AnatoMemory

Organ

Arachnoid granulations

Arachnoid projections associated with CSF outflow

Head & neckNervous system

High-yield

Granulations are part of the anatomy of CSF outflow, but drainage also involves pathways associated with cranial nerves and meningeal lymphatics.

Overview

Arachnoid granulations project toward dural venous spaces, often near the superior sagittal sinus and its lateral lacunae. They have traditionally been described as a route for cerebrospinal fluid to enter venous blood. Their structure and exact contribution to total drainage are more complex than a simple valve model.

Reference facts

Location
At the arachnoid–dura interface, including projections into venous sinuses and lateral lacunae, especially near the superior sagittal sinus
Parts
Microscopic arachnoid villi and larger granulations; size, shape and distribution change with age
Blood supply
Generally considered avascular, although rare capillaries have been demonstrated in the connective-tissue core of some granulations
Function
Associated with transfer of CSF toward venous and perisinus spaces; their share of total outflow remains under study

Clinical correlation

Subarachnoid bleeding or meningitis can impair CSF circulation and absorption, causing communicating hydrocephalus. This cannot always be reduced to scarring of granulations alone.

Frequently asked questions

Where are the arachnoid granulations located?

At the arachnoid–dura interface, including projections into venous sinuses and lateral lacunae, especially near the superior sagittal sinus.

What do the arachnoid granulations do?

Associated with transfer of CSF toward venous and perisinus spaces; their share of total outflow remains under study.

What are the parts of the arachnoid granulations?

Microscopic arachnoid villi and larger granulations; size, shape and distribution change with age.

What is the blood supply of the arachnoid granulations?

Generally considered avascular, although rare capillaries have been demonstrated in the connective-tissue core of some granulations.