The main rivers in the Nördlinger Ries crater area of Germany are the Wörnitz and the Eger.
The Wörnitz flows south to the Danube, across Central and Eastern Europe into the Black Sea in Romania and Ukraine. The Eger flows east to the Elbe river which empties into the North Sea off the coast of Germany, over 150km from the Dutch border and about 500km from Lent.
Although the river Waal is a major branch of the Rhine, the nearest the Rhine comes to the Ries crater is over 200km to the east.
The furthest that heavy ejecta is known to have been thrown from the crater is about 180km, although tiny fragments and dust were carried much further. Microscopic shocked quartz grains have been found in soil at Geldrop-Aalsterhut in the Netherlands, a little south of Lent.
I'm also not seeing the planar deformation features diagnostic for intense-pressure-shocked quartz in your specimen.