Return to the path and continue walking down hill.
Beware of loose rocks, water and mud.
You will come to a small stream at the bottom of the hill.
There is a crossing point just to the left of the main path.
The woodlands lie on Oxford Clay, mainly on gentle to moderate slopes and encompass a system of small streams and ditches.
Valley alder wood is widespread along these streams and ditches.
The Oxford Clay Formation is a Jurassic marine sedimentary rock formation underlying much of southeast England, from as far west as Dorset and as far north as Yorkshire. The Oxford Clay is of middle Callovian to lower Oxfordian age and comprises 2 main facies. The lower facies comprises the Peterborough Member, a fossiliferous organic-rich mudstone. This facies and its rocks are commonly known as lower Oxford Clay. The upper facies comprises the middle Oxford Clay, the Stewartby Member, and the upper Oxford Clay, the Weymouth Member. The upper facies is a fossil poor assemblage of calcareous mudstones.
I'm currently looking for people who might be able to help look after my caches whilst I'm away undertaking a doctorate. If you think you might be able to help, please do let me know by contacting me at geocachingjohn@googlemail.com (If you can't help maintain them long term, it would be wonderful if you could take along some spare logs/pencils/etc. to keep these caches alive, just in case)