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Regolith is a mass of weathered material that is charged
Regolith is thin
Regolith is thus constantly being bombarded by the solar wind
Regolith is the surface layer of rocky solar system bodies which is created by destruction of the uppermost rock layer
Regolith is a few meters per 10 years
Regolith is a function of the ilmenite content
Regolith is not affected by impacts
Regolith is syn
Regolith is sufficiently large to
Regolith is formed on earth and on the moon
Regolith is overturned or mixed
Regolith is considerably more
Regolith is switched on
Regolith is defined as "unconsolidated earth material above bedrock"
Regolith is formed in the same way
Regolith is formed on the moon and on the earth? key ideas
Regolith is commonly used to refer to the surficial layer
Regolith is made up of soils
Regolith is composed of rock particles that have been broken down from the original bedrock beneath the soil surface
Regolith is solid and brittle
Regolith is the weathered rind of the earth's crust
Regolith is thin and turnover is slow
Regolith is discussed
Regolith is sufficient to reduce radiation to the level we experience on the surface of the earth
Regolith is in desired
Regolith is rarely seen
Regolith is equal to 1%
Regolith is relatively transparent to the radio
Regolith is rich in sulphur
Regolith is altered by exposure to the space environment over time
Regolith is surficial
Regolith is launched into llo in "smart" projectiles using a rotary mass launcher with two "rotors
Regolith is recognised as a major impediment to diamond exploration across many parts of australia
Regolith is saturated with saline
Regolith is the main object of human impact and "victim" of many natural catastrophes
Regolith is idealized as a single layer of uniform properties
Regolith is initially 1 m thick
Regolith is dumped=20 into a reactor cell
Regolith is dumped in
Regolith is the explanation for the
Regolith is capable of providing us information on the elemental and isotopic abundance ratio of the solar wind and the sun
Regolith is held behind a door until the shuttle reaches orbit
Regolith is the layer of broken and unconsolidated rock and soil material that forms the surface of the land and covers the bedrock nearly everywhere
Regolith is developed which lacks large blocks
Regolith is dominantly weathered granite with corestones
Regolith is re
Regolith is a layer made of unconsolitaded debris coming from the numerous impacts of meteorites
Regolith is another word for soil on
Regolith is the term used to describe the complex zone of interaction between rocks
Regolith is the unconsolidated material sitting above bedrock
Regolith is referred to as impact gardening
Regolith is stable on
Regolith is poorly bound together
Regolith is the layer rock or blanket of unconsolidated debris of any thickness that overlies bedrock and forms the surface of the land
Regolith is saturated with craters
Regolith is a very important technique necessary for many soil uses and planning applications
Regolith is 'shaked' out evenly on passing trays so it can be spectrophotomically analyzed for its' mineral content
Regolith is crucial in the elucidation of a landscape's development
Regolith is formed by physical disaggregation of welded tuff
Regolith is frozen
Regolith is very important in groundwater development as it is able to provide a cheap and more sustainable source of water supply and can
Regolith is more susceptible than bedrock to this process
Regolith is of resource utilization interest and is an indicator of Regolith maturity
Regolith is the principal component of soil
Regolith is a mass of weathered material that is
Regolith is presumed to be
Regolith is stable on the
Regolith is just about 100m
Regolith is that deposited by some geologic agent;
Regolith is simply the debris created by meteorites striking the moon at high velocity
Regolith is now known to be a critical element in
Regolith is rich in blobs and spherules of glass
Regolith is less dense than limestone
Regolith is dominated by alluvial and colluvial
Regolith is discussed in many of the papers prepared for the 17th international geochemical exploration symposium of 15
Regolith is a thin covering of loose rock debris that has formed as a result of a process called weathering
Regolith is often referred to in general terms as a landslide
Regolith is most likely to occur where the Regolith is thick and relatively impermeable with few large cracks
Regolith is a metastable system in which mineral phases undergo processes of destabilisation and breakdown
Regolith is the layer of dust and fragmented rock produced by meteor impacts that covers the uppermost surfaces of most moons
Regolith is the source of sediment carried by wind
Regolith is the source for sediment that are transported and deposited in a fluid medium
Regolith is ubiquitous to the surface of the volatile depleted lunar environment and is composed of a wide array of anhydrous silicates and accessory
Regolith is the second most common Regolith type
Regolith is composed in a large part by oxides of silicon and other metals
Regolith is controlled by closed
Regolith is diverse
Regolith is a wealth of raw material
Regolith is the layer of weathered rock fragments covering much of the earth’s surface
Regolith is all stuff on top of hard rock
Regolith is old with saprolites ranging from palaeogene to late cretaceous
Regolith is very small
Regolith is
Regolith is delineated its description is generalised or it is depicted as homogenous in character
Regolith is a relatively immature
Regolith is struck by