Related Experiment Video
Updated: Feb 8, 2026

Testing of all Six Semicircular Canals with Video Head Impulse Test Systems
Published on: April 18, 2019
Development of ossification in the vertical semicircular canals: tomographic study
Ana Isabel Cisneros1, Marta Herreros2, Jesús Obón2
1Department of Human Anatomy and Histology, School of Medicine, University of Zaragoza, C/Domingo Miral, s/n, 50009, Zaragoza, Spain. aicisner@unizar.es.
Purpose:
To describe the ontogeny of vertical semicircular canals using computed tomography.
Materials And Methods:
We have studied 39 human fetuses aged between 17 and 38 weeks of development through multi-helicoidal CT.
Results:
The first signs of ossification in the semicircular canals, superior and posterior, are from 19 weeks of development, through two primary ossification centers in each canal, which will take part in the formation of the outer cover oriented towards the middle and posterior brain fossae, respectively. In this process it must be added the intervention of the common branch. Internal bone covers are formed by ossification of the fossa subarcuata in the superior semicircular canal, and from the compact center of the labyrinthine capsule into the posterior canal. The tomographic study has allowed us to demonstrate how ossification follows a variable rate, establishing a period between 21 and 26 weeks where there are completely closed canals with others still open to the brain fossae.
Conclusions:
The tomographic study of the semicircular canals has enabled us to establish a critical period in its ossification that could explain the etiology of the congenital-type dehiscence.
Related Concept Videos
Bone Formation by Intramembranous Ossification
The process begins when mesenchymal cells in the embryonic skeleton gather together and differentiate into osteogenic cells, which then develop into ...
Vertical Curve: Problem Solving
Introduction to Vertical Curves
Bone Formation by Endochondral Ossification
Elevation of Intermediate Points on Vertical Curves
Sight Distance in a Vertical Curve

