Cancellous bone, sometimes known as trabeculated or spongy bone, is composed of interconnected plates of bone tissue with large spaces between the plates of bone
The plates of bone contain osteocytes located within lacunae
The osteocytes in each lacuna are connected to each other, and to the osteoblasts on the surface of the plate, by cytoplasmic processes which run in small channels (canaliculi) in the bone matrix
These processes connect the osteocytes within the plate of bone to the osteoblasts on the surface
Blood vessels run adjacent to the surface of the plates of bone
As in compact bone, these associations provide the route through which nutrients are distributed throughout the bone tissue
Cancellous bone is typically found in the epiphyses of long bones
The plates of bone are not randomly organised but are orientated to provide support against the stresses that are applied to the region of bone in which they lie
Like compact bone, cancellous bone is continually being broken down and replaced as part of the maintenance of the bone tissue
If different stresses become applied to a region of bone, new replacement bone will align with the lines of stress present at the time
In life, the spaces between the plates of bone, in cancellous bone, contain bone marrow