Corrie of Inchdowrie

Corrie of Inchdowrie, located in Angus, Scotland, is a striking example of a glacial valley, commonly known as a corrie. Nestled within the Grampian Mountains, this geological feature is a result of glacial erosion during the last ice age.

The corrie is situated at an elevation of approximately 400 meters above sea level and is surrounded by steep, rocky slopes. Its distinctive U-shaped profile is a testament to the immense power of the glacier that once occupied this region. The glacier slowly carved out the corrie by grinding and scouring the bedrock, leaving behind a deep, amphitheater-like hollow.

Corrie of Inchdowrie is approximately 300 meters in diameter and is characterized by its steep back wall, known as a headwall, which rises to a height of nearly 100 meters. The headwall is composed of rugged cliffs and scree slopes that were formed by the deposition of debris as the glacier retreated.

The valley floor of Corrie of Inchdowrie is relatively flat, with a small stream meandering through it. The stream is fed by melting snow and rainwater, adding to the scenic beauty of the corrie. The surrounding landscape boasts an array of native flora and fauna, making it a popular destination for hikers, nature enthusiasts, and geology enthusiasts alike.

Corrie of Inchdowrie stands as a testament to the powerful forces of nature and provides a glimpse into the Earth's glacial history. It serves as a captivating reminder of the lasting impact of the ice age on the Scottish landscape.