processes is especially well-expressed in this study case. The characteristics of archaeological traces provide the geomorphological tools for studying post fluvial processes and hydrological conditions. Additionally, these archaeological traces can provide evidence regarding the study of the areas land use and development, reworked sedimentary deposits and most importantly, the paleoenvironment conditions of the area.
We would like to express our appreciation to Prof. Marcello Schiattarella for the fruitful and incisive discussion during the study and also for his encouragement and help to submit this work.
Stamatopoulos, L., Alevizos, G. and Evelpidou, N. (2018) Geomorphological Evolution and Fluvial System Development during the Holocene: The Case of Vouraikos River Evolution in Kalavrita Plain, Northern Peloponnese, Greece. Journal of Geoscience and Environment Protection, 6, 17-35. https://doi.org/10.4236/gep.2018.61002