Fulford Battlefield Research Website


Geological evidence
 Recording the events of September 1066
tanged arrow from Fulford
yorks releif map

The Fulford Tapestry Website

York map
Fulford map
York in 1066
Norse arrive 1066
Norse march to Fulford
Post-conquest Fulford
3D view of battle
LIDAR image
Geological evidence
1851 map of Fulford
John Speed map
Locating site
Proposed road
Riccall Rampage

York City Planning documents online


YouTube videos


The Final Report

Finding Fulford cover

Kindle edition of Finding Fulford is now available

The Fulford Tapestry


Visiting Fulford

Map York


The Geology of the Fulford Battle Site

The ground created by the last ice age provided the surface on which the Battle of Fulford was fought.

The key feature is the rib of sand and gravel deposited at the face of the glacier as it melted. Its route is precisely marked by the line of the modern A19 road running roughly north-south. The competing armies would have approached the site along this route from the south. This geological wall has only been breached at one location near Fulford at Germany Beck.

Either side of this firm, elevated ground the land has been waterlogged since the ice retreated. The glacial deposit has determined the eastern course of the river Ouse which itself rests on the glacial material. The ground between the river and the glacial moraine is filled with alluvial material that is periodically refreshed when the river floods. This is the area of the Fulford Ings. The action of periodic flooding has also produced a firm path near the river bank as heavier material is left on the banks while fines are flushed back to the river.

To the east of the high ground is an extensive area of wet land. Over the centuries, much of this waterlogged land has been recovered. Most recently, the University of York was created after extensive hydrological work to drain the land. This area of silt and clay was deposited during the last glaciation and encircles the ground the to east of the battle site. While not impassable, there would be no easy route to bypass or outflank any blocking force at Fulford.

Germany Beck is the drain for this extensive area. At some stage the build-up of water on the area covered by the modern Walmgate Stray, Heslington and Fulford Damlands (Water Fulford) broke through the glacial bank to reach the Ouse. The size of the catchment area provides the flow necessary to cut, and then, keep this restricted route to the river open.

The only other area noted in geological surveys covers the area now covered by Fulford Cemetery. This deposit points to the weak point in the glacial material that was exploited by Germany Beck. At this point the melting glacier steps to the west. It would have provided a small area of firm, relatively high ground for the Viking army.

Sketch map based on information in 1908 and 1987 OS Geological Survey maps

Some core samples have been taken from the Ings. The results should be published in October 02


Related sites Facebook  Twitter (@ helpsavefulford)        Visiting Fulford        Map York

The author of the content is Charles Jones - fulfordthing@gmail.com   Last updated April 2015

This site does not use any cookies - so nothing is knowingly installed on your computer when browsing