Answer:
changed the way that landowners used their land
Explanation:
The enclosure system is a form of land ownership practice originated in England around the thirteenth century. This system of land holdings gave the owners land that is restricted from the use by any other person aside from the owner of the land. It protects the landholding of individuals against communal use.
This thereby in turn led to the industrial and agricultural revolution. Because most of the private owners then decide to fence their land in which some chose to farm extensively on it or build a factory that manufactured natural products to refine goods.
I would have to say its a very hot place to be. but being surrounded by desserts benefited in Egypt in fact that no one could attack or conquer them there. No group could ever cross the Sahara to get to Egypt for they would die half way in. over 40,000 sq kms (15000 sq miles) flowed through Egypt.
I hope this helps, if not I am sure there other images on google.
It is warmer and milder temperatures today, and back in the Ice Age it was colder and the summer seasons were much shorter.
A geological fold occurs when one or a stack of originally flat and planar surfaces, such as sedimentary strata, are bent or curved as a result of permanent deformation. Synsedimentary folds are those due to slumping of sedimentary material before it is lithified. Folds in rocks vary in size from microscopic crinkles to mountain-sized folds. They occur singly as isolated folds and in extensive fold trains of different sizes, on a variety of scales.
Folds form under varied conditions of stress, hydrostatic pressure, pore pressure, and temperature gradient, as evidenced by their presence in soft sediments, the full spectrum of metamorphic rocks, and even as primary flow structures in some igneous rocks. A set of folds distributed on a regional scale constitutes a fold belt, a common feature of orogenic zones. Folds are commonly formed by shortening of existing layers, but may also be formed as a result of displacement on a non-planar fault (fault bend fold), at the tip of a propagating fault (fault propagation fold), by differential compaction or due to the effects of a high-level igneous intrusion e.g. above a laccolith.
