The Red Lands roughly correspond with the southern part of the canton of Esch-sur-Alzette, along the border with France. Geologically, the Red Lands are sedimentary, mostly sandstones and conglomerates, formed in the Middle Jurassic epoch.
The Red Lands are located in the southern part of Esch-sur-Alzette canton, bordering France. Geologically, these lands consist primarily of sedimentary rocks such as sandstones and conglomerates, which were formed during the Middle Jurassic period.