FACTOID # 176: Russia produces more natural gas than the next six countries combined, and has over a quarter of the world's proven gas reserves.
 
 Home   Encyclopedia   Statistics   Countries A-Z   Flags   Maps   Education   Forum   FAQ   About 
 
WHAT'S NEW
RECENT ARTICLES
More Recent Articles »
 

Encyclopedia > Old Rhine
 close-up of the Utrecht region showing the Leidse Rijn-Oude Rijn stream (d).
Enlarge
Satellite close-up of the Utrecht region showing the Leidse Rijn-Oude Rijn stream (d).

The Oude Rijn (Old Rhine) is a branch of the Rhine delta in the Dutch provinces of Utrecht and South Holland. Its present-day length is 52 kilometres. In Roman times, it was the main Rhine branch, forming the northern border of the Empire. The river silted up in the course of the Middle Ages and had lost all of its importance by the seventeenth century.


The city of Utrecht was founded at a ford near the fork of river Kromme Rijn into the Vecht to the north, and the Oude Rijn to the west. Of the original fork, little remains today and both Vecht and Rijn start from the city moat. For the first few kilometres of its course, the river is channelised and known as Leidse Rijn ("Leyden Rhine"). It flows past the towns of De Meern, Harmelen, Woerden, Nieuwerbrug, Bodegraven, Zwammerdam, Alphen aan den Rijn, Koudekerk aan den Rijn, Leiderdorp and Leiden towards Katwijk. Here, the Oude Rijn originally flowed into the North Sea, but the stream has been closed off by a sluice complex regulating its water level.


Many of the cities and villages along the Oude Rijn are of Roman origin, stemming from border-guarding castella and castra.


  Results from FactBites:
 
Rhine - Wikipedia, the free encyclopedia (3638 words)
The Rhine canyon (Ruinaulta) in Graubünden in Switzerland
Since the Rhine flows from the Alps, a precondition of its existence is the uplifting of the Alps, which began in the Alpine Orogeny.
These highlands helped to divert the Rhine to the west; however, the Rhine's course is set by the Rhine graben, a rift that opened in the Eocene and Oligocene periods between the western Alps and the central Alps, caused by their moving in slightly different directions.
Rhine - LoveToKnow 1911 (3334 words)
The Rhine rises in the mountains of the Swiss canton of the Grisons, and flows for 233 m.
In Roman times the Rhine at this part of its course seems to have been a full and flowing river, but by the 9th century it had lost itself in the sands of Katwijk, and it was not until the beginning of the 19th century that its way to the sea was re-opened.
The Rhine has been one of the chief waterways of Europe from the earliest times; and, as its channel is not exposed to the danger of silting up like those of the Elbe and the Oder, it has always been comparatively easy to keep it open.
  More results at FactBites »

 

COMMENTARY     


Share your thoughts, questions and commentary here
Your name
Your location
Your comments
Please enter the 5-letter protection code


Lesson Plans | Student Area | Student FAQ | Reviews | Press Releases |  Feeds | Contact
The Wikipedia article included on this page is licensed under the GFDL.
Images may be subject to relevant owners' copyright.
All other elements are (c) copyright NationMaster.com 2003-5. All Rights Reserved.
Usage implies agreement with terms.