Question: The following article contains an answer for the question: What was the first name of James' assistant? , can you please find it?   In late 1854 or early 1855 James Robertson married Beato's sister, Leonilda Maria Matilda Beato. They had three daughters, Catherine Grace (b. 1856), Edith Marcon Vergence (b. 1859), and Helen Beatruc (b. 1861).In 1855 Felice Beato and Robertson travelled to Balaklava, Crimea, where they took over reportage of the Crimean War following Roger Fenton's departure. Beato was ostensibly Robertson's assistant, however the unpredictable conditions of a war-zone forced Beato to assume a more active role. In contrast to Fenton's depiction of the dignified aspects of war, Beato and Robertson showed the destruction and death. They photographed the fall of Sevastopol in September 1855, producing about 60 images. Their Crimean images dramatically changed the way that war was reported and depicted.In February 1858 Beato arrived in Calcutta and began travelling throughout Northern India to document the aftermath of the Indian Rebellion of 1857. During this time he produced possibly the first-ever photographic images of corpses. It is believed that for at least one of his photographs taken at the palace of Sikandar Bagh in Lucknow he had the skeletal remains of Indian rebels disinterred or rearranged to heighten the photograph's dramatic impact (see events at Taku Forts). He was also in the cities of Delhi, Cawnpore, Meerut, Benares, Amritsar, Agra, Simla, and Lahore. Beato was joined in July 1858 by his brother Antonio, who later left India, probably for health reasons, in December 1859. Antonio ended up in Egypt in 1860, setting up a photographic studio in Thebes in 1862.
Answer: Felice

Question: The following article contains an answer for the question: Where is the location that has the least amount of loss of tons of soil in the area with a vast marshland? , can you please find it?   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

Question: The following article contains an answer for the question: What is the last name of the actual person who began composing songs in a distinctive, original style on his return to England in 1918? , can you please find it?   Philip Arnold Heseltine (30 October 1894 – 17 December 1930), known by the pseudonym Peter Warlock, was a British composer and music critic. The Warlock name, which reflects Heseltine's interest in occult practices, was used for all his published musical works. He is best known as a composer of songs and other vocal music; he also achieved notoriety in his lifetime through his unconventional and often scandalous lifestyle. As a schoolboy at Eton College, Heseltine met the British composer Frederick Delius, with whom he formed a close friendship. After a failed student career in Oxford and London, Heseltine turned to musical journalism, while developing interests in folk-song and Elizabethan music. His first serious compositions date from around 1915. Following a period of inactivity, a positive and lasting influence on his work arose from his meeting in 1916 with the Dutch composer Bernard van Dieren; he also gained creative impetus from a year spent in Ireland, studying Celtic culture and language. On his return to England in 1918, Heseltine began composing songs in a distinctive, original style, while building a reputation as a combative and controversial music critic.  During 1920–21 he edited the music magazine The Sackbut. His most prolific period as a composer came in the 1920s, when he was based first in Wales and later at Eynsford in Kent. Through his critical writings, published under his own name, Heseltine made a pioneering contribution to the scholarship of early music. In addition, he produced a full-length biography of Frederick Delius and wrote, edited, or otherwise assisted the production of several other books and pamphlets. Towards the end of his life, Heseltine became depressed by a loss of his creative inspiration. He died in his London flat of coal gas poisoning in 1930, probably by his own hand.
Answer:
Heseltine