Hilo (soil) explained

Hilo
Type:lnceptisols
Parent Material:Volcanic ash
Climate:Hamakua coast, Hawaii
Ph:5.5

Hilo soil is the official state soil of the state of Hawaii. These soils cover about 21000acres and are considered prime agricultural land.[1] The Hawaiian definition of the word “Hilo” is “first night after the new moon.” Also, the word is the Polynesian term for “Navigator,” and the name of a town, Hilo, Hawaii.

Profile

The Hilo soil series consists of very deep, moderately well drained soils that formed in many layers of volcanic ash with lesser amounts of dust from the deserts of central Asia.[2] These dust layers are noticeable because their gray color contrasts with the dark brown and dark reddish brown subsoil formed in volcanic ash. There are several buried layers within the Hilo soil profile.[3] Hilo soils occur on the uplands of the Mauna Kea volcano along the Hāmākua Coast on the island of Hawaii.

See also

References

Notes and References

  1. Web site: Official Series Description - HILO Series . 2023-09-28 . soilseries.sc.egov.usda.gov.
  2. Web site: Official Series Description - HILO Series . 2023-09-28 . soilseries.sc.egov.usda.gov.
  3. Web site: Sato . Harry H. . 2007-06-09 . Soil Survey of the Island of Hawaii, State of Hawaii . 2023-09-28 . https://web.archive.org/web/20070609163001/http://www.ctahr.hawaii.edu/soilsurvey/Hawaii/Htm/howmade.htm . 2007-06-09 .