structural geology
dororieth kesweythel
geology oor Kornies
geology
en
The science that studies the structure of the earth (or other planets), together with its origin and development, especially by examination of its rocks
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en
scientific discipline
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Geology
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geology [ s ]
Res o dhyn mos ena war-barth.langbot langbot
geology
Yth esov vy owth assaya gul henna.langbot langbot
geology
Res yw dhis dalleth!langbot langbot
engineering geology
Re domm o an dowr de.langbot langbot
petroleum geology
My a vetyas orth ow hothman.langbot langbot
geology
Seytek bloodh yw Helen.langbot langbot
A dwarf planet is a small planetary-mass object that is in direct orbit of the Sun – something smaller than any of the eight classical planets, but still a world in its own right. The prototypical dwarf planet is Pluto. The interest of dwarf planets to planetary geologists is that, being possibly differentiated and geologically active bodies, they may display planetary geology, an expectation borne out by the Dawn mission to Ceres and the New Horizons mission to Pluto in 2015. Counts of the number of dwarf planets among known bodies of the Solar System range from 5-and-counting (the IAU)[1] to over 120 (Runyon et al).[2] Apart from Sedna, the largest ten of these candidates have either been visited by spacecraft (Pluto and Ceres) or have at least one known moon (Pluto, Eris, Haumea, Makemake, Gonggong, Quaoar, Orcus, and Salacia), which allows their masses and thus an estimate of their densities to be determined. Mass and density in turn can be fit into geophysical models in an attempt to determine the nature of these worlds. The term dwarf planet was coined by planetary scientist Alan Stern as part of a three-way categorization of planetary-mass objects in the Solar System: classical planets, dwarf planets and satellite planets. Dwarf planets were thus conceived of as a category of planet. However, in 2006 the concept was adopted by the International Astronomical Union (IAU) as a category of sub-planetary objects, part of a three-way recategorization of bodies orbiting the Sun: planets, dwarf planets and small Solar System bodies.[3] Thus Stern and other planetary geologists consider dwarf planets and satellite planets to be planets,[4] but since 2006 the IAU and perhaps the majority of astronomers have excluded them from the roster of planets.
Yma dhywgh lies lyver.langbot langbot
structural geology
Losow a dyv.langbot langbot
geology
Yw hemma dha garr?langbot langbot
planetary geology
Pyth es’ta ow hwilas?langbot langbot
geology
Kas yw genev pel droos.langbot langbot
geology
Hi yw pymp bloodh.langbot langbot
geology
Megi difennys!langbot langbot
Glaciology (from Latin: glacies, "frost, ice", and Ancient Greek: λόγος, logos, "subject matter"; literally "study of ice") is the scientific study of glaciers, or more generally ice and natural phenomena that involve ice. Glaciology is an interdisciplinary Earth science that integrates geophysics, geology, physical geography, geomorphology, climatology, meteorology, hydrology, biology, and ecology. The impact of glaciers on people includes the fields of human geography and anthropology. The discoveries of water ice on the Moon, Mars, Europa and Pluto add an extraterrestrial component to the field, which is referred to as "astroglaciology".
Ro dhyn diw gollel ha peder forgh, mar pleg.langbot langbot
geology
Hi eth dhe’n cinema ganso.langbot langbot
A wide variety of maps can also be found in the Cornwall Council archives, including maps showing land use and geology.
Dohajydh da!langbot langbot
glacial geology
Yma tri flogh dhodho.langbot langbot
A wide variety of maps can also be found in the Cornwall Council archives, including maps showing land use and geology. We also hold a wide range of Admiralty charts, showing ports and harbours around the coast.
Ny allav vy klewes yn ta.langbot langbot
The geologic time scale, or geological time scale, (GTS) is a representation of time based on the rock record of Earth. It is a system of chronological dating that uses chronostratigraphy (the process of relating strata to time) and geochronology (scientific branch of geology that aims to determine the age of rocks). It is used primarily by Earth scientists (including geologists, paleontologists, geophysicists, geochemists, and paleoclimatologists) to describe the timing and relationships of events in geologic history. The time scale has been developed through the study of rock layers and the observation of their relationships and identifying features such as lithologies, paleomagnetic properties, and fossils. The definition of standardized international units of geologic time is the responsibility of the International Commission on Stratigraphy (ICS), a constituent body of the International Union of Geological Sciences (IUGS), whose primary objective is to precisely define global chronostratigraphic units of the International Chronostratigraphic Chart (ICC) that are used to define divisions of geologic time. The chronostratigraphic divisions are in turn used to define geochronologic units. While some regional terms are still in use, the table of geologic time presented in this article conforms to the nomenclature, ages, and color codes set forth by the ICS as this is the standard, reference global geologic time scale – the International Geological Time Scale.
Ny gar hi den vyth ha ny’s kar den vyth.langbot langbot
The spiritual traditions associated with natural wells and springs; those places where life-sustaining water ‘magically’ appears from the ground, pervade native cultures all over the World. Cornwall and the Isles Of Scilly, with it’s unique geology has many such places and this book, first published in 1894 seeks to provide a record of the traditions and beliefs, Chrisitian and Pagan which survived in the memories of the folk dwelling around them.
Prag y fynn'ta prena an lyverma?langbot langbot
geology
My a’th kar!langbot langbot
historical geology
My a vynn ri dhodho y lyver a-vorow.langbot langbot
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