Hilo (soil)

Today, Hilo (soil) is a topic that arouses great interest and debate in society. From its origins to the present, Hilo (soil) has been the subject of study and analysis by experts from different disciplines. Its impact on people's lives and on the development of humanity has been profound, and its relevance has remained over time. In this article, we will explore in detail the most relevant aspects of Hilo (soil), from its origins to its implications today. From his impact on society to his influence on popular culture, Hilo (soil) has left an indelible mark on history and on people's minds.

Hilo
Hilo soil profile, Summer 2009
lnceptisols
Parent materialVolcanic ash
ClimateHamakua coast, Hawaii
pH5.5

Hilo soil is the official state soil of the state of Hawaii. These soils cover about 21,000 acres (85 km2) and are considered prime agricultural land. 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. 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. Hilo soils occur on the uplands of the Mauna Kea volcano along the Hāmākua Coast on the island of Hawaii.

See also

References

  1. ^ a b "Official Series Description - HILO Series". soilseries.sc.egov.usda.gov. Retrieved 2023-09-28.
  2. ^ "Official Series Description - HILO Series". soilseries.sc.egov.usda.gov. Retrieved 2023-09-28.
  3. ^ Sato, Harry H. (2007-06-09). "Soil Survey of the Island of Hawaii, State of Hawaii". Archived from the original on 2007-06-09. Retrieved 2023-09-28.