Find your village. Follow a valley. Get to know the rocks under your feet. Malta is small — there’s a lot to play with.
68 localities3 ways to play∞ things to notice
A little place. A whole lot of wow. ✦
Loading terrain and geological survey…
Click an area for locality details · Drag to pan · Zoom for smaller councils
Select land for a height reading
YOUR LOCAL FIELD NOTES
Click a locality. Discover its landscape.
Explore all 68 council areas, from the western plateau to Gozo’s valleys. Each area includes its region, area, neighbours, sampled elevation range, mapped rock formations and groundwater bodies.
68CLICKABLE LOCALITY AREAS
54 Malta · 14 Gozo Għajnsielem includes Comino.
THREE ISLANDS. COUNTLESS PERSPECTIVES.
Explore heights, slopes, valleys and the rock units that shape them.
DIG A LITTLE DEEPER
Meet the rocks under your feet.
Malta’s five main sedimentary formations were deposited in ancient seas. Select a layer to discover how it shapes the islands today.
Schematic sequence · youngest at top · thicknesses not to scale
THE LIVING SURFACE
Soil is more than weathered rock.
These traditional broad soil groups are an introduction. Real soil patterns vary over short distances and do not form one universal stack.
Terra rossa
Red, clay-rich soil associated with coralline limestone landscapes. Its colour comes from iron compounds.
Xerorendzina
Often shallow, calcium-rich soil associated with limestone terrain. Vegetation and local conditions affect its development.
Carbonate raw soil
Pale grey soil developed from calcareous material, including Globigerina Limestone and Blue Clay. Often rich in calcium carbonate.
WATER BENEATH THE ISLANDS
One landscape. Different water tables.
Rain can enter pores, joints and fractures in limestone. Where water accumulates depends on the rock sequence and its connection to the sea.
Mean sea-level aquifer
Fresh groundwater forms a lens above denser saline water. Its upper surface is the water table; its height and salinity vary with recharge, location and abstraction.
Perched aquifer
In some uplands, less-permeable Blue Clay holds water within the overlying limestone above the regional sea-level system. Water may emerge where these layers meet a valley side.
Coastal groundwater bodies
Smaller northern systems occur around coastal lowlands. Their geometry and seawater connection differ from the larger regional freshwater lenses.
Conceptual only · not to scale · not a cross-section of the selected locality. The groundwater map shows surface projections of aquifer bodies, not water depth.