Gros Morne National Park is a Canadian national park and World Heritage Site located on the west coast of Newfoundland. At 1,805 km2 (697 sq mi), it is the second largest national park in Atlantic Canada after Torngat Mountains National Park, which has an area of 9,700 km2 (3,700 sq mi).
Portland stone is a limestone geological formation dating to the Tithonian age of the Late Jurassic that is quarried on the Isle of Portland in Dorset, England. The quarries are cut in beds of white-grey limestone separated by chert beds. It has been used extensively as a building stone throughout the British Isles, notably in major public buildings in London such as St Paul's Cathedral and Buckingham Palace. Portland stone is also exported to many countries, being used for example at the United Nations headquarters in New York City.
Carrara marble, Luna marble to the Romans, is a type of white or blue-grey marble popular for use in sculpture and building decor. It has been quarried since Roman times in the mountains just outside the city of Carrara in the province of Massa and Carrara in the Lunigiana, the northernmost tip of modern-day Tuscany, Italy.
Ediacara Hills, also known as Ediacaran Hills, are a range of low hills in the northern part of the Flinders Ranges of South Australia, around 650 kilometres (400 mi) north of the state capital of Adelaide. They are within the Nilpena Ediacara National Park.
The International Union of Geological Sciences (IUGS) is an international non-governmental organization devoted to international cooperation in the field of geology. As of 2023, it represents more than 1 million geoscientists around the world.
Tyndall Stone is a registered trademark name by Gillis Quarries Ltd. Tyndall Stone is a dolomitic limestone that is quarried from the Selkirk Member of the Ordovician Red River Formation in the vicinity of Garson and Tyndall, Manitoba, Canada. It is a cream-coloured limestone with a pervasive mottling of darker dolomite. The mottling gives the rock a tapestry-like effect, and it is popular for use as a building and ornamental stone.
The Beartooth Mountains are located in south central Montana and northwest Wyoming, U.S. and are part of the 944,000 acres (382,000 ha) Absaroka-Beartooth Wilderness, within Custer, Gallatin and Shoshone National Forests. The Beartooths are the location of Granite Peak, which at 12,807 feet (3,904 m) is the highest point in the state of Montana. The mountains are just northeast of Yellowstone National Park and are part of the Greater Yellowstone Ecosystem. The mountains are traversed by road via the Beartooth Highway with the highest elevation at Beartooth Pass 10,947 ft (3,337 m)). The name of the mountain range is attributed to a rugged peak found in the range, Beartooth Peak, that has the appearance of a bear's tooth.
The Chibanian, widely known as the Middle Pleistocene, is an age in the international geologic timescale or a stage in chronostratigraphy, being a division of the Pleistocene Epoch within the ongoing Quaternary Period. The Chibanian name was officially ratified in January 2020. It is currently estimated to span the time between 0.770 Ma and 0.126 Ma, also expressed as 770–126 ka. It includes the transition in palaeoanthropology from the Lower to the Middle Paleolithic over 300 ka.
Makrana is an urban city located at the centre of Rajasthan in Kuchaman City District. It also served as a tehsil headquarters, with 136 villages under its jurisdiction thus making it the largest tehsil in the district. The biggest village of Makrana tehsil by area is Modicharna. Makrana is 110 km (68 mi) west of Jaipur and 190 km (120 mi) north-east of Jodhpur. Makrana is known for the part it has played in building the Taj Mahal by supplying marble, craftsmen and stonemasons to build the iconic UNESCO world heritage centre. It is one of the developing cities in the state. The marble from the town Makrana which is known as Makrana Marble, gets the GHSR status from the IUGS.
The United Nations General Assembly declared 2008 as the International Year of Planet Earth to increase awareness of the importance of Earth sciences for the advancement of sustainable development. UNESCO was designated as the lead agency. The Year's activities spanned the three years 2006–2009.
The Lesvos Petrified Forest is a petrified wood forest on the island of Lesbos, Greece.
Larvikite is an igneous rock, specifically a variety of monzonite, notable for the presence of thumbnail-sized crystals of feldspar. These feldspars are known as ternary because they contain significant components of all three endmember feldspars. The feldspar has partly unmixed on the micro-scale to form a perthite, and the presence of the alternating alkali feldspar and plagioclase layers give its characteristic silver-blue schiller effect on polished surfaces. Olivine can be present along with apatite, and locally quartz. Larvikite is usually rich in titanium, with titanaugite and/or titanomagnetite present.
GeoMôn UNESCO Global Geopark is a Geopark covering the entire island of Anglesey in north Wales. It was admitted to the European Geoparks Network and to the UNESCO-assisted Global Network of National Geoparks in May 2009. It was the second Geopark to be designated in Wales, the seventh within the United Kingdom and the thirty-third in Europe. The UNESCO Geopark designation reflects the diversity of the island's geology, which encompasses solid rocks from the Precambrian to the Neogene with some Miocene sediments and extensive Pleistocene glaciation features from the Quaternary period. GeoMôn covers 720 square kilometres and has 125 miles of coastal walks.
UNESCO Global Geoparks (UGGp) are geoparks certified by the UNESCO Global Geoparks Council as meeting all the requirements for belonging to the Global Geoparks Network (GGN). The GGN is both a network of geoparks and the agency of the United Nations Educational, Scientific and Cultural Organization (UNESCO). that administers the network.
Estremoz is a municipality in Portugal. The population in 2011 was 14,318, in an area of 513.80 km². The city Estremoz itself had a population of 7,682 in 2001. It is located in the Alentejo region.
Petit Granit is, despite its name, a grey-bluish limestone, rather than being a true Granite. It is mined exclusively in Belgium, where use of the name Petit Granit is subject to an Appellation d’Origine Locale designation. The stone becomes shiny black on polishing and is considered to be an easily worked and versatile dimension stone. It has also been used widely in sculpture and architecture, especially in Brussels and other Belgian cities. Petit Granit has been designated by the International Union of Geological Sciences as a Global Heritage Stone Resource.
The Geology of Malta consists of a sequence of sedimentary rocks of late Oligocene to late Miocene age cut through by a set of extensional faults of Pliocene age.
The Meghalayan age is the name given in 2018, by the International Commission on Stratigraphy, to the current age or latest geologic age – or uppermost stage of the Quaternary. It is also the upper, or latest, of three subdivisions of the Holocene epoch or series. This way of breaking down time is based only on geology; for example it is unrelated to the three age system of historical periods into which human development is sometimes divided.
Lioz, also known as Royal Stone, is a type of limestone, originating in Portugal, from the Lisbon region. It is famed for its use as an ornamental stone, resulting in its proliferation in palaces, cathedrals, and important civic buildings throughout Portugal and the former Portuguese Empire. Owing to its historical relevance, lioz was designated a Global Heritage Stone Resource.
Connemara marble or "Irish green" is a rare variety of green marble from Connemara, Ireland. It is used as a decoration and building material. Its colour causes it to often be associated with the Irish identity, and for this reason it has been named the national gemstone of Ireland. It strongly resembles the verd antique, a green serpentinite breccia found in the Mediterranean. It is named after the region in which it is found .. The marble was deposited as a limestone mud during the neoproterozoic.
