What does ashram mean?

What does ashram mean?

1 : a secluded dwelling of a Hindu sage also : the group of disciples instructed there. 2 : a religious or spiritual retreat.

What does sociability mean?

1 : inclined by nature to companionship with others of the same species : social. 2a : inclined to seek or enjoy companionship. b : marked by or conducive to friendliness or pleasant social relations. sociable.

What is the spirit of torment?

The masked creatures known as Spirit Torments were pitiless jailers in life. In death they seek out those that Nagash deems his by right of rulership, bludgeoning them with their ensorcelled iron padlocks before locking away their souls.

What does Hummock mean?

1 : a rounded knoll or hillock. 2 : a ridge of ice.

What is a Humicks?

In geology, a hummock is a small knoll or mound above ground. They are typically less than 15 meters (50 ft) in height and tend to appear in groups or fields. It is difficult to make generalizations about hummocks because of the diversity in their morphology and sedimentology.

What is hummocky topography?

‘Hummocky topography’ is a non‐genetic, descriptive term applied to landscapes with irregular hills and depressions. This term implies that the hummocky topography was formed by the melt‐out and collapse of supraglacial till, during the melting of stagnant ice (Gravenor & Kupch, 1959, Boulton, 1972).

What is hummocky moraine?

Ablation moraines form where rock and sediment debris accumulate on the glacier surface near the margin and subsequently undergo melt-out4,11. When a debris-covered snout melts over time material is gradually let down from the ice surface to produce an area of ‘hummocky moraine’.

What causes a Drumlin?

Drumlin, oval or elongated hill believed to have been formed by the streamlined movement of glacial ice sheets across rock debris, or till.

What are hummocks made of?

(1) [sea ice] a smooth hill of ice that forms on the sea ice surface from eroding ridges, particularly during the summer melt; the formation of hummocks is similar to young mountain peaks with steep slopes that erode into smooth, rolling hills.

What does Thermokarst mean?

Periglacial Processes in Glacial Environments Thermokarst is an erosional process unique to permafrost with excess ice; it is defined as ‘the process by which characteristic landforms result from the thawing of ice-rich permafrost and/or melting of massive ice’ (van Everdingen, 1998).

How does hummocky cross stratification form?

Hummocky cross-stratification is a type of sedimentary structure found in sandstones. It is a form of cross-bedding usually formed by the action of large storms, such as hurricanes. It is only formed at a depth of water below fair-weather wave base and above storm-weather wave base.

How is hummocky terrain formed?

Hummocky terrains in Gusev Crater, Mars, are interpreted to be Martian counterparts of deglaciated terrestrial hummocky landscapes and formed by sublimation of ice-rich deposits, leaving behind poorly sorted, angular debris (Gregg et al. 2007). Hummocky moraines ( Moraine-mound complexes) are deglaciated surfaces.

What do ripple marks signify?

In geology, ripple marks are sedimentary structures (i.e., bedforms of the lower flow regime) and indicate agitation by water (current or waves) or wind.

What is Swaley cross stratification?

B: Swaley cross-stratification (SCS) was introduced by Leckie and Walker (1982, p. 143) to describe “a series of superimposed concave-upward shallow scours about 0.5–2 m wide and a few tens of centimeters deep” observed in fine to medium sandstone.

Where are hummocky cross stratification found?

Hummocky cross stratification (Fig. 18) is commonly found in finer-grained sediments. The structure comprises low angle laminations that drape over peaks and troughs of underlying bedforms.

What is ripple cross lamination?

Quick Reference. The form of cross-lamination (see crossstratification) produced by the migration of wave-generated ripples, or combined flow ripples (i.e. ripples formed by a combination of wave action and unidirectional flow).

What causes convolute bedding?

Convolute bedding forms when complex folding and crumpling of beds or laminations occur. This type of deformation is found in fine or silty sands, and is usually confined to one rock layer. This deformation is caused from sand being deposited onto mud, which is less dense.

How do laminations form?

Lamination consists of small differences in the type of sediment that occur throughout the rock. They are caused by cyclic changes in the supply of sediment. It can occur in many different types of sedimentary rock, from coarse sandstone to fine shales, mudstones or in evaporites.

What is horizontal lamination?

Laminae are defined as sedimentary strata that are less than 10 mm thick, according to McKee and Weir (1953). Hence, planar lamination has also been called horizontal lamination, even lamination and parallel lamination.

What are laminators?

A heated roll laminator uses heated rollers to melt glue extruded onto lamination film. This film is in turn applied to a substrate such as paper or card using pressure rollers. The primary purpose of laminating with such a machine is to embellish or protect printed documents or images.

What is the difference between stratification and lamination?

comparison with stratification Thus, lamination consists of thin units in bedded, or layered, sequence in a natural rock succession, whereas stratification consists of bedded layers, or strata, in a geologic sequence of interleaved sedimentary rocks.