Page 38 - Poat_to_Poot_Engels
P. 38

The land was covered with peat many feet thick, but this was rapidly
                  stripped away.  The dark soil beneath the peat was good for farming, but
                  when the rich organic matter was exposed to the air, it oxidized and
                  shrank, causing land subsidence.  The drainage channels, levees and
                  seawalls that were built to reduce flooding, also lowered the water table,
                  which caused further land subsidence.  Land that started above sea level
                  often sank to several feet below sea level.  Sometimes areas had to be
                  abandoned as storms and floods would wash away the land or simply
                  cause too much flooding to allow any farming.  The Zuider Zee, a large
                  inland sea, was created by erosion from ocean storms in the 12th
                  century.  Through the wonders of modern engineering, and at vast
                  expense, some 632 square miles of the Zuider Zee were reclaimed for
                  human use in the late 1900's.


                  By the late Middle Ages, technology had improved, and dykes, levees,
                  sluices, gates, and windmills were used to block the ocean, regulate
                  rivers, and pump out water.  In Friesland, the land could be owned by
                  anyone willing to reclaim it.  Individual farmers typically reclaimed the
                  land for use in small plots.  These plots are called polders.  A person who
                  went to the work of preparing a polder was given title to that plot of
                  land.  The result was a government not dominated by feudal lords as in
                  the rest of Europe.  Although the Frisian language was shared, there was
                  no central government.  There were informal districts that formed
                  around the principal towns.  Although each municipality issued its own
                  coinage, they followed common standards.  Laws were locally
                  administered, but were generally consistent between municipalities,
                  following the standards set by Charlemagne.  The difficult marshes and
                  moors made outside conquest impractical.  For a long time this gave
                  Friesland independence in its daily life, and it was rather democratic in
                  its governance.  As travel became easier and the population grew, some
                  landowners became wealthy, and the forces of greed and power took
                  hold.  In the 1400's the city-states began fighting with each other, about
                  land and power.  The resulting chaos and effort wasted on warfare
                  allowed the dykes to decline and some towns were destroyed by floods,
                  and valuable farmlands were lost.  In 1498 the people petitioned to
                  become part of the government to the south so they could again focus
                  on the battle with nature instead of with each other.  Dutch then became
                  the official language of Friesland, although the common people
                  continued to use Frisian in their daily lives.


                  In the 1500's, engineers from Holland arrived and the entire system of
                  dykes and water control was greatly improved.  Canals were built to
                  provide transportation between towns, and canal building continued far
                  into the 1900's.  Canals were so important for transportation, that roads
                  were to remain secondary in quality and capacity in much of the region
                  until the late 1800's and early 1900's.  During the 1500's the engineers
                  standardized the earthwork and reclamation practices.  Newly protected
                  land was allowed to drain and settle before building on it.  Villages were



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