Impact of Urban Development on Physical and Chemical Hydrogeology

Urban environments significantly alter physical and chemical hydrogeologic settings. The physical alteration of the landscape can change recharge, groundwater flow dynamics, and local water balances. Microbial contamination of water sources due to wastewater is an everpresent threat, but contamination by metals and industrial compounds is a long-term concern in cities with industrial economies. The hydrogeologic setting and the age and wealth of a city are important factors influencing the magnitude of the impact on and the recovery of a hydrogeologic system from urban activities. Urban environments can have unique influences on water geochemistry, making delineation of site-specific urban geochemical markers necessary to quantify the extent of urban effects on water quality.

This content is for Registered members only. To subscribe, please
join one of our participating societies or contact the Editorial Team.

Login
Already a member? Log in here
Scroll to Top

December 2025 --The Variscan Orogeny in Europe – Understanding Supercontinent Formation

The Variscan orogen formed between 380 and 300 million years ago through several accretionary and collisional cycles, culminating with the construction of the Pangea supercontinent. This process occurred via sequential opening and closure of oceanic basins, synchronous detachment of Gondwana derived continental ribbons, and their outboard amalgamation onto the Laurussia margin. The Variscan orogen is rather unique compared with other orogenic belts on Earth: its overthickened and dominantly magmatic crust in the central belt, surprisingly minor mantle involvement in the magmatic and geodynamic processes, coherent and pulsed magmatism along the collision suture, and its complex accretionary history. Because its final product, Pangea, is the youngest and best-understood supercontinent on Earth, the Variscan orogeny offers clues for understanding the mechanisms of supercontinent formation.