Kyloe Out

The rock has been repeatedly saturated over the past two weeks (39.2mm June 1–4, then further rain on June 6–11 totalling ~10.6mm), with only three genuinely dry days (June 12–14) before today's light rain — internal moisture levels will remain critically high despite any surface drying.

The three dry days on June 12–14 brought strong westerly winds (34–38 km/h) and lower humidity (~68%), which will have dried the surface effectively, but this is insufficient to draw out the deep internal moisture from the prolonged saturation period — and today's 0.6mm plus forecast rain resets even that limited surface drying.

With the sandstone likely still well above 1% internal saturation after weeks of repeated wetting, compressive strength will be significantly reduced, making hold breakage a real risk especially on the small iron-oxide features that characterise Fell Sandstone.

Early June in Northumberland has delivered below-average temperatures and above-average rainfall this year; while days are long and the SW aspect gets reasonable sun hours, the cool, humid conditions have severely limited drying potential.

The rock is almost certainly saturated internally: 39.2mm fell over June 1–4, followed by repeated light rain events through to today's 8.6mm, giving zero consecutive fully dry days and no opportunity for the deep moisture to evaporate.

Despite the SW aspect and exposed wind position (winds 19–35 km/h recently), the absence of any dry spell longer than a single day since May 30 means surface drying has been repeatedly reset, and deep capillary moisture from the heavy June 1–4 rain remains trapped within the stone.

With internal saturation likely well above the critical 1% threshold, compressive strength could be reduced by 10–50%, making hold breakage a serious risk on these iron-oxide-cemented Fell Sandstone features.

Early June should offer reasonable drying conditions with long daylight hours and moderate temperatures (14–17°C), but the unusually wet spell has overridden seasonal advantages; once a sustained dry window arrives, 2–3 days should suffice given the exposed aspect.

The rock is almost certainly saturated to depth: 39.2mm fell between June 1–4, followed by only brief trace-dry spells with further light rain on June 6–9, giving no opportunity for meaningful drying.

Despite the SW aspect and exposed position, the persistent rain and elevated humidity (averaging 77% over the last week) have prevented any significant drying; cumulative wetting far outstrips any evaporation that occurred during the short dry gaps.

With the sandstone deeply saturated, compressive strength will be reduced by up to 30–50%, making hold breakage and grain loosening a serious risk — climbing now could cause permanent, irreversible damage to routes.

Early June temperatures (~13–15°C) are moderate and helpful for eventual drying, but the current unsettled pattern with frequent frontal rain is preventing any sustained drying window from developing.

With 35.4mm of rain in the last 7 days — including significant events on June 1st (7.4mm), 2nd (13.2mm), 3rd (8.1mm), 4th (10.5mm), and today (3.1mm) — the Fell Sandstone is almost certainly saturated well beyond the critical 1% threshold at which significant strength loss begins.

The only dry day in the past week was June 5th (with strong 30 km/h SW wind), but this single day was immediately followed by trace rain on the 6th and 7th and heavier rain today, meaning no cumulative drying has occurred; the rock has been repeatedly re-wetted before any meaningful internal drying could take place.

At likely saturation levels of 60%+ after this prolonged wet spell, compressive strength may be reduced by 30–50%, creating a serious risk of hold breakage on the small iron-oxide-cemented features that Fell Sandstone climbing depends on.

Early June temperatures (averaging ~13°C) and moderate humidity (~78%) provide only modest evaporative potential; while freeze-thaw is not a concern at this time of year, the cumulative wetting from a very wet late-May/early-June period means internal moisture will take several dry days to dissipate.

With 39.7mm of rain in the past 7 days — including a heavy 13.2mm on June 2nd, 8.1mm on June 3rd, and 10.5mm on June 4th — the sandstone will be deeply saturated well beyond the surface, likely exceeding the critical 60% pore saturation threshold internally.

Only 2.5 truly dry days have elapsed since the last significant rain (June 4th), with today showing trace precipitation and humidity averaging 81% over the past week; even with the exposed SW aspect and moderate wind, this is far short of the 48–72+ hours of genuinely good drying conditions needed after heavy rain.

At current internal saturation levels, compressive strength is likely reduced by 30%+ and iron-oxide cemented holds are at serious risk of breakage — climbing now would risk both injury and permanent route damage.

Early June temperatures are moderate (13–16°C) which supports some drying, but the persistent high humidity and ongoing unsettled weather pattern are preventing effective moisture removal from the rock.

With 41.7mm of rain over the past seven days — including 10.5mm as recently as June 4 and 1.2mm today — the rock is almost certainly saturated well beyond the critical ~1% threshold at which significant strength loss begins.

Despite the favourable SW aspect and exposed position, only one dry day (June 5) has occurred since the heavy rain sequence, and today brought further precipitation; at 80% average humidity and ~14°C, drying rates are far too slow to have meaningfully reduced internal moisture.

At the current saturation level, Fell Sandstone could be experiencing 30–50% compressive strength loss, creating serious risk of hold breakage on the small iron-oxide-cemented features that characterise these routes.

Early June should offer reasonable drying potential, but the current unsettled pattern with above-average humidity and below-average temperatures for the season is suppressing evaporation and keeping the rock in poor condition.