The system
This page brings together the structure, movement, and scale of a spring-fed headwater landscape.
It is not a designed system.
It is a natural process that is now being observed as it re-expresses.
Time
This landscape has functioned as a headwater system over long timescales.
Historical mapping shows the presence of springs and a defined flow path across the site, indicating continuity beyond recent land use.
What is being observed today is not new.
It is the continuation of a system that has persisted through time, now becoming visible again.
Structure
This system is defined by its underlying geology and landform.
Permeable sandstone allows water to move through the subsurface before emerging where the ground surface and geology intersect.
The valley shape concentrates this movement, creating a natural pathway for groundwater to become surface flow.
This is not random.
It is the structure that determines how water behaves here.
Movement
Water moves through this system as groundwater and surface flow.
It emerges at multiple points before converging within the valley, forming a connected flow path across the site.
Movement is not linear.
It spreads, slows, gathers, and redirects depending on ground conditions and structure.
This is a dynamic system, responding continuously to rainfall, saturation, and seasonal change.
Scale
This system extends beyond what is immediately visible.
It forms part of a wider headwater network, connecting into the Brockey and the River Exe catchment.
The processes observed here operate at multiple scales, from local groundwater movement to downstream flow and water quality.
What happens within this landscape is not isolated.
It contributes to a larger system.
Response
Following the removal of agricultural pressure, the system is beginning to respond.
Water is reappearing across the landscape, with increased surface expression and connectivity.
Wetness, flow, and ecological activity are becoming more visible as underlying processes reassert themselves.
This is not restoration in the conventional sense.
It is the re-expression of a natural system that was previously suppressed.
