The lecture focuses on the bony architecture of the pelvis and upper thigh, specifically the osteology of this region, including the proximal femur (thigh bone) and the pelvic bones.
The pelvis is discussed to provide a complete picture of the lower limb, even though a detailed examination of the pelvis will occur later in the course.
The hip joint discussion is deferred to a later session, but clinical implications, such as hip fractures, will be addressed.
The os coxa forms the bony pelvis and acts as a wedge-shaped stone in the superolateral portion of the arch, similar to how the sacrum serves as the keystone.
The os coxa is composed of three separate bones that fuse in the third decade of life: the ilium, ischium, and pubis.
The ilium is the largest and most superior of the three bones.
The ala (wings) of the ilium project laterally, forming the iliac crests, which serve as attachment points for abdominal musculature.
The iliac crests terminate in the anterior superior iliac spine (ASIS) and posterior superior iliac spine (PSIS), which are also muscle attachment sites.
Below these are the anterior inferior iliac spine and posterior inferior iliac spine, additional sites for muscle attachments.
The auricular surface of the ilium articulates with the sacrum medially. Its irregular convolutions minimize joint movements.
The ilium fuses with the other pelvic bones at the acetabulum, the socket for the head of the femur.
The acetabulum includes:
The articular lunate surface: makes direct contact with the head of the femur.
The acetabular fossa: opens inferiorly as the acetabular notch, which is separated from the head of the femur by a small gap.
The ischium is located posteriorly and fuses at the acetabulum.
Key structures include the ischial tuberosity.
The ischial ramus projects anteriorly, laterally, and inferiorly towards the acetabulum.
The pubic bone is located anteriorly.
The body of the pubis lies anteriorly with superior and inferior rami projecting towards the acetabulum and the ischial ramus, respectively.
These rami form the obturator foramen, which facilitates neurovascular communication with the medial compartment of the thigh.
The collective protrusions and processes of the os coxae will be identified in small group osteology sessions and discussed in relation to muscle attachments.
The sacroiliac joint, located between the sacrum and ilium, has limited motion and plays a role in shock absorption from ground reaction forces during walking and running and helps resist pelvic fractures.
It consists of two parts:
Anteriorly: a synovial joint between the ilium and sacrum.
Posteriorly: a syndesmosis, where bone tuberosities are connected through thick ligaments without a true joint space.
The sacroiliac joint is reinforced by intrinsic and extrinsic ligaments, including:
Deep interosseous ligaments: bind the posterior tuberosities.
Posterior sacroiliac ligaments: provide additional reinforcement.
Anterior sacroiliac ligaments: reinforce the anterior synovial joint.
Iliolumbar ligaments.
Sacrospinous ligament: runs from the sacrum to the ischial spine.
Sacrotuberous ligament: runs from the sacrum to the ischial tuberosity, blending with the common hamstring origin.
The fifth lumbar vertebra and axial load are anterior to the sacroiliac joints, creating a tendency for the sacrum to rotate anteriorly relative to the ilium.
The sacrospinous and sacrotuberous ligaments resist this rotation by anchoring the posterior aspect of the sacrum to the inferior aspect of the pelvis.
The greater sciatic notch on the posterior surface of the ilium and ischium is transformed into the greater sciatic foramen by the sacrospinous and sacrotuberous ligaments.
The lesser sciatic notch, inferior to the ischial spine, becomes the lesser sciatic foramen due to the same ligaments.
These foramina allow passage of muscles and neurovascular components between the pelvic cavity and the gluteal region.
The obturator foramen is mostly closed by the obturator membrane, which provides a site for muscle attachment, leaving the obturator canal for passage of the obturator nerve and vessels.
The lecture discusses the prominent features of the femur, even though the distal components will be addressed later.
Head of the femur: directed superomedially towards the acetabulum.
Neck of the femur: elongated compared to the anatomical neck of the humerus, compensating for the depth of the acetabulum.
Greater and lesser trochanters: oblique bony masses serving as muscular attachment sites.
Shaft of the femur: angles down towards the knee.
Gluteal tuberosity: on the posterior surface, serves as an attachment point for the gluteus maximus muscle.
Linea aspera: a prominent ridge of bone on the posterior surface, serving as an elongation site for numerous muscle attachments.
Femoral condyles: articulate with the tibia to form the knee joint.
Epicondyles: located near the condyles, serve as sites for tendon and ligament attachment.
Adductor tubercle: proximal to the medial epicondyle, allows attachment of a prominent muscle in the medial compartment of the thigh.
Angle of inclination: the angle between the neck and shaft of the femur in the coronal plane, typically between 120 and 135 degrees.
Coxa valga: a higher angle of inclination, common in young individuals.
Coxa vara: a smaller angle of inclination, common in the elderly and a confounding factor in hip fractures.
Torsion angle: the degree to which the neck projects posteriorly relative to the femoral shaft in the transverse plane.
A hip fracture is a general term for any fracture to the femoral neck or proximal shaft of the femur, often outside the joint capsule.
Radiography confirms the fracture and misalignment of the fractured heads.
The distal end is typically displaced superiorly due to muscle contraction and laterally rotated due to muscle imbalance.
Patients present with severe pain in the lateral pelvic region and inability to bear weight on the affected limb, which appears shortened and laterally rotated.
Distal fractures can be surgically corrected with rods and plates.
Fractures affecting the articular surface or complicated by osteoarthritis may require a total hip replacement.
Hip fractures are common in the elderly due to loss of bone mineral density.
The femur consists of outer cortical bone and inner cancellous bone.
Cancellous bone's porous nature reduces the overall weight of the bone.
Bone mineralization follows the compression and tension lines of force in a weight-bearing position.
Loss of bone mineralization and organic collagen matrix makes bones brittle and subject to fracture.
Deficient bone mineral density in younger populations is less likely to cause fracture due to a higher concentration of organic matrix, which provides flexural strength.
Selective loss in bone mineralization without loss of organic matrix makes the bone more flexible than brittle.
Severe bone demineralization, as seen in rickets (associated with vitamin D deficiency), can cause permanent bowing of weight-bearing structures.