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About Land Subsidence
This document summarizes a study on land subsidence in the Stavros-Farsala region of western Thessaly, Greece due to excessive groundwater withdrawal. Key points: - Land subsidence first appeared in 1990 due to overexploitation of groundwater, lowering water levels up to 20-40m. This caused tensile surface ruptures starting in 2002 that damaged roads and buildings. - The area has alternating permeable and impermeable sediment layers creating successive confined aquifers, initially artesian. Overpumping has caused non-reversible compaction of drained layers. - Groundwater levels dropped over 40m on average from 1972-2007, with an annual drop of 60
Detailed Information
| Author: | ['anniecv'] |
|---|---|
| Publication Year: | 2018 |
| Pages: | 8 |
| Language: | English |
| Format: | |
| Price: | FREE |
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