Leaf mold

Leaf mold (Leaf mould outside of the United States) is the compost produced by decomposition of deciduous shrub and tree leaves, primarily by fungal breakdown.
Description.
Leaves shed in autumn tend to have a very low nitrogen content and are often dry. Their main constituents are cellulose and lignin. Because of this, autumn leaves break down far more slowly than most other compost ingredients with very little bacterial decomposition involved.
Time and process.
Fungal decomposition of a heap of leaves in damp temperate climates can take between one and three years to break down into a dark brown fine powdery humic matter. A succession of different fungal species may be involved. A range of micro detritivores are also involved in converting the leaf material into a fine-grained humus, including many isopods, millipedes, earthworms, etc.
Uses.
In the natural environment, the decomposition of leaves provides a moist growing medium for young plants and protects the ground from drying out during periods of low rainfall. It is a significant component of soil organic matter, particularly in temperate deciduous woodland. The slow rate of decomposition gradually releases plant nutrients bound up in the leaves back into the environment to be re-used by plants. Autumn leaves are often collected in gardens and farms into pits or containers for the resultant leaf mold to be used later. 
Oxygen and moisture are essential for leaf decomposition. Leaf mold is not high in nutrient content but is an excellent humic soil conditioner because its structure and moisture retention provide a good growing medium for seedling roots. 
Leaves collected from roads and pavements may be contaminated by pollutants which can become more concentrated as the leaves decompose into a smaller volume 