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Coordinates: 42°0′17.5″N 71°27′13″W / 42.004861°N 71.45361°W / 42.004861; -71.45361
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==Background==
==Background==
Cumberlandite is considered sacred to the [[Nipmuc]] tribe. <ref>Ferguson, Joseph L. eReferenceDesk. https://www.ereferencedesk.com/resources/state-symbols/rhode-island/rock.html</ref>{{Citation needed|date=February 2024}} During the 18th and 19th centuries, colonial settlers recognized its value as [[ore]]. Historical records reveal that as early as 1703, it was [[Smelting|smelted]] and was later employed in the forging of cannons during significant events such as the [[Siege of Louisbourg (1745)|Siege of Louisbourg in 1745]] and quite possibly the [[American Revolutionary War|Revolutionary War]].<ref>{{cite journal |last1=Dietrich |first1=R. |title=Rhode Island's State Rock and Mineral: Cumberlandite & “Bowenite” |journal=Rocks & Minerals |date=1986 |volume=61 |issue=5 |pages=251-256 |doi=10.1080/00357529.1986.11762723}}</ref>
Colonial settlers recognized its value as ore during the 18th and 19th centuries. Historical records reveal that it was smelted as early as 1703, and it was used in forging cannons during significant events such as the [[Siege of Louisbourg (1745)|Siege of Louisbourg in 1745]] and possibly the [[American Revolutionary War]].<ref>{{cite journal |last1=Dietrich |first1=R. |title=Rhode Island's State Rock and Mineral: Cumberlandite & “Bowenite” |journal=Rocks & Minerals |date=1986 |volume=61 |issue=5 |pages=251-256 |doi=10.1080/00357529.1986.11762723}}</ref>


Cumberlandite weathers to a brownish black with white crystals and has secondary [[Chlorite group|chlorite]] and [[saussurite]].<ref>[http://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=RIDZc;0 Mineral Resources Spatial Data and Geology: Rhode Island; United states Geological Survey]</ref> It is predominantly found in glacial deposits stretching from south of its origin to the southern shores of Narragansett. Unlike other rocks in Rhode Island's glacial deposits, Cumberlandite is denser than common granites or metamorphic rocks. Its unique origin, distinct appearance, and ease of identification contributed to its selection as the Rhode Island state rock.
Cumberlandite weathers to a brownish black with white crystals and has secondary [[Chlorite group|chlorite]] and [[saussurite]].<ref>[http://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=RIDZc;0 Mineral Resources Spatial Data and Geology: Rhode Island; United states Geological Survey]</ref> It is predominantly found in glacial deposits stretching from south of its origin to the southern shores of Narragansett. Cumberlandite is denser than common granites or metamorphic rocks. Its unique origin, distinct appearance, and ease of identification contributed to its selection as the Rhode Island state rock.


==Petrology==
==Petrology==

Revision as of 11:27, 10 September 2024

Cumberlandite is the state rock of Rhode Island and a specific type of plutonic rock called a melanocratic troctolite, or melatroctolite.[1][2] It can be found in a 4-acre (0.016 km2) lot in Cumberland, Rhode Island at Iron Mine Hill.[3] Further traces can be found scattered throughout the Narragansett Bay watershed as far as Martha's Vineyard.[4] Cumberlandite is not exclusive to Rhode Island, but is also found in Taberg, Sweden.[5] It is slightly ferrimagnetic due to its high concentration of iron.

Two pieces of Cumberlandite
Specimen on display at the Roger Williams Park Museum of Natural History and Planetarium. Specimen is approximately 1 foot (30 cm) wide.

Background

Colonial settlers recognized its value as ore during the 18th and 19th centuries. Historical records reveal that it was smelted as early as 1703, and it was used in forging cannons during significant events such as the Siege of Louisbourg in 1745 and possibly the American Revolutionary War.[6]

Cumberlandite weathers to a brownish black with white crystals and has secondary chlorite and saussurite.[7] It is predominantly found in glacial deposits stretching from south of its origin to the southern shores of Narragansett. Cumberlandite is denser than common granites or metamorphic rocks. Its unique origin, distinct appearance, and ease of identification contributed to its selection as the Rhode Island state rock.

Petrology

Cumberlandite is an uncommon mafic igneous rock known as a melanocratic troctolite, or by IUGS classification, titaniferous magnetite melatroctolite.[8]

Bulk rock geochemistry shows the below analysis with trace Pb:

Bulk Rock Geochemistry[9]
Oxide Weight %
SiO2 22.35
TiO2 9.75
Al2O3 5.26
MgO 16.10
Fe2O3 14.05
FeO 28.84
MnO 0.43
CaO 1.17
Na2O 0.44
K2O 0.10
P2O5 0.02
V2O3 0.18
S 0.38
Zn 0.71
Cu 0.08
CO & Ni 0.08
H2O 0.42
CO2 0.02
Sum 100.38

Troctolites are unusual olivine-rich pyroxene-poor gabbros common in layered mafic intrusions believed to have formed as cumulates in a magma chamber. Cumberlandite has light phenocrysts of labradorite in a dark, fine to medium-grained matrix of magnetite, ilmenite, olivine, and hercynite spinel. Magnetite and ilmenite cumulates are also common in layered intrusions and these minerals can account for up to 70 percent of the rock's volume contributing to the rock's high density and magnetism. The preferred orientation of the plagioclase crystals gives the rock a lamination.[10]

The rock is part of the Esmond-Dedham Subterrane with an uncertain age ranging widely from Late Proterozoic to around the Devonian.[11] He-Magnetite dating suggest an improbable age of 1.5Ga.[12] Given its chemical composition and the presence of inclusions from a nearby gabbro, experts believe the rock is mid-Paleozoic.[13][14]

References

  1. ^ Fun Facts and Figures about Rhode Island
  2. ^ Dietrich, R. (1986). "Rhode Island's State Rock and Mineral: Cumberlandite & "Bowenite"". Rocks & Minerals. 61 (5): 251–256. doi:10.1080/00357529.1986.11762723.
  3. ^ "Iron Mine Hill quarry, Cumberland, Providence County, Rhode Island, USA". Mindat.org. Hudson Institute of Mineralogy.
  4. ^ Quinn, Alonzo (1971). Bedrock Geology of Rhode Island Survey 1295 (PDF). USGS.
  5. ^ Quinn, Alonzo (1971). Bedrock Geology of Rhode Island Survey 1295 (PDF). USGS.
  6. ^ Dietrich, R. (1986). "Rhode Island's State Rock and Mineral: Cumberlandite & "Bowenite"". Rocks & Minerals. 61 (5): 251–256. doi:10.1080/00357529.1986.11762723.
  7. ^ Mineral Resources Spatial Data and Geology: Rhode Island; United states Geological Survey
  8. ^ R. V. Dietrich (1986) Rhode Island's State Rock and Mineral: Cumberlandite & “Bowenite”, Rocks & Minerals, 61:5, 251-256, DOI: 10.1080/00357529.1986.11762723
  9. ^ Quinn, Alonzo (1971). Bedrock Geology of Rhode Island Survey 1295 (PDF). USGS.
  10. ^ Dietrich, R. (1986). "Rhode Island's State Rock and Mineral: Cumberlandite & "Bowenite"". Rocks & Minerals. 61 (5): 251–256. doi:10.1080/00357529.1986.11762723.
  11. ^ Mineral Resources Spatial Data and Geology: Rhode Island; United states Geological Survey
  12. ^ Quinn, Alonzo (1971). Bedrock Geology of Rhode Island Survey 1295 (PDF). USGS.
  13. ^ Quinn, Alonzo (1971). Bedrock Geology of Rhode Island Survey 1295 (PDF). USGS.
  14. ^ Dietrich, R. (1986). "Rhode Island's State Rock and Mineral: Cumberlandite & "Bowenite"". Rocks & Minerals. 61 (5): 251–256. doi:10.1080/00357529.1986.11762723.


42°0′17.5″N 71°27′13″W / 42.004861°N 71.45361°W / 42.004861; -71.45361

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