The lateral cuneiform is one of the three cuneiform bones in the foot, located between the intermediate cuneiform and the cuboid bone, playing a crucial role in the stability and function of the foot arch. It articulates with four other bones and serves as an attachment point for several ligaments and tendons, contributing to foot movements and weight distribution during walking and running.

Lateral Cuneiform

Cuneiform bones are a group of three wedge-shaped bones located in the midfoot, playing a crucial role in the stability and arch formation of the foot. These bones, named the medial, intermediate, and lateral cuneiforms, articulate with the navicular bone proximally and the first three metatarsals distally, facilitating movement and weight distribution during walking and running.

Cuneiform Bones

The intermediate cuneiform is one of the three cuneiform bones located in the midfoot, playing a crucial role in the stability and function of the foot by articulating with the navicular bone proximally and the second metatarsal distally. It is essential for the proper distribution of weight and flexibility during movement, contributing to the foot's arch structure and overall locomotion efficiency.

Intermediate Cuneiform

The cuboid bone is one of the seven tarsal bones in the human foot, located on the lateral side and playing a crucial role in stabilizing the foot and facilitating movement. It serves as a critical component in the foot's arches and is involved in the articulation with the fourth and fifth metatarsals, the calcaneus, and the lateral cuneiform bones.

Cuboid Bone

Stability of the foot arch

Function of the foot arch

Articulation with bones

Attachment point for ligaments

Attachment point for tendons

Foot movements

Weight distribution refers to how weight is spread across an object or system, impacting its balance, stability, and performance. Understanding weight distribution is crucial in fields like engineering, transportation, and sports, where it influences design, safety, and efficiency.

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