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The phrase "alternate bed" is correct and usable in written English.
It can be used to refer to a different bed that is used as a substitute or in rotation with another bed, often in contexts like travel or shared living arrangements.
Example: "When traveling, I prefer to have an alternate bed ready in case my first choice is unavailable."
Alternatives: "replacement bed" or "substitute bed".
Exact(1)
If there is an unused baby crib in the house and you figure there to be a possibility of other babies coming, roll it into an area and provide the adult chaperone to sleep on an alternate bed nearby.
Similar(58)
Pipalkoti Formation consists of alternate beds of slate, dolomite and dolomitic limestone, while the Berinag Formation consists of quartzite, orthoquartzite and amphibolites (basic rocks).
The upper and middle parts of the river basin are predominated by alternate beds of clay and cobbles, pebbles, gravel, sand.
Toddlers and young school-age children should use these alternate beds instead of the floor or crib in any and all cases.
Toddlers and young school-age children however, should use these alternate beds instead of the floor in any and all cases.
d Alternated beds of sand and mud of the lower part of the Sunakothi Formation at Sunakothi.
Phyllites of alternating beds of sandstone and shale make up the hanging wall Kitagawa group (0 to 41.3 mbgs) (Figure 2a).
Deformation structures such as phyllitic cleavages, kink folds of alternating beds of sandstones and shales, and quartz-carbonate veins characterize the hanging wall.
Catastrophic landslides observed along or below the rims of paleosurfaces were preceded by buckling of alternating beds of sandstone and shale.
From 2.94 to 2.77 m b.s. the sediment consists of thin alternating beds of carbonate sand (light brown) and grey layers of silty clay, both containing gypsum and halite crystals.
Geological investigations suggest that there are two dominant types of DGSD: one is flexural toppling of slate and argillite with high-angle cleavage, and the other is buckling of alternating beds of sandstone and mudstone on parallel or underdip cataclinal slopes.
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