Title: Geology of Missouri
Content:  Galena is the official state mineral of Missouri and lead mining began in the 1720s in Madison County, spearheaded by French miners. The state is the leading extractor of lead in the U.S., both from galena and sphalerite. The minerals are sourced from Mississippi Valley Type deposits, deposited through hydrothermal activity. The Old Lead Belt and Tri-State Area were mined significantly before World War II, with new deposits found since in the southeast. The new deposit is known as the Viburnum Trend and spans Iron County and Reynolds County, with secondary production of copper, cadmium and silver, housed in the Bonneterre Dolomite between 600 and 1500 feet deep. During the late Cambrian, stromatalite beds shielded carbonates forming below and created a permeable interface for mineralization.
Title: Selsertown, Mississippi
Content:  Selsertown is an extinct town in Adams County, Mississippi, United States. A Plaquemine culture platform mound is located there, once known as the Selsertown Mound but currently known as Emerald Mound. The mound is 35 ft in height, with two secondary mounds at either end of its summit that rise even higher. It once had a total of six to eight mounds on its summit but only the two on the ends have survived. It covers 6 acre. It was described as being of "extraordinary size" in the 1848 book Ancient Monuments of the Mississippi Valley and it is the second-largest Pre-Columbian earthwork in 
Title: Sellars Farm Site
Content:  Sellars Farm Site (40WI1), also known as the Sellars Farm State Archaeological Area and Sellars Indian Mound, is a Mississippian culture archaeological site located in Wilson County, Tennessee near Lebanon. The platform mound was the site of a settlement from about 1000 to 1300 CE. Today, the site is a satellite unit of Long Hunter State Park. The non-profit Friends of the Sellars Farm State Archaeological Area organization conducts tours and upkeep of the site. It was listed on the National Register of Historic Places on December 11, 1972. Numerous sandstone figurines have been unearthed on the site. One of these statues, known as "Sandy," was featured on a United States postage stamp. and is the official State Artifact of Tennessee
Title: Illinois Basin
Content:  The rocks of the Illinois Basin are thought to be the source of metals in Mississippi Valley-Type lead-zinc deposits, both within the basin and in surrounding areas, such as the Lead Belt of southeast Missouri. Within the basin, deposits valuable for lead, zinc, coal balls and fluorite are mined in Hardin and Pope counties, Illinois, and Crittenden and Livingston counties, Kentucky. the deposits are in the form of veins and limestone replacement deposits in Mississippian sedimentary rocks. Ore minerals are fluorite, galena, and sphalerite. Gangue minerals include common quartz and calcite, and minor barite and chalcopyrite.
Title: Southeast Missouri Lead District
Content:  The formal geological name for the Lead Belt is the "Southeastern Missouri Mississippi Valley-type Mineral District." It contains the highest concentration of galena (lead(II) sulfide) in the world as well as significant economic quantities of zinc, copper and silver and currently sub-economic quantities of metals such as cadmium, nickel and cobalt. Most of the mined ore minerals are found as sulfides such as galena, sphalerite, and chalcopyrite. Gangue minerals associated with the economic minerals include pyrite, calcite, dolomite, and quartz. Specimens from the Lead Belt are highly prized by gem and mineral collectors and are found in museums worldwide. The ore minerals of the Lead Belt are primarily hosted by bacterial stromatolite reefs and associated oolitic rocks of the dolomitic Bonneterre Formation. This Cambrian age formation was deposited in a shallow sea around the Precambrian age St. Francois Mountains, which formed an island archipelago. Ore mineralization most likely occurred during the late Pennsylvanian and/or Permian periods when warm metal and petroleum bearing fluids from adjacent sedimentary basins migrated through these rocks.
Title: Minong Mine Historic District
Content:  The Minong Mine is a historic mine site located west of McCargoe Cove campground on Isle Royale National Park, Michigan, United States. The district contains both the remnants of a 19th-century copper mine and remains of pre-contact mining activity. Pre-contact archeological sited in the district include a Late Archaic copper mining pit site designated 20KE24 and a nearby site designated 20KE73. It was listed on the National Register of Historic Places in 1977 and designated a National Historic Landmark in 2021.
Title: Emerald Mound Site
Content:  The Emerald Mound Site (22 AD 504), also known as the Selsertown site, is a Plaquemine culture Mississippian period archaeological site located on the Natchez Trace Parkway near Stanton, Mississippi, United States. The site dates from the period between 1200 and 1730 CE. It is the type site for the Emerald Phase (1500 to 1680 CE) of the Natchez Bluffs Plaquemine culture chronology and was still in use by the later historic Natchez people for their main ceremonial center. The platform mound is the second-largest Mississippian period earthwork in the country, after Monk's Mound at Cahokia, Illinois. The mound covers eight acres, measuring 770 ft by 435 ft at 
Title: Old Mines, Missouri
Content:  The southeast Missouri lead district is the location of the earth's greatest known concentration of galena, an ore of lead. Found first in surface deposits over a wide area, and now mined deep underground, the ore was known to the native Indians of the region from whom it became known to early French explorers. Father Jacques Gravier noted in his journal in October 1700, the presence of rich lead ore twelve or thirteen leagues from the mouth of the "River Miaramigoua" (Meramec), that is 36 to 39 mi. At that time the Meramec tributary Big River was considered part of the Meramec and often called the Little Meramec (French 
Title: Silver Mound Archeological District
Content:  the Indian quarries on the mound since the 1840s. It was named Silver Mound because they mistakenly believed it contained silver. Some mining was done, but no silver was found. The land around the base of the mound has been farmed for years, but much of the mound itself remains largely undisturbed. Professional archeologists first visited the mound in 1928. Gradually the remarkable age of some of the Indian quarries emerged. In 1975 Silver Mound was placed on the National Register of Historic Places. In 2006 it was named a National Historic Landmark, largely because of the potential information it may still hold about the earliest people in Wisconsin.
Title: Madisonville Site
Content:  The Madisonville Site is a prehistoric archaeological site near Mariemont, Ohio, United States. It was listed on the National Register of Historic Places on October 16, 1974 as the "Mariemont Embankment and Village Site". Madisonville is the type site for the Madisonville phase of Fort Ancient pottery. The 5-acre site is located on a bluff above the Little Miami River about 5 miles upstream from the Ohio River. While occupied over hundreds of years, it was settled most intensively in the late sixteenth and early seventeenth centuries, and is the most excavated Fort Ancient site of this time period. Early twentieth-century excavations were carried out by staff of the Peabody Museum 

Question: Verify the following claims with "True" or "False": Well the 11th Mississippi Infantry Monument falls under the category of Selenate minerals in Pennsylvania.
Answer: False