Administratum Planetary Surveys
Vhoorl Planetary Survey
Binary Star AL-Janubi
Personal Log: Donovan Gilman, Lead Planetologist
Planet Vhoorl, strategically located on the edge of Segmentum Obscurus is an earth-like planet in many respects. Atmosphere composed primarily of Nitrogen and oxygen, slightly richer in oxygen than Terra with a gravity approx 4/5s that of Terra.
The planet is majority water with two primary land masses, a northern and southern continent. The ocean separating the continents is primarily salt water.
The Northern Continent has an extensive river system, with eight major drainage basins, all of which drain into the ocean. Two of these basins account for more than half the total drainage area. The largest river system in the Northern Continent originates in a mountainous region and receives tributaries from a basin that covers 45.7% of the continent, principally the north and west. The main river system flows from west to east. Through this basin flows one-fifth of Vhoorls fresh water. This system provides a sufficient supply of potable water for the hive city, Astra Militarum garrison and cooling for the factories.
Although 90% of the continent is within the tropical zone, the climate varies considerably from the mostly tropical North to temperate zones below the 23°27′ S latitude. The Northern Continent has five climatic regions: equatorial, tropical, semiarid, highland tropical, and subtropical.
Temperatures along the equator are high, averaging above 25 °C (77 °F), but not reaching the summer extremes of up to 40 °C (104 °F) in the temperate zones. There is little seasonal variation near the equator. At the country’s other extreme, there are frosts south of the 23°27′ S latitude during the winter and there is snow in the mountainous areas. Temperatures outside the Hive City are moderate (usually between 15 and 30 °C or 59 and 86 °F), despite their relatively low latitude, because of their elevation of approximately 1,000 meters (3,281 ft). The coast has warm climates, with average temperatures ranging from 23 to 27 °C (73.4 to 80.6 °F), but enjoys constant winds. The southern coast has a subtropical climate and temperatures can fall below freezing in winter.
Precipitation levels vary widely. The Northern Continent has moderate rainfall of between 1,000 and 1,500 millimetres (39.4 and 59.1 in) a year, with most of the rain falling in the summer south of the Equator. The region is notoriously humid, with rainfall generally more than 2,000 millimetres (78.7 in) per year and reaching as high as 3,000 millimetres (118.1 in) in parts of the western side of the continent. Despite high annual precipitation, the rain forest can have a three- to five-month dry season, the timing of which varies according to location north or south of the equator.
In contrast to the Southern Continent which rose to elevations of nearly 17,000 meters (55774.3 ft) in a relatively recent epoch and inverted the river flows direction of flow from westward to eastward, the Northern continent geological formation is very old. Crystalline shields cover 36% of the territory, especially its central area. The dramatic granite sugarloaf mountains are an example of the terrain of the shield regions, where continental basement rock has been sculpted into towering domes and columns by tens of millions of years of erosion, untouched by mountain-building events.
The principal mountain ranges average elevations just under 3,500 meters (11482.9 ft). The Murum Mar range hugs the eastern coast, and the Murrum Medius Range, the largest in area, extends through the south-central part of the continent. The highest mountains are in this range, others traverse the northern border.
In addition to mountain ranges (about 0.5% of the country is above 1,200 m or 3,937 ft), the Northern Central Highlands include a vast central plateau (Planalto Central). The plateau’s uneven terrain has an average elevation of 1,000 meters (3,281 ft). The rest of the territory is made up primarily of sedimentary basins.
The Southern Continents main structural lines show both the east-to-west direction characteristic, at least in the eastern hemisphere, of the more northern parts of the world, and the north-to-south direction seen in the southern peninsulas. The Southern Continent is thus mainly composed of two segments at right angles, the northern running from east to west, and the southern from north to south.
With a heavily grown rainforest and has not been extensively explored at this time. Orbital surveys have shown extremely high mountain ranges circling the central portion of the continent, pictures of which provide the suggestion of jagged teeth biting their way through the planet. The forest canopy prevents the penetration of any light creating a perpetual twilight gloom.
Mean monthly temperatures exceed 18 °C (64 °F) during all months of the year. Average annual rainfall is no less than 168 cm (66 in) and can exceed 1,000 cm (390 in) although it typically lies between 175 cm (69 in) and 200 cm (79 in).
The highest of these peaks reaches nearly 17,000 meters (55774.3 ft). Mons Imperalis as it has been deemed is about two thirds the height of Olympus Mons on Mars.
Inside the ring of mountains, appear the outlines of an ancient city. Preliminary review and exploration by the planetary geologist assigned to the colonization and establishment of munitoriums on Vhoorl indicate the city appears intact and is made of a black rock which may not be native to the planet.
A xeno-archeologist has been requested for further review. All exploration of the Southern Continent has been placed on hold pending his arrival. As a footnote the geologist came down with a strange malady after the visit to the Southern Continent. In his delirium he even decried his faith in the Emperor and was exterminated before further contamination could occur.
Thank you for reading,