Yep... you live about 30 miles east of me and you and me are just two lucky sons of guns living exactly where we live.
There is a large band of extra iron running from my county east through yours thanks to the Red Mountain chain.
Try to explain to others that have other mineralization problems about what we deal with in our particular areas and many just won't get it...like all mineralization types and amounts are the same in problem areas.
I guess there is worse out there somewhere but I can't worry about that...I don't live there.
We have so much Hemitite in this state, so extremely concentrated in our area, that it is officially the state mineral.
Like I said...lucky us.
Some info.
Hematite, an oxide of iron (Fe2O3), is also known as "red iron ore" and in 1967 was designated as the State Mineral by the Alabama Legislature. Hematite was mined for many years in the Valley and Ridge area of central and northeastern Alabama. The mining of hematite was once the state's most developed nonfuel mineral industry, and the occurrence of hematite with nearby deposits of coal (a fossil fuel) and limestone (used as flux) led to the development of Birmingham as an industrial center. Iron ore mining in the state ceased in 1975 primarily owing to the availability of inexpensive higher grade imported ores. Red iron ore (from the Red Mountain Formation) has been mined in Bibb, Blount, De Kalb, Cherokee, Etowah, Jefferson, St. Clair, and Tuscaloosa Counties. Hematite occurs along the entire length of Red Mountain which passes through these counties. From about l840 to 1975, approximately 375 million tons of iron ore were mined in Alabama, principally from the Birmingham red-ore district. In 1904 Birmingham iron ore was used in casting the statue of Vulcan, which stands atop Red Mountain as the largest cast-iron structure ever made.