Q: Found the following article online, use it to answer the question: What are the exact dates of the two specific days during which a total of 174 shocks of magnitude 2.6 or greater were recorded? Mount St. Helens remained dormant from its last period of activity in the 1840s and 1850s until March 1980. Several small earthquakes, beginning on March 15, indicated that magma may have begun moving below the volcano. On March 20, at 3:45 p.m. Pacific Standard Time (all times will be in PST or PDT), a shallow magnitude 4.2 earthquake centered below the volcano's north flank, signaled the volcano's violent return from 123 years of hibernation. A gradually building earthquake swarm saturated area seismographs and started to climax at about noon on March 25, reaching peak levels in the next two days, including an earthquake registering 5.1 on the Richter scale. A total of 174 shocks of magnitude 2.6 or greater were recorded during those two days. Shocks of magnitude 3.2 or greater occurred at a slightly increasing rate during April and May with five earthquakes of magnitude 4 or above per day in early April, and eight per day the week before May 18. Initially there was no direct sign of eruption, but small earthquake-induced avalanches of snow and ice were reported from aerial observations. At 12:36 p.m. on March 27, phreatic eruptions (explosions of steam caused by magma suddenly heating groundwater) ejected and smashed rock from within the old summit crater, excavating a new crater 250 feet (75 m) wide, and sending an ash column about 7,000 feet (2.1 km) into the air. By this date a 16,000-foot-long (3.0 mi; 4.9 km) eastward-trending fracture system had also developed across the summit area. This was followed by more earthquake swarms and a series of steam explosions that sent ash 10,000 to 11,000 feet (3,000 to 3,400 m) above their vent. Most of this ash fell between three and twelve miles (5 and 19 km) from its vent, but some was carried 150 miles (240 km) south to Bend, Oregon, or 285 miles (460 km) east to Spokane, Washington.
A: March 15
Question: Found the following article online, use it to answer the question: What officials did the traders that met French expedition report the expedition to in New Mexico? For several months after the permanent camp was built, the colonists took short trips to explore their surroundings. At the end of October 1685, La Salle decided to undertake a longer expedition and reloaded the Belle with many of the remaining supplies. He took 50 men, plus the Belle's crew of 27 sailors, leaving behind 34 men, women, and children. Most of the men traveled with La Salle in canoes, while the Belle followed further off the coast. After three days of travel, they learned of hostile Native Americans in the area. Twenty of the Frenchmen attacked the Native American village, where they found Spanish artifacts. Several of the men died on this expedition from eating prickly pear. The Karankawa killed a small group of the men who had camped on shore, including the captain of the Belle.From January until March 1686, La Salle and most of his men searched overland for the Mississippi River, traveling towards the Rio Grande, possibly as far west as modern-day Langtry, Texas. The men questioned the local Native American tribes, asking for information on the locations of the Spaniards and the Spanish mines, offering gifts, and telling stories that portrayed the Spanish as cruel and the French as benevolent. When the group returned, they were unable to find the Belle where they had left her and were forced to walk back to the fort.The following month they traveled east, hoping to locate the Mississippi and return to Canada. During their travels, the group encountered the Caddo, who gave the Frenchmen a map depicting their territory, that of their neighbors, and the location of the Mississippi River. The Caddo often made friendship pacts with neighboring peoples and extended their policy of peaceful negotiation to the French. While visiting the Caddo, the French met Jumano traders, who reported on the activities of the Spanish in New Mexico. These traders later informed Spanish officials of the Frenchmen they had seen.
Answer: Spanish
Question: Found the following article online, use it to answer the question: Where is the location that has the least amount of loss of tons of soil in the area with a vast marshland? A vast marshland could only have been formed due to the underlying rock formations in southern Florida. The floor of the Everglades formed between 25 million and 2 million years ago when the Florida peninsula was a shallow sea floor. The peninsula has been covered by sea water at least seven times since the earliest bedrock formation. The rock that makes up the Everglades floor was created as layers of calcium carbonate were compressed by ocean water, making limestone. Fossilized bryozoans and tiny shells, or ooids, make the limestone porous. Water is stored in the rock, sometimes from one year to the next. The length of time that a region in the Everglades remains flooded, called a hydroperiod, determines what particular soils and vegetation are present. Shorter hydroperiods of three or four months promote the growth of periphyton: algae and other microscopic organisms covered with calcium carbonate crystals. Periphyton is the basic building block of marl, a calcitic mud. In areas with hydroperiods of longer than nine months, peat builds up over hundreds or thousands of years due to many generations of decaying plant matter. Peat and marl are considered nutrient-poor soils that foster the growth of specialized vegetation depending on the length of the regional hydroperiod. Five types of peat appear in the Everglades system; each type supports a specific type of vegetation, such as sawgrass, tree islands, or custard apple trees. Peat buildup is possible because water prevents oxygen from quickly decomposing plant matter. Once peat buildup reaches the surface, oxygen reacts with the microorganisms to decay the peat rapidly in a process called subsidence. Initial attempts at developing agriculture near Lake Okeechobee were successful, but the nutrients in the peat quickly deteriorated by drying, and were broken down by bacteria in the soil. The dried peat burned or was degraded into carbon dioxide and water by microorganisms. Some homes built near early farms had to restructure their foundations on stilts as...
Answer:
Everglades National Park