Welcome to Anagrammer Crossword Genius! Keep reading below to see if iceless is an answer to any crossword puzzle or word game (Scrabble, Words With Friends etc). Scroll down to see all the info we have compiled on iceless.
iceless
Searching in Crosswords ...
The answer ICELESS has 6 possible clue(s) in existing crosswords.
Searching in Word Games ...
The word ICELESS is VALID in some board games. Check ICELESS in word games in Scrabble, Words With Friends, see scores, anagrams etc.
Searching in Dictionaries ...
Definitions of iceless in various dictionaries:
adj - having no ice
Word Research / Anagrams and more ...
Keep reading for additional results and analysis below.
| Possible Crossword Clues |
|---|
| Without rocks |
| Straight, in a way |
| Straight up |
| Neat |
| Not slippery at all, as a winter road |
| Neat, like a mixed drink |
| Last Seen in these Crosswords & Puzzles |
|---|
| Jun 28 2016 New York Times |
| May 30 2007 The A.V Club |
| Jul 2 2006 New York Times |
| Feb 17 2006 Newsday.com |
| Jun 27 1999 New York Times |
| Mar 22 1998 New York Times |
| Possible Dictionary Clues |
|---|
| Without ice. |
| Iceless might refer to |
|---|
| Ice lenses are bodies of ice formed when moisture, diffused within soil or rock, accumulates in a localized zone. The ice initially accumulates within small collocated pores or pre-existing crack, and, as long as the conditions remain favorable, continues to collect in the ice layer or ice lens, wedging the soil or rock apart. Ice lenses grow parallel to the surface and several centimeters to several decimeters (inches to feet) deep in the soil or rock. Studies between 1990 and present have demonstrated that rock fracture by ice segregation (i.e., the fracture of intact rock by ice lenses that grow by drawing water from their surroundings during periods of sustained subfreezing temperatures) is a more effective weathering process than the freeze-thaw process which older texts proposed.Ice lenses play a key role in frost induced heaving of soils and fracture of bedrock, which are fundamental to weathering in cold regions. Frost heaving creates debris and dramatically shapes landscapes into complex patterns. Although rock fracture in periglacial regions (alpine, subpolar and polar) has often been attributed to the freezing and volumetric expansion of water trapped within pores and cracks, the majority of frost heaving and of bedrock fracture results instead from ice segregation and lens growth in the near-surface frozen regions. Ice segregation results in rock fracture and frost heave. |