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Board game

Permainan berpapan

Last Update: 2014-04-15
Usage Frequency: 9
Quality:
Reference: Wikipedia

Mother board

Papan induk

Last Update: 2013-10-03
Usage Frequency: 1
Quality:
Reference: Wikipedia

Board member

Lembaga pengarah

Last Update: 2013-01-23
Usage Frequency: 1
Quality:
Reference: Wikipedia

Black board

Papan hitam

Last Update: 2012-12-09
Usage Frequency: 1
Quality:
Reference: Wikipedia

Skate board

Papan luncur

Last Update: 2012-06-21
Usage Frequency: 1
Quality:
Reference: Wikipedia

Composite board
http://aims.fao.org/standards/agrovoc

Papan komposit
http://aims.fao.org/standards/agrovoc

Last Update: 2013-06-12
Subject: Agriculture and Farming
Usage Frequency: 1
Quality:

Board of directors

Lembaga pengarah

Last Update: 2014-03-21
Usage Frequency: 2
Quality:
Reference: Wikipedia

Printed circuit board

Papan litar tercetak

Last Update: 2014-02-18
Usage Frequency: 1
Quality:
Reference: Wikipedia

k board not working

mesej

Last Update: 2013-12-07
Subject: General
Usage Frequency: 1
Quality:
Reference: Anonymous

Command™ Mounting Products
http://solutions.3m.com/wps [...] ds/index.html

Produk Command™ Mounting
http://solutions.3m.com/wps [...] ds/index.html

Last Update: 2011-02-26
Usage Frequency: 1
Quality:

Board of language and literature

kesempurnaan

Last Update: 2011-06-08
Subject: General
Usage Frequency: 1
Quality:

What processors does this board support

ADJUNCT PROFESSOR

Last Update: 2013-07-28
Subject: General
Usage Frequency: 1
Quality:
Reference: Anonymous

Circuit board

Papan litar tercetak nn

Last Update: 2013-09-16
Usage Frequency: 1
Quality:
Reference: Wikipedia

Mount Sumbing

Gunung Sumbing

Last Update: 2014-04-12
Usage Frequency: 1
Quality:
Reference: Wikipedia

citchat5.2 Shore platforms Many cliffs are bordered by shore platforms that extend across the intertidal zone. They have been shaped by the various processes described in the previous section. The term wave-cut platform should be restricted to features shaped entirely by the hydraulic action of waves, usually seen only on soft rock formations such as clay. Erosional processes such as abrasion by waves armed with sand or gravel, tidal scour and weathering have contributed to the shaping of most shore platforms. Generally these processes operate slowly, and the presence of a shore platform indicates that the coast has been relatively stable for asubstantial period, perhaps the whole of the time (up to 6000 years) that the sea has stood at its present level in Holocene times. Laboratory simulations of weathering and erosion processes on shore platforms have been conducted by Moses et al. (2006). Some shore platforms are seaward sloping, others subhorizontal, with a sharp drop at the outer edge; some are structural in the sense that they coincide with the upper surface of a resistant formation(which may be horizontal or gently sloping). Seaward sloping shore platforms (Figure 5.5(a)) are usually planation surfaces (cut across shore structures) that extend from the high tide line at the base of the cliff to a level below and beyond the low tide line. It has been suggested that a shore platform of this kind may be bordered by a wave-built terrace constructed by deposition at its outer margin, but although this can be found on some lake and reservoir shores such a nearshore terrace is rarely formed off sea coasts (Dietz, 1963). Structural shore platforms (Figure 5.6) coincide with the upper surfaces of resistant rock formations that may dip seaward, landward or alongshore. There are also more or less horizontal shore platforms, standing close to high tide level (submerged only briefly at high tides), which may have a sharp drop or low tide cliff(of- ten>3m)at these award edge. These are termed high tide shore platforms (Figure 5.5(b)). Similar subhorizontal shore platforms are found close to low tide level (submerged for most of the tidal cycle), particularly on lime stones, and generally these also end seaward in a sharp drop: they may be termed low tide shore platforms (Figure 5.5(c)). Shore platforms that are narrow (up to about 10 m wide) are called benches, and may be structural ledges coinciding with the outcrop of a resistant rock formation. On some coasts the shore topography includes sloping ramps and flat segments, as well as steps or micro cliffs, uprising ridges and stacks, and dissecting features such as grooves, gulches and clefts. In high latitudes, particularly in Scandinavia, there are strand flats (Section 5.2.5), almost flat shore platforms that grade land- ward into gently shelving coastal plains. Some shore platforms are of artificial origin, as on the shores of Valetta Harbour in Malta. Finally, there are coasts where cliffs descend into deep water close inshore without any platforms or intertidal rocky areas. These are termed plunging cliffs (Figure 5.5(d)), and will be discussed after the evolution of shore platforms has been considered. There is the problem of how smooth and continuous a planed rock surface should be for the term shore platform to be applied. Many shore platforms are dissected by grooves and channels, or diversified by small rising outcrops. As these increase in dimensions it may be more appropriate to use the terms incipient shore platform (with higher residual ridges and stacks) or dissected shore platform (with wide trans- verse gulches and furrows parallel to the coastline). It is difficult to define these quantitatively, but one suggestion is that the term shore platform should be used only where the platform surface is sufficiently well formed, intact and un dissected for a four-wheel drive vehicle to be driven across it. Where less than 10 per cent of the shore is a smooth platform and the rest irregular the term rocky shore could be used. The various kinds of shore platform and rocky shore may vary along the coast in relation to geology, aspect and morphogenic factors such as tide range and wave regime. Contrasts in shore profile related to geology are evident where there are varied geological outcrops along a coastline and other factors are relatively uniform, and contrasts related to morphogenic factors may occur on a particular rock outcrop, especially fringing headlands and islands. Such contrasts have been analysed along the southern New South Wales coast (Bird and Dent, 1966) and along the Victorian coast (Hills,1971) in SE Australia. Shore platforms may vary in relation to lateral changes in rock resistance. This is well illustrated on the coast at Mount Martha, Port Phillip Bay, Australia, where the coast intersects a granodiorite intrusion, the upper part of which has been strongly weathered and decomposed to clay. Where the clay descends to sea level at the northern and southern ends of the intrusion there are irregular receding cliffs, fronted by seaward sloping abrasion ramps, but in the central sector, where the granodiorite is more resistant, it forms steep cliffs that descend into deep near shore water (Jutson, 1940).

citchat

Last Update: 2014-04-09
Subject: General
Usage Frequency: 1
Quality:
Reference: Anonymous
Warning: Contains invisible HTML formatting

The CAG process is normally manually operated. The apparatus can be mounted on a travel carriage. This is considered machine cutting or gouging. Special applications have been made where cylindrical work has been placed on a lathe-like device and rotated under the air carbon arc torch. This is machine or automatic cutting, depending on operator involvement.

Mekanikal

Last Update: 2013-10-25
Subject: General
Usage Frequency: 1
Quality:
Reference: Anonymous

Mount Arafat

Arafah

Last Update: 2013-10-17
Usage Frequency: 1
Quality:
Reference: Wikipedia

Particle boards
http://aims.fao.org/standards/agrovoc

Papan zarah
http://aims.fao.org/standards/agrovoc

Last Update: 2013-06-12
Subject: Agriculture and Farming
Usage Frequency: 1
Quality:

Chalk boards

Papan hitam

Last Update: 2012-10-06
Usage Frequency: 1
Quality:
Reference: Wikipedia

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