Answer:
A. Oath of the Horatii
Explanation:
The title of a painting by Jacques-Louis David, where Roman orator Horace receives allegiance from his three sons to protect Rome is known as "OATH OF THE HORATII"
The painting was made in the year 1784 with a Neoclassical painting style. The painting depicts the 7th century BC conflict between two Rome and Alba Longa cities. And it also reveals the sacrifices men undergo when defending their countries.
<span>The consolidation of economic power by the wealthiest.
Prior to the 16th amendment, direct taxes had to apportioned to the states according to population. There were some exceptions based upon indirect taxes such as tariffs and excise taxes, but in general income from rentals of property were effectively unable to be taxed. The Pollock v. Farmers' Loan & Trust Co., case eased the governments ability to tax, in that it made wages exempt from the apportionment clause, but income via rentals, interest, and dividends were restricted to apportionment and effectively untaxable. The 16th amendment allowed for taxation on those sources of income.</span>
The Canadian Shield, one of the world’s largest geologic continental shields, centred on Hudson Bay and extending for 8 million square km (3 million square miles) over eastern, central, and northwestern Canada from the Great Lakes to the Canadian Arctic and into Greenland, with small extensions into northern Minnesota, Wisconsin, Michigan, and New York, U.S. The Canadian Shield constitutes the largest mass of exposed Precambrian rock on the face of Earth. The region, as a whole, is composed of ancient crystalline rocks whose complex structure attests to a long history of uplift and depression, mountain building (orogeny), and erosion. Some of the ancient mountain ranges can still be recognized as a ridge or belt of hills, but the present appearance of the physical landscape of the Canadian Shield is not so much a result of the folding and faulting and compression of the rocks millions of years ago as it is the work of ice in relatively recent geologic time. During the Pleistocene Epoch (2.6 million to 11,700 years ago), the vast continental glaciers that covered northern North America had this region as a centre. The ice, in moving to the south, scraped the land bare of its overlying mantle of weathered rock. Some of this material was deposited on the shield when the ice melted, but the bulk of it was carried southward to be deposited south and southwest of the Canadian Shield. The resulting surface consists of rocky, ice-smoothed hills with an average relief of 30 metres (100 feet), together with irregular basins, which are mostly filled by lakes or swamps. In places the old mountain ranges may be recognized by hills several hundreds of meters in height. The northeastern portion, however, became tilted up so that, in northern Labrador and Baffin Island, the land rises to more than 1,500 metres (5,000 feet) above sea level. :)
Answer:
Sir Stafford Cripps hope it helps all the best
