Varves Lamination Sedimentary Rock

The word varve derives from the swedish word varv whose meanings and connotations include revolution in layers and circle.

Varves lamination sedimentary rock.

Sedimentology experiments on lamination of sediments resulting from a periodic graded bedding subsequent to deposition a contribution to the explanation of lamination of various sediments and sedimentary rocks. Laminae are normally smaller and less pronounced than bedding. When sedimentary rocks have no lamination at all their structural character is called massive bedding. These types of lamination are attributed to successive deposits of layers.

This annual deposit may comprise paired contrasting laminations of alternately finer and coarser silt or clay reflecting seasonal sedimentation summer and winter within the year. Any sedimentary rock composed of millimeter or finer scale layers can be named with the general term laminite. Numerous fluviatile and marine sediments as well as sedimentary rocks showing the microstratified aspect are given such names as. The term first appeared as hvarfig lera on the first map produced by the geological survey of sweden in 1862.

Of the many rhythmites found in the geological record varves are one of. In geology lamination is a small scale sequence of fine layers that occurs in sedimentary rocks. Terms such as annually laminated are synonymous with varve. Laminae laminites varves etc.

A varve is any sedimentary bed or lamination deposit within the period of one year or any pair of contrasting laminae representing seasonal sedimentation as summer and winter within the period of one year. More beds and the term lamina is sometimes applied to a unit less than one centimetre in thickness. Initially varve referred to each of the separate components comprising a single annual layer in glacial lake sediments but at the 1910 geological congress the swedish geologist gerard de geer. A varve is an annual layer of sediment or sedimentary rock.

The value of varves as climatic and paleoclimatic proxies lies in 1 demonstration that they are annual deposits and therefore may be used to determine absolute chronology and 2 assessment that their sedimentary properties relate demonstrably to hydroclimatic processes. However structures from several millimetres to many centimetres have been described as laminae. Lamination is often regarded as planar structures one centimetre or less in thickness whereas bedding layers are greater than one centimetre. Varved deposit any form of repetitive sedimentary rock stratification either bed or lamination that was deposited within a one year time period.

Laminae that represent seasonal changes similar to tree rings are called varves. A single sedimentary rock can have both laminae and beds. A varve is an annual layer of sediment or sedimentary rock.