In such surroundings as these there were established in the Middle Ages, two religious houses, within a mile of one another, on opposite sides of the swirling river. On the north bank, not far from Marrick village, you may still see the ruins of Marrick Priory in its beautiful situation much as Turner painted it a century ago. Leland describes Marrick as 'a Priory of Blake Nunnes of the Foundation of the Askes.' It was, we know, an establishment for Benedictine Nuns, founded or endowed by Roger de Aske in the twelfth century. At Ellerton, on the other side of the river a little lower down, the nunnery was of the Cistercian Order; for, although very little of its history has been discovered, Leland writes of the house as 'a Priori of White clothid Nunnes.' After the Battle of Bannockburn, when the Scots raided all over the North Riding of Yorkshire, they came along Swaledale in search of plunder, and we are told that Ellerton suffered from their violence.
Where the dale becomes wider, owing to the branch valley of Arkengarthdale, there are two villages close together. Grinton is reached first, and is older than Reeth, which is a short distance north of the river. The parish of Grinton is one of the largest in Yorkshire. It is more than twenty miles long, containing something near 50,000 acres, and according to Mr. Speight, who has written a very detailed history of Richmondshire, more than 30,000 acres of this consist of mountain, grouse-moor and scar. For so huge a parish the church is suitable in size, but in the upper portions of the dales one must not expect any very remarkable exteriors; and Grinton, with its low roofs and plain battlemented tower, is much like other churches in the neighbourhood. Inside there are suggestions of a Norman building that has passed away, and the bowl of the font seems also to belong to that period. The two chapels opening from the chancel contain some interesting features, which include a hagioscope, and both are enclosed by old screens.
Leaving the village behind, and crossing the Swale, you soon come to Reeth, which may, perhaps, be described as a little town. It must have thrived with the lead-mines in Arkengarthdale and along the Swale, for it has gone back since the period of its former prosperity, and is glad of the fact that its situation, and the cheerful green which the houses look upon, have made it something of a holiday resort.
When Reeth is left behind, there is no more of the fine 'new' road which makes travelling so easy for the eleven miles from Richmond. The surface is, however, by no means rough along the nine miles to Muker, although the scenery becomes far wilder and more mountainous with every mile. The dale narrows most perceptibly; the woods become widely separated, and almost entirely disappear on the southern side; and the gaunt moors, creeping down the sides of the valley seem to threaten the narrow belt of cultivation, that becomes increasingly restricted to the river margins. Precipitous limestone scars fringe the browny-green heights in many places, and almost girdle the summit of Calver Hill, the great bare height that rises a thousand feet above Reeth. The farms and hamlets of these upper parts of Swaledale are of the same greys, greens, and browns as the moors and scars that surround them. The stone walls, that are often high and forbidding, seem to suggest the fortifications required for man's fight with Nature, in which there is no encouragement for the weak. In the splendid weather that so often welcomes the mere summer rambler in the upper dales the austerity of the widely scattered farms and villages may seem a little unaccountable; but a visit in January would quite remove this impression, though even in these lofty parts of England the worst winter snowstorm has, in quite recent years, been of trifling inconvenience. Bad winters will, no doubt, be experienced again on the fells; but leaving out of the account the snow that used to bury farms, flocks, roads, and even the smaller gills, in a vast smother of whiteness, there are still the winds that go shrieking over the desolate heights, there is still the high rainfall, and there are still destructive thunderstorms that bring with them hail of a size that we seldom encounter in the lower levels.
The great rapidity with which the Swale, or such streams as the Arkle, can produce a devastating flood can scarcely be comprehended by those who have not seen the results of even moderate rainstorms on the fells. When, however, some really wet days have been experienced in the upper parts of the dales, it seems a wonder that the bridges are not more often in jeopardy.
Of course, even the highest hills of Yorkshire are surpassed in wetness by their Lakeland neighbours; for whereas Hawes Junction, which is only about seven miles south of Muker, has an average yearly rainfall of about 62 inches, Mickleden, in Westmorland, can show 137, and certain spots in Cumberland aspire towards 200 inches in a year.
The weather conditions being so severe, it is not surprising to find that no corn at all is grown in Swaledale at the present day. Some notes, found in an old family Bible in Teesdale, are quoted by Mr. Joseph Morris. They show the painful difficulties experienced in the eighteenth century from such entries as: '1782. I reaped oats for John Hutchinson, when the field was covered with snow,' and: '1799, Nov. 10. Much corn to cut and carry. A hard frost.'
Muker, notwithstanding all these climatic difficulties, has some claim to picturesqueness, despite the fact that its church is better seen at a distance, for a close inspection reveals its rather poverty-stricken state. The square tower, so typical of the dales, stands well above the weathered roofs of the village, and there are sufficient trees to tone down the severities of the stone walls, that are inclined to make one house much like its neighbour, and but for natural surroundings would reduce the hamlets to the same uniformity. At Muker, however, there is a steep bridge and a rushing mountain stream that joins the Swale just below. The road keeps close to this beck, and the houses are thus restricted to one side of the way.
Away to the south, in the direction of the Buttertubs Pass, is Stags Fell, 2,213 feet above the sea, and something like 1,300 feet above Muker. Northwards, and towering over the village, is the isolated mass of Kisdon Hill, on two sides of which the Swale, now a mountain stream, rushes and boils among boulders and ledges of rock. This is one of the finest portions of the dale, and, although the road leaves the river and passes round the western side of Kisdon, there is a path that goes through the glen, and brings one to the road again at Keld.
Just before you reach Keld, the Swale drops 30 feet at Kisdon Force, and after a night of rain there are many other waterfalls to be seen in this district. These are not to me, however, the chief attractions of the head of Swaledale, although without the angry waters the gills and narrow ravines that open from the dale would lose much interest. It is the stern grandeur of the scarred hillsides and the wide mountainous views from the heights that give this part of Yorkshire such a fascination. If you climb to the top of Rogan's Seat, you have a huge panorama of desolate country spread out before you. The confused jumble of blue-grey mountains to the north-west is beyond the limits of Yorkshire at last, and in their strong embrace those stern Westmorland hills hold the charms of Lakeland.