The rocks at Red Rock Gate consist of sandstone, siltstone, conglomerate, and other formations. Their layered arrangement makes it easy for visitors to identify them as sedimentary rock. But why do they have such a striking red hue? Geologists believe that during the time these rocks formed, the climate was extremely hot, and oxidation was particularly intense. Iron-bearing minerals in the sediments were converted into iron oxide, which cemented the grains of sand together, resulting in uniquely colored red sedimentary rock.
When a boat reaches the end of the Cape d’Aguilar Channel and turns toward Wong Chuk Kok Tsui, it enters Wong Chuk Kok Hoi, where steep green slopes line the waterway. The farther west the boat goes, the calmer the sea becomes, enveloped in near-total silence—as if entering a hidden paradise. Suddenly, the waterway narrows, and purplish-red rocks jut boldly from the shoreline out into the sea, with crystal-clear waters so transparent the boat seems almost to be running aground. This is the renowned Red Rock Gate, famous among travelers.
Transportation Guide
Location: Yan Chau Tong, Tai Po District, New Territories, Hong Kong
Getting There: Take Citybus routes 275R or 75K
This article is published by HowToTrip. Sharing and reposting are welcome — please credit the source.
Article URL: https://www.howtotrip.net/travel-9364