Population of maryland in the years of 1700, 1750, 1775

The population of Maryland In 1700 was 29,604, In 1750 it was 141,073, and in 1775 the population peaked at a 225,036. Maybe wrong due to their is no real way to judge population

the correct answer is 2.

a slump in geology means a mass movement process of slope failure. a mass of rock or unconsolidated material drops along a slip surface. in other words, rock layers move a short distance down the slope. the slump block is an intact block (2), without any landslide material.

in this image, 1 is the surface of rapture (scarp), 2 the slump block, 3 main scarp (crown), 4 base of rapture with debris flow.

slumps are caused by clear cutting on unstable soils and the sagging of earth, in coastal areas they are due to wave infiltration.

answer; the region experienced a surplus of food;