Log In
Traprain Law, Haddington, East Lothian, Scotland, UKi
| Regional Level Types | |
|---|---|
| Traprain Law | Hill |
| Haddington | Town |
| East Lothian | Council Area |
| Scotland | Country |
| UK | Country |
This page is currently not sponsored. Click here to sponsor this page.
Latitude & Longitude (WGS84):
55° 57' 44'' North , 2° 40' 17'' West
Latitude & Longitude (decimal):
Type:
Köppen climate type:
Nearest Settlements:
| Place | Population | Distance |
|---|---|---|
| East Linton | 1,700 (2017) | 2.9km |
| Haddington | 9,020 (2017) | 7.0km |
| Gifford | 780 (2017) | 8.0km |
| West Barns | 680 (2017) | 8.1km |
| Dunbar | 8,470 (2017) | 10.7km |
Nearest Clubs:
Local clubs are the best way to get access to collecting localities
Local clubs are the best way to get access to collecting localities
| Club | Location | Distance |
|---|---|---|
| The Scottish Mineral & Lapidary Club | Leith, Edinburgh | 31km |
Other/historical names associated with this locality:
East Lothian
A sodalite-bearing phonolitic analcime-trachyte.
From Wikipedia:
"Traprain Law is a hill about 221 m (725 ft) elevation, located 6 km (4 mi) east of Haddington in East Lothian, Scotland. It is the site of an oppidum or hill fort, which covered at its maximum extent about 16 ha (40 acres). It is the site of the Traprain Law Treasure, the largest Roman silver hoard from anywhere outside the Roman Empire and which included exquisite silver artefacts.
The hill was already a place of burial by around 1500 BC, and showed evidence of occupation and signs of ramparts after 1000 BC. The ramparts were rebuilt and realigned many times in the following centuries. Excavations have shown it was occupied in the Late Iron Age from about AD 40 until the last quarter of the 2nd century (about the time that the Antonine Wall was manned). Following the Roman withdrawal to Hadrian's Wall, it was predominantly uninterruptedly occupied from about 220 until about 400 when the rampart was replaced by one more impressive. The site was abandoned after a few decades.
In the 1st century AD the Romans recorded the Votadini as a British tribe in the area, and Traprain Law is generally thought to have been one of their major settlements; named Curia by Ptolemy. They emerged as a kingdom under the Brythonic version of their name Gododdin and Traprain Law is thought to have been their capital before moving to Din Eidyn (Castle Rock in modern Edinburgh).
In 1938 an area of the hill was leased to the district council for use as a quarry for road stone, causing substantial disfigurement to the landscape."
From Wikipedia:
"Traprain Law is a hill about 221 m (725 ft) elevation, located 6 km (4 mi) east of Haddington in East Lothian, Scotland. It is the site of an oppidum or hill fort, which covered at its maximum extent about 16 ha (40 acres). It is the site of the Traprain Law Treasure, the largest Roman silver hoard from anywhere outside the Roman Empire and which included exquisite silver artefacts.
The hill was already a place of burial by around 1500 BC, and showed evidence of occupation and signs of ramparts after 1000 BC. The ramparts were rebuilt and realigned many times in the following centuries. Excavations have shown it was occupied in the Late Iron Age from about AD 40 until the last quarter of the 2nd century (about the time that the Antonine Wall was manned). Following the Roman withdrawal to Hadrian's Wall, it was predominantly uninterruptedly occupied from about 220 until about 400 when the rampart was replaced by one more impressive. The site was abandoned after a few decades.
In the 1st century AD the Romans recorded the Votadini as a British tribe in the area, and Traprain Law is generally thought to have been one of their major settlements; named Curia by Ptolemy. They emerged as a kingdom under the Brythonic version of their name Gododdin and Traprain Law is thought to have been their capital before moving to Din Eidyn (Castle Rock in modern Edinburgh).
In 1938 an area of the hill was leased to the district council for use as a quarry for road stone, causing substantial disfigurement to the landscape."
Select Mineral List Type
Standard Detailed Gallery Strunz Chemical ElementsMineral List
8 valid minerals.
Rock Types Recorded
Select Rock List Type
Alphabetical List Tree DiagramDetailed Mineral List:
| ⓘ Aegirine Formula: NaFe3+Si2O6 |
| ⓘ Analcime Formula: Na(AlSi2O6) · H2O |
| ⓘ 'Apophyllite Group' Formula: AB4[Si8O20]X · 8H2O |
| ⓘ Augite Formula: (CaxMgyFez)(Mgy1Fez1)Si2O6 |
| ⓘ Fayalite Formula: Fe2+2(SiO4) |
| ⓘ Magnetite Formula: Fe2+Fe3+2O4 |
| ⓘ Nepheline Formula: Na3K(Al4Si4O16) |
| ⓘ Powellite Formula: Ca(MoO4) Description: A single greenish-black crystal (c. 1 cm), associated with apophyllite and analcime, in a geode in phonolite. |
| ⓘ Sodalite Formula: Na4(Si3Al3)O12Cl Description: Associated with analcite in small (< 0.2 mm) irregular patches in the groundmass or as larger ( < 0.5 mm) roundish patches with ophitic relations to the feldspars, in the phonolite. [This mineral has been confirmed by electron-probe microanalysis. U. Söffler pers. com.] References: MacGregor, A. G. (1922) The Traprain Law Phonolite. Geological Magazine, 59 (11) 514-523 doi:10.1017/s0016756800109173 |
Gallery:
List of minerals arranged by Strunz 10th Edition classification
| Group 4 - Oxides and Hydroxides | |||
|---|---|---|---|
| ⓘ | Magnetite | 4.BB.05 | Fe2+Fe3+2O4 |
| Group 7 - Sulphates, Chromates, Molybdates and Tungstates | |||
| ⓘ | Powellite | 7.GA.05 | Ca(MoO4) |
| Group 9 - Silicates | |||
| ⓘ | Fayalite | 9.AC.05 | Fe2+2(SiO4) |
| ⓘ | Augite | 9.DA.15 | (CaxMgyFez)(Mgy1Fez1)Si2O6 |
| ⓘ | Aegirine | 9.DA.25 | NaFe3+Si2O6 |
| ⓘ | Nepheline | 9.FA.05 | Na3K(Al4Si4O16) |
| ⓘ | Sodalite | 9.FB.10 | Na4(Si3Al3)O12Cl |
| ⓘ | Analcime | 9.GB.05 | Na(AlSi2O6) · H2O |
| Unclassified | |||
| ⓘ | 'Apophyllite Group' | - | AB4[Si8O20]X · 8H2O |
List of minerals for each chemical element
| H | Hydrogen | |
|---|---|---|
| H | ⓘ Analcime | Na(AlSi2O6) · H2O |
| H | ⓘ Apophyllite Group | AB4[Si8O20]X · 8H2O |
| O | Oxygen | |
| O | ⓘ Aegirine | NaFe3+Si2O6 |
| O | ⓘ Analcime | Na(AlSi2O6) · H2O |
| O | ⓘ Apophyllite Group | AB4[Si8O20]X · 8H2O |
| O | ⓘ Augite | (CaxMgyFez)(Mgy1Fez1)Si2O6 |
| O | ⓘ Fayalite | Fe22+(SiO4) |
| O | ⓘ Magnetite | Fe2+Fe23+O4 |
| O | ⓘ Nepheline | Na3K(Al4Si4O16) |
| O | ⓘ Powellite | Ca(MoO4) |
| O | ⓘ Sodalite | Na4(Si3Al3)O12Cl |
| Na | Sodium | |
| Na | ⓘ Aegirine | NaFe3+Si2O6 |
| Na | ⓘ Analcime | Na(AlSi2O6) · H2O |
| Na | ⓘ Nepheline | Na3K(Al4Si4O16) |
| Na | ⓘ Sodalite | Na4(Si3Al3)O12Cl |
| Mg | Magnesium | |
| Mg | ⓘ Augite | (CaxMgyFez)(Mgy1Fez1)Si2O6 |
| Al | Aluminium | |
| Al | ⓘ Analcime | Na(AlSi2O6) · H2O |
| Al | ⓘ Nepheline | Na3K(Al4Si4O16) |
| Al | ⓘ Sodalite | Na4(Si3Al3)O12Cl |
| Si | Silicon | |
| Si | ⓘ Aegirine | NaFe3+Si2O6 |
| Si | ⓘ Analcime | Na(AlSi2O6) · H2O |
| Si | ⓘ Apophyllite Group | AB4[Si8O20]X · 8H2O |
| Si | ⓘ Augite | (CaxMgyFez)(Mgy1Fez1)Si2O6 |
| Si | ⓘ Fayalite | Fe22+(SiO4) |
| Si | ⓘ Nepheline | Na3K(Al4Si4O16) |
| Si | ⓘ Sodalite | Na4(Si3Al3)O12Cl |
| Cl | Chlorine | |
| Cl | ⓘ Sodalite | Na4(Si3Al3)O12Cl |
| K | Potassium | |
| K | ⓘ Nepheline | Na3K(Al4Si4O16) |
| Ca | Calcium | |
| Ca | ⓘ Augite | (CaxMgyFez)(Mgy1Fez1)Si2O6 |
| Ca | ⓘ Powellite | Ca(MoO4) |
| Fe | Iron | |
| Fe | ⓘ Aegirine | NaFe3+Si2O6 |
| Fe | ⓘ Augite | (CaxMgyFez)(Mgy1Fez1)Si2O6 |
| Fe | ⓘ Fayalite | Fe22+(SiO4) |
| Fe | ⓘ Magnetite | Fe2+Fe23+O4 |
| Mo | Molybdenum | |
| Mo | ⓘ Powellite | Ca(MoO4) |
Other Databases
| Wikipedia: | https://en.wikipedia.org/wiki/Traprain_Law |
|---|---|
| Wikidata ID: | Q1119359 |
Other Regions, Features and Areas containing this locality
British and Irish IslesGroup of Islands
Eurasian PlateTectonic Plate
- CaledonidesOrogenic Belt
EuropeContinent
UK
- Scotland
This page contains all mineral locality references listed on mindat.org. This does not claim to be a complete list. If you know of more minerals from this site, please register so you can add to our database. This locality information is for reference purposes only. You should never attempt to
visit any sites listed in mindat.org without first ensuring that you have the permission of the land and/or mineral rights holders
for access and that you are aware of all safety precautions necessary.
References
MacGregor, A. G. (1922) The Traprain Law Phonolite. Geological Magazine, 59 (11) 514-523 doi:10.1017/s0016756800109173
Battey, M. H., Moss, A. A. (1962) Powellite from Traprain Law, Haddingtonshire, Scotland. Mineralogical Magazine and Journal of the Mineralogical Society, 33 (257) 158-161 doi:10.1180/minmag.1962.033.257.09



Traprain Law, Haddington, East Lothian, Scotland, UK