Middle Dodd
| Middle Dodd | |
|---|---|
Middle Dodd, with Brothers Water
beyond, from Red Screes |
|
| Highest point | |
| Elevation | 654 m (2,146 ft) |
| Prominence | c. 10 m |
| Parent peak | Red Screes |
| Listing | Wainwright |
| Coordinates | 54°28′41″N 2°55′56″W / 54.47815°N 2.93211°WCoordinates: 54°28′41″N 2°55′56″W / 54.47815°N 2.93211°W |
| Geography | |
 Middle Dodd
Location in Lake District, UK
|
|
| Location | Cumbria, England |
| Parent range | Lake District, Eastern Fells |
| OS grid | NY397096 |
| Topo map | OS Explorer OL5, OL7 |
Middle Dodd is a fell in the English Lake District, an outlier of the Helvellyn range in the Eastern Fells. It stands above Kirkstone Pass on the road from Ullswater to Ambleside.
Middle Dodd is properly the northern ridge of Red Screes, but was given the status of a separate fell by Alfred Wainwright in his Pictorial Guide to the Lakeland Fells and that convention is followed here. His decision was based on its being "…the most striking object in a fine array of mountain scenery…"
The fell is named as the middle one of three Dodds when viewed from Hartsop, the others being (Low) Hartsop Dodd and High Hartsop Dodd. The names thus refer to position in the valley rather than height. All three present an imposing pyramidal profile when seen from below, totally obscuring their parent fells. Similarly, all three appear entirely derivative when viewed from other angles.
From the wide summit of Red Screes a narrowing ridge curves northward, passing around the rim of a cove on the Kirkstone side. The ridge, named Smallthwaite Band, narrows to a fine grassy promenade and then throws up the summit of Middle Dodd. Beyond this the character of the fell changes completely and a rough slope plunges straight down to the valley floor, 1,500 ft below.
The fell is bounded on either side by valleys of the Ullswater catchment. To the east is Kirkstone Beck, flowing from the summit of the pass with its famous inn. On the west is Caiston Glen, its beck descending from the walker's crossroads of Scandale Pass. These valleys meet beneath the nose of Middle Dodd and continue northward to Brothers Water.
Middle Dodd dacite forms the crest of the ridge, lying above the volcaniclastic laminated claystones and siltstone of the Esk Pike Formation.
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Wikipedia