A wide variety of rocks, minerals and gemstones can be found in Florida, including agatized coral, calcite, silicified wood, flint, chalcedony and geodes. In 1979, the Florida Legislature designated agatized coral as the state stone of Florida. It is described in the law as “a pseudomorph of chalcedony in honor of coral, which appears as limestone geodes coated with agate or botryoidal quartz crystals and dry quartz fingers, native to Florida. Along the banks of rivers in Panama City, Florida, a plethora of rocks and minerals can be discovered.
For information on Florida's geological formations, visit the Formations page. PANAMA CITY BEACH Right on the coast, a kind of river runs parallel to the coast of Panama City Beach. The first is the change observed through tectonic discrimination diagrams in which basaltic and silicic Miocene rocks are traced in extensional fields. A wide variety of rocks, minerals and gemstones can be found in Florida, such as agatized coral, calcite, silicified wood, flint, chalcedony and geodes. For both Fe and Ti, Pedro Miguel's silicic tuffs connect rocks enriched with late basalt in a continuous trend with the more silicic formation in Panama City.
This sample presents a large negative Sr anomaly that is also present in the data from Las Cascadas and the Panama City Formation, but is not common in most Panamanian arc rocks. However, some calcite and quartz crystals can be found near Crystal River and Brooksville in local quarries. The third group of units consists of the Las Cascadas Formation, the Cucaracha ash layer and the Panama City Formation. The structural maps and cross-sections clearly show the existence of normal faults and that the Panama Canal itself exists in a small structural graben. On November 6, 1903, Philippe Bunau-Varilla, as Panama's ambassador to the United States, signed the Hay—Bunau-Varilla Treaty, which gives the United States the rights to build and administer the Panama Canal Zone and its defenses indefinitely.
The oldest record of a canal that crossed the Isthmus of Panama dates back to 1534, when Charles V, emperor of the Holy Roman Empire and king of Spain, ordered a study of a route through the Americas in order to facilitate the travel of ships traveling between Spain and Peru. Roosevelt changed tactics, based in part on the Mallarino—Bidlack Treaty of 1846, and actively supported the separation of Panama from Colombia. In 1855, William Kennish, an engineer born on the Isle of Man who worked for the United States government, inspected the isthmus and published a report on the proposed route for the Panama Canal. One of Stevens' first achievements in Panama was to build and rebuild the homes, cafeterias, hotels, water systems, repair shops, warehouses and other infrastructure needed by the thousands of incoming workers. The most silicic units along the Panama Canal are the Panama City and Las Cascadas formations, which are traced together and measure between 57 and 70 feet in height. The Panama City Formation (n) suggests that an additional petrological mechanism is needed to generate the full range of observed compositional variability. Panama City is home to an abundance of rocks and minerals that are unique to this region.
From agatized coral to calcite to silicified wood to flint to chalcedony to geodes - there is something for everyone! Whether you're looking for specimens for your collection or just want to explore nature's wonders - you'll find it here! From tectonic discrimination diagrams that trace basaltic and silicic Miocene rocks in extensional fields to samples that present large negative Sr anomalies - there's something for everyone! You can even explore historical sites related to canal building - from Charles V's 1534 study route through America to William Kennish's 1855 report on a proposed route for a canal. So if you're looking for an adventure - come explore all that Panama City has to offer! From its unique rocks and minerals to its historical sites - you won't be disappointed!.
