Costa Rica vs Faroe Islands: Cropland organic soils — Area
Costa Rica
860.57 ha
in 2024
Faroe Islands
563.66 ha
in 2024
Costa Rica rank
87th
Faroe Islands rank
90th
Cropland organic soils — Area over time
- Costa Rica
- Faroe Islands
How they compare
Costa Rica currently reports 860.57 ha against 563.66 ha in Faroe Islands, a difference of 296.91 ha.
That makes Costa Rica's figure about 1.5 times Faroe Islands's.
Across all 35 years both countries report, Costa Rica has been ahead every year.
Costa Rica ranks 87th and Faroe Islands ranks 90th of 221 countries.
Costa Rica has averaged higher in every one of the 4 decades both report.
Head to head by decade
| Decade | Costa Rica | Faroe Islands | Difference | Ahead |
|---|---|---|---|---|
| 1990s | 1,677 ha | 467.78 ha | 1,209 ha | Costa Rica |
| 2000s | 1,547 ha | 467.78 ha | 1,079 ha | Costa Rica |
| 2010s | 1,322 ha | 473.52 ha | 848.17 ha | Costa Rica |
| 2020s | 860.57 ha | 563.66 ha | 296.91 ha | Costa Rica |
Averages of every year both report within each decade.
Frequently asked questions
- Which has higher cropland organic soils — area, Costa Rica or Faroe Islands?
- Costa Rica, at 860.57 ha against 563.66 ha in Faroe Islands as of 2024.
- What is the difference in cropland organic soils — area between Costa Rica and Faroe Islands?
- 296.91 ha, with Costa Rica ahead.
- How many years of comparable data are there for Costa Rica and Faroe Islands?
- 35 years are reported by both, from 1990 to 2024.
- How do Costa Rica and Faroe Islands rank globally for cropland organic soils — area?
- Costa Rica ranks 87th and Faroe Islands ranks 90th of 221 countries.
- Where does this data come from?
- Food and Agriculture Organization of the United Nations, published as Cropland organic soils — Area. Statizoid refreshes it automatically from the source and publishes the full history for both places.
Individual pages
About this data
The FAOSTAT domain on Emissions from drained organic soils consists of nitrous oxide (N2O) and carbon dioxide (CO2) emissions generated from the mineralization and oxidation of organic matter in organic soils that are drained for agricultural activities.