The Old Lines Still Hold — Part 7: The Terrain Sets the Terms

The ride covered 25.5 km with 600 m of ascent and 610 m of descent, set along a rolling multi-sector loop linking coastal approaches, intermediate ridge systems, agricultural terraces, drainage lines, and repeated short climbs across the Apokoronas basin. Moving time totalled 1:47:53, with an ascent time of 1:02:06 and descent in 0:43:59. Gradients reached +19.9% on the steeper sections and –19.7% on the descents. Maximum speed recorded was 44.4 km/h, averaging 14.2 km/h across compact gravel, embedded limestone, exposed bedrock, agricultural tracks, erosion channels, concrete ramps, olive grove access roads, and secondary tarmac, with 70% off-road. It was a stepped route — seven distinct climbs distributed across multiple terrain compartments, each separated by descents, transitions, and changes in visibility. Nothing sustained for long, but very little of the route came without effort.

Climb profile (summary):

7 climbs | Total structured effort

Longest: C5 – 1.9 km @ 3.9%
Steepest: C3 – 19.9%
Final: C7 – 1.6 km @ 7.0%
Climb profile (C1–C7)

C1: 0.5 km | 0.0% | +16.1%
C2: 0.7 km | -1.6% | +10.0%
C3: 0.9 km | -6.6% | +19.9%
C4: 1.1 km | -2.4% | +18.2%
C5: 1.9 km | -19.7% | +13.5%
C6: 0.4 km | -1.2% | +13.7%
C7: 1.6 km | -12.5% | +17.6%

I left Kokkino Chorio and climbed towards Kambia under clear morning skies. The route immediately began to reveal the character of the day. Nothing here followed a straight line for long. The ground rose and fell in a series of ridges, folds, terraces, and drainage lines, each imposing its own conditions upon movement. Before long I reached the descent of Four Hills Climb, dropping away from the higher ground towards the network of tracks below.

From Four Hills the route entered Aspro Tracks. The surface alternated between compact gravel and embedded limestone, allowing speed in places while demanding concentration in others. The line ahead was never entirely obvious. Small changes in contour altered both traction and visibility. Sections that appeared straightforward from a distance often concealed loose stone, erosion channels, or abrupt transitions in gradient.

St Basil's Track carried the route onwards towards Gavalochori. Dry stone walls bordered sections of the track, dividing olive groves that have shaped this landscape for generations. Here the agricultural character of Apokoronas becomes particularly evident. The land is worked, inhabited, and productive, yet the terrain continually interrupts direct movement. Terraces, folds in the ground, and changes in elevation repeatedly break line of sight.

Crossing Gavalochori, I joined Slabs Track. Exposed limestone dominates this section, with bedrock surfacing through the soil to dictate the available lines. The terrain determines where wheels can travel just as surely as it once determined where animals and people could move. Progress is shaped by the ground itself rather than by intention alone.

The route then climbed towards Almyrida before turning inland once more. Looking back, the coastline remained visible, but only intermittently. One ridge would reveal the sea, the next would hide it. This constant alternation between exposure and concealment became one of the defining characteristics of the ride.

Roller Coaster followed. The name is entirely appropriate. Short climbs were followed by short descents, each demanding renewed effort before momentum could fully develop. The terrain offered no sustained ascent and no prolonged recovery. Every gain was temporary. Every descent eventually led towards another rise.

From Roller Coaster the route crossed the Olive Grove sector before beginning the reverse climb towards Prophet Elijah. The church occupies a commanding position above the surrounding landscape. From here the structure of Apokoronas becomes easier to appreciate. The basin is not a single geographical unit but a collection of smaller terrain compartments connected by ridges, terraces, valleys, and agricultural corridors.

The route continued onto Tony's Gully Ascent before linking towards Douliana. The climbs here were steeper and more confined. Vegetation, walls, and terrain features reduced visibility while simultaneously creating multiple route options. The line never remained obvious for long.

Eventually I returned to Gavalochori for coffee before retracing sections of Aspro Tracks and beginning the ascent of Four Hills Climb. The return journey reinforced many of the observations made earlier in the ride. Routes that appeared straightforward on the map revealed themselves to be a sequence of linked terrain problems once ridden on the ground. Each climb altered perspective. Each descent revealed another fold in the landscape.

By the end of the ride the central characteristic of Apokoronas had become clear. This is neither mountain country nor lowland plain. It is a landscape divided into interconnected compartments. Coastal shelves, intermediate ridges, agricultural terraces, drainage systems, and small valleys combine to create a terrain that continually shapes movement.

Historically, this is important.

During the Ottoman period, the Cretan revolutions of 1821, 1866–69, and 1897, and later during the German occupation, movement across Apokoronas rarely followed the most obvious route. Main roads could be watched. Valley floors could be controlled. The intermediate ground between them offered alternatives.

The terrain around Kambia, Gavalochori, Douliana, and the surrounding ridges demonstrates this clearly. A person moving through the area can pass repeatedly between observation and concealment. One ridge provides extensive views across the basin; the next drops into a hollow where movement becomes difficult to detect. A terrace line offers a route across a hillside; a drainage channel provides another option entirely.

The result is a landscape of fragmented visibility. Control of one sector does not automatically provide control of the next. The ground itself interrupts observation, movement, and communication.

This helps explain why Apokoronas appears so frequently in the history of Crete. The area was not merely a place through which people travelled. It was a place where movement could be managed, redirected, concealed, or sustained according to circumstance. Villages remained connected through networks of tracks and routes that often avoided the most exposed ground.

The Constitution of Armenoi, agreed in May 1822 within the wider Apokoronas region, illustrates the significance of this landscape. Representatives from across the island were able to gather because the geography supported communication while providing a degree of security. The terrain that sustained resistance also enabled organisation.

The same principle remained relevant more than a century later. Resistance couriers, local guides, and SOE personnel operating in western Crete depended upon knowledge of ridges, terraces, observation points, dead ground, and alternate routes. Success often depended less upon secrecy than upon understanding the landscape better than those attempting to control it.

Riding through Apokoronas today does not recreate those experiences, but it does reveal the physical realities that shaped them. Every climb reveals another ridge. Every descent enters another compartment. Every apparent line of travel breaks into alternatives.

The old lines still hold because the ground itself has changed very little. Roads have been surfaced, vehicles have replaced mules, and modern navigation has replaced local memory for many travellers, yet the ridges remain where they always stood. The valleys still interrupt movement. The terraces still shape the available routes.

The terrain sets the terms.

It always has.