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Geological Formation

Malvern Hills

Hill and Mountain Ranges

The Malvern Hills are a narrow ridge of ancient igneous and metamorphic rock straddling Worcestershire, Herefordshire and Gloucestershire in western England, running about thirteen kilometers between Great Malvern and Colwall and reaching their highest point, Worcestershire Beacon, at 425 meters. Their exposed rock, known as Malvernian and dated to the late Precambrian at roughly 680 million years old, includes granite, gneiss, schist, pegmatite and dolerite, among the oldest rock exposed anywhere in England, brought to the surface along the north-south Malvern Line fault and left standing as a ridge once softer surrounding rock wore away. The hills are also known for the mineral springs that emerge from their ancient rock, long associated with Malvern's spa water industry.

Facts
Classification
Protected Status
National Park or Reserve 1
Protected Status
Locally or Regionally Protected 1
Connections

Caused By

Orogeny, Processes

Wikidata P31 (Q9381142) mapped to formative process Orogeny via earth5 extended reviewed judgment map; source citation is this entity's own cited Wikidata item.

Source Wikidata: Malvern Hills

In Discipline

Wikidata P31 (Q9381142) mapped to discipline Geomorphology via earth5 extended reviewed judgment map; source citation is this entity's own cited Wikidata item.

Source Wikidata: Malvern Hills
In the Other Atlases

Found In

Also in Geography Atlas: where this subject is found.

Source Wikidata: Malvern Hills
Sources
1. Wikidata: Malvern Hills
  • Wikidata Q1577855, class allow-list match (w-wdresolver-0926)
  • Wikidata P1435 heritage-designation or P3425 Natura 2000 claim on the formation's own item (w-bbfill-earth2-0926)
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