ribbed finish - ορισμός. Τι είναι το ribbed finish
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Τι (ποιος) είναι ribbed finish - ορισμός

LANDFORM OF RIDGES DEPOSITED BY A GLACIER OR ICE SHEET TRANSVERSE TO ICE FLOW
Ribbed moraines; Ribbed moraine
  • Lake Rogen, Sweden as seen from the north. The forested ridges in the lake are 'Rogen moraines' of which this is the type location

Fill and finish         
MANUFACTURING PROCESS
Fill finish; Fill-finish; Fill/finish
In the pharmaceutical industry, fill and finish (also referred to as fill finish, fill-finish or fill/finish) is the process of filling vials with vaccine and finishing the process of packaging the medicine for distribution. Many vaccine manufacturers use third parties to fill and finish their vaccines.
Rib vault         
  • Crossing vault of [[Seville Cathedral]] by [[Juan Gil de Hontañón]]
  • Keystone]] of a vault Church Notre-Dame in [[Morienval]], [[Oise]], (12th century)
  • alt=
ARCHITECTURAL ELEMENT
Ribbed vault; Net vault; Ploughshare vault; Qudripartite vault; Stellar vault; Quadripartite vault; Cross-ribbed vault; Ribbed vaulting; Rib vaulting
A rib vault or ribbed vault is an architectural feature for covering a wide space, such as a church nave, composed of a framework of crossed or diagonal arched ribs. Variations were used in Roman architecture, Byzantine architecture, Islamic architecture, Romanesque architecture, and especially Gothic architecture.
finish         
WIKIMEDIA DISAMBIGUATION PAGE
Finish (disambiguation); Finishes
¦ verb
1. bring or come to an end.
consume or get through the whole or the remainder of (food or drink).
reach the end of a race or other sporting competition.
(finish up) chiefly Brit. end by doing something or being in a particular position.
(finish someone off) kill or comprehensively defeat someone.
2. (finish with) have no more need for.
Brit. end a relationship with.
3. complete the manufacture or decoration of (something) by giving it an attractive surface appearance.
complete the fattening of (livestock) before slaughter.
4. dated prepare (a girl) for entry into fashionable society.
¦ noun
1. an end or final stage.
the place at which a race or competition ends.
2. the manner in which a manufactured article is finished.
the surface appearance of a manufactured article.
the final taste impression of a wine or beer.
Phrases
to the finish until the complete defeat of one of the participants.
Origin
ME: from OFr. feniss-, lengthened stem of fenir, from L. finire, from finis 'end'.

Βικιπαίδεια

Rogen moraine

A Rogen moraine (also called ribbed moraine) is a subglacially (i.e. under a glacier or ice sheet) formed type of moraine landform, that mainly occurs in Fennoscandia, Scotland, Ireland and Canada. It is one of the three main types of hummocky moraines. They cover large areas that have been covered by ice, and occur mostly in what is believed to have been the central areas of the ice sheets. Rogen moraines are named after Lake Rogen in Härjedalen, Sweden, the landform's type locality. Rogen Nature Reserve serves to protect the unusual area.

The landform occurs in groups that are often closely and regularly spaced. They consist of glacial drift, with till being the most common constituent. The individual moraines are large, wavy ridges orientated transverse to ice flow. Drumlins are often found in close proximity of Rogen moraines, and are often interpreted to be formed at the same time as the Rogen moraines. Although Rogen moraines can span a large range of sizes, the most common distribution seems to be 10–30 metres high, 150–300 metres wide and 300–1,200 metres long.

The exact mechanics of Rogen moraine formation are not known, but since the 1970s, several theories on the formation have been proposed:

  • Megaripples eroded in the basal ice fill during subglacial outburst floods.
  • Already existing landforms, such as drumlins and flutes or marginal moraines are reshaped due to a ≈90° change in the direction of the ice flow.
  • Debris-rich basal ice or pre-existing sediments are sheared and stacked, or folded during compressive ice flow.
  • Shearing of sediment under a glacier causes growth of waves with spacing characteristic of Rogen moraine (300 m to 1000 m).
  • Sediment sheets become fractured and extended during a transition of the overlying glacier from being cold based ice to warm based.

However, it has been suggested that, due to the diversity of morphological characteristics displayed by Rogen moraine, different processes might be able to create the landform. This means that all of the processes mentioned above might be correct. The different theories that proposed a formation near or at the glacial margin have largely been abandoned. Some of these theories proposed that Rogen moraines had an origin as a series of end moraines, that they formed in association with calving ice termini in glacial lakes, or that Rogen moraines formed in dead-ice, where supraglacial material fell down into crevasses in the ice.