Forged Earth
'Forged Earth' - 5th planet of it's system - is home to a Human society descendant from pre-warp colonists who left Earth in the mid 22nd Century; discovered by Starfleet in late 2417. It is one of two M-Class worlds in the system; the second of which - Newfrika - hosts a significant mining operation in support of the primary colony.
The planet is dominated by two major continents - North & South - with the core of the colony built around numerous cities in the northern continent, whilst the Southern continent plays host to more rural settings and coastal tourism destinations. The most developed of said population centers is the capital city - The Valley - which has developed around the crash site of the original colony vessel (a site which is now home to something resembling a cathedral), though the landscape is distinctly more dominated now by the FEPD HQ building, standing at approximately 74 storeys tall.
Though a large portion of the oxygen-rich world is of moderate climate and stable geology, extreme regions show signs of historical tectonic instability and inclement conditions - all of which appear to have been countered through a combined use of biodomes and terraforming techniques (techniques which are also evident across other planetary bodies in this star system). Further in depth study by Starfleet research teams has yielded additional insight into the cultural and spiritual heart of the Forged people; being the cathedral which now sits at the heart of The Valley and preserves the remnants of the original colony vessel. Though the limited remains of the now deeply buried vessel are largely preserved for posterity, a significant section of it has been re-purposed as a prestigious burial site which yields yet further insight into the spiritual connection formed between the modern population and their immediate ancestry.
SYSTEM INDEX
Newsia | Class E
//Detailed survey to be conducted//
Newopa | Class S
//Detailed survey to be conducted//
Newsa | Class K
Newceana | Class L
Newna (Forged Earth) | Class M
Newfrika | Class M
Newtica | Class P
//Detailed survey to be conducted//
NEWSA
Physics | Class K |
Type | Small iron/silicate |
Radius | 1952.51 km (0.31 x earth) |
Surface Area | 4.79 x 107 km2 |
Land Area | 4.84 x 107 km2 (0.32 x earth) |
Mass | 1.53 x 1023 kg (0.03 x earth) |
Density | 4.91 g/cm3 (0.89 x earth) |
Composition | 37.2% oxygen, 36.4% iron, 20.7% silicon, 3.3% other metals, 2.4% other elements |
Gravimetry | | Atmosphere | |
Gravity | 2.67 m/s2 (0.27 x earth) | Type | Thin toxic |
Escape Velocity | 3.23 km/s | Pressure | 20.76 kPa (0.20 x earth) |
| | Composition | 80.2% sulfur dioxide, 19.8% carbon dioxide, trace other gases |
Rotation | | Hydrosphere | | Biosphere | |
Period | 24.95 hours | Water | 0 % | Chemistry | Carbon |
Axis Tilt | 20.41 ° | Ice | 37 % | Lifeforms | N/A |
Climate | | Civilization | |
Type | Cold | Type | N/A |
Min Temp | 220 K (-53 °C) | Population | N/A |
Avg Temp | 285 K (12 °C) | Society | N/A |
Max Temp | 444 K (171 °C) | Tech Level | N/A |
Special Features | Planetary Rings |
NEWCEANA
Physics | Class L |
Type | Small iron/silicate |
Radius | 6651.43 km (1.04 x earth) |
Surface Area | 5.56 x 108 km2 |
Land Area | 3.95 x 108 km2 (2.65 x earth) |
Mass | 6.52 x 1024 kg (1.09 x earth) |
Density | 5.29 g/cm3 (0.96 x earth) |
Composition | 37.7% iron, 28.4% oxygen, 17.9% silicon, 5.3% magnesium, 4.8% sulphur, 4.8% other metals, 1.2% other elements |
Gravimetry | | Atmosphere | |
Gravity | 9.79 m/s2 (1.00 x earth) | Type | Thin toxic |
Escape Velocity | 11.41 km/s | Pressure | 56.30 kPa (0.56 x earth) |
| | Composition | 79.4% sulfur dioxide, 20.6% carbon dioxide, trace other gases |
Rotation | | Hydrosphere | | Biosphere | |
Period | 16.92 hours | Water | 30 % | Chemistry | Carbon |
Axis Tilt | 39.19 ° | Ice | 10 % | Lifeforms | Prokaryotic microbes |
Climate | | Civilization | |
Type | Standard | Type | N/A |
Min Temp | 292 K (19 °C) | Population | N/A |
Avg Temp | 297 K (24 °C) | Society | N/A |
Max Temp | 330 K (57 °C) | Tech Level | N/A |
Special Features | |
NEWNA (Forged Earth)
Physics | Class M |
Type | Large iron/silicate |
Radius | 9507.68 km (1.49 x earth) |
Surface Area | 1.14 x 109 km2 |
Land Area | 7.72 x 108 km2 (5.19 x earth) |
Mass | 1.83 x 1025 kg (3.06 x earth) |
Density | 5.07 g/cm3 (0.92 x earth) |
Composition | 40.3% iron, 31.2% oxygen, 18.8% silicon, 5.4% calcium, 3.0% other metals, 1.3% other elements |
Gravimetry | | Atmosphere | |
Gravity | 13.41 m/s2 (1.37 x earth) | Type | Dense breathable |
Escape Velocity | 15.97 km/s | Pressure | 170.13 kPa (1.68 x earth) |
| | Composition | 73.7% oxygen, 26.3% argon, trace other gases |
Rotation | | Hydrosphere | | Biosphere | |
Period | 27.66 hours | Water | 53 % | Chemistry | Carbon |
Axis Tilt | 55.58 ° | Ice | 33 % | Lifeforms | Prokaryotic microbes, fungi, bryophytes, flora & fauna, land mammals, aquatic, humanoid |
Climate | | Civilization | |
Type | Standard | Type | Colony |
Min Temp | 240 K (-33 °C) | Population | 216,433,038 |
Avg Temp | 302 K (29 °C) | Society | Representative Democracy |
Max Temp | 401 K (128 °C) | Tech Level | Spacefaring |
Special Features | Planetary rings, wreckage of a crashed starship (Valley Forge ~2150) |
NEWFRIKA
Physics | Class M |
Type | Large iron/silicate |
Radius | 8688.06 km (1.36 x earth) |
Surface Area | 9.49 x 108 km2 |
Land Area | 8.73 x 108 km2 (5.86 x earth) |
Mass | 1.46 x 1023 kg (2.45 x earth) |
Density | 5.32 g/cm3 (0.97 x earth) |
Composition | 33.2% iron, 26.1% oxygen, 18.2% other metals, 12.7% aluminum, 7.1% sulphur, 2.7% other elements |
Gravimetry | | Atmosphere | |
Gravity | 12.87 m/s2 (1.32 x earth) | Type | Dense breathable |
Escape Velocity | 14.95 km/s | Pressure | 126.77 kPa (1.25 x earth) |
| | Composition | 87.4% nitrogen, 12.6% oxygen, trace other gases |
Rotation | | Hydrosphere | | Biosphere | |
Period | 17.54 hour | Water | 9 % | Chemistry | Carbon |
Axis Tilt | 17.82 ° | Ice | 2 % | Lifeforms | Prokaryotic microbes, fungi, bryophytes, flora & fauna |
Climate | | Civilization | |
Type | Cold | Type | Colony |
Min Temp | 229 K (-43 °C) | Population | ~56,472 |
Avg Temp | 296 K (23 °C) | Society | Representative Democracy |
Max Temp | 300 K (27 °C) | Tech Level | Spacefaring |
Special Features | Element One mining facility, Iconian facility (archaeological excavation) |
Reference Documents:
Astrological Survey, Newsa
SUBMITTED: Stardate 95301.5 FILED BY: LT K. Sumida, Acting CSO, U.S.S. Attar SECURITY: Level 1 - Open
LOCATION: Newsa, Forged Earth System
MISSION: Astrological survey of Newsa
OUTCOME: All data collected and duly stored; further analysis underway; new sensor anomaly detected and under investigation
NARRATIVE: Standard analysis from geo-centric orbit of Newsa has proven to be harder than originally estimated. The presence of a very slight percentage, though highly concentrated, of high-density minerals under the planet surface has initially hampered some of the efforts put by the Geology Department to accurately map the mineral deposits in certain areas. In order to compensate, a modification has been implemented to the ship's multi-band linear sensor suites. This modification allowed a more in-depth penetration of small-size portions of the surface for a more accurate analysis of the different mineral layers. A few hours before the survey was to be completed, another gravitational anomaly, identical to the one already detected while in Newceana's orbit, showed up on sensors. However, it proved impossible to determine almost anything about it, and due to its sudden disappearance, it is actually considered to be a sensor anomaly. Under specific orders by Capt. Timoreev, Engineering is now employing all available resources in order to identify and contain the anomaly in our sensor systems, in order to avoid any interference with the data coming from our surveys. Five probes have also been launched on the planet surface to collect geological samples which are now under detailed analysis in our laboratories. DATA: Physics Type Small iron/silicate Radius 1952.51 km (0.31 x earth) Surface Area 4.79 x 107 km2 Land Area 4.84 x 107 km2 (0.32 x earth) Mass 1.53 x 1023 kg (0.03 x earth) Density 4.91 g/cm3 (0.89 x earth) Composition 37.2% oxygen, 36.4% iron, 20.7% silicon, 3.3% other metals, 2.4% other elements Gravimetry Gravity 2.67 m/s2 (0.27 x earth) Escape Velocity 3.23 km/s Rotation Period 24.95 hours Axis Tilt 20.41 ° Hydrosphere Water 0 % Ice 37 % Atmosphere Type Thin toxic Pressure 20.76 kPa (0.20 x earth) Composition 80.2% sulfur dioxide, 19.8% carbon dioxide, trace other gases Climate Type Cold Min Temp 220 K (-53 °C) Avg Temp 285 K (12 °C) Max Temp 444 K (171 °C)
Astrological Survey, Newceana
SUBMITTED: Stardate 95284.2 FILED BY: LT K. Sumida, Acting CSO, U.S.S. Attar SECURITY: Level 1 - Open
LOCATION: Newceana, Forged Earth System
MISSION: Astrological survey of Newceana
OUTCOME: All data collected and duly stored; further analysis underway; sensor malfunction identified and repaired
NARRATIVE: After completing its survey of Newna, the U.S.S. Attar has moved on to Newceana. Sensors had already started collecting data during transit, but once standard orbit had been established, work began in order to obtain a preliminary survey of the whole planet as soon as possible. The idea was to spot and identify those elements of potential interests that would have been worthy of further and closer inspection. In particular, attention has been devoted to those elements which could have helped clarify the geological history of the planet, in conjunction with the work of the archaeological team on the surface, and to trace eventual traces left by other Iconian facilities. Unfortunately, collection of data had been hampered by a suspected gravitational anomaly. Further analysis, however, proved that the anomaly was, in fact, a fake signal, the result of a sensor malfunction. Engineering has promptly intervened in order to re-establish sensor standard capacity, though a full investigation of the causes of the issue is still underway. The malfunction has in no way altered the result of the successive analysis. DATA: Physics: Type Standard iron/silicate Radius 6651.43 km (1.04 x earth) Surface Area 5.56 x 108 km2 Land Area 3.95 x 108 km2 (2.65 x earth) Mass 6.52 x 1024 kg (1.09 x earth) Density 5.29 g/cm3 (0.96 x earth) Composition 37.7% iron, 28.4% oxygen, 17.9% silicon, 5.3% magnesium, 4.8% sulphur, 4.8% other metals, 1.2% other elements Gravimetry: Gravity 9.79 m/s2 (1.00 x earth) Escape Velocity 11.41 km/s Rotation: Period 16.92 hours Axis Tilt 39.19 ° Hydrosphere: Water 30 % Ice 10 % Atmosphere: Type Thin toxic Pressure 56.30 kPa (0.56 x earth) Composition 79.4% sulfur dioxide, 20.6% carbon dioxide, trace other gases Climate: Type Standard Min Temp 292 K (19 °C) Avg Temp 297 K (24 °C) Max Temp 330 K (57 °C) Biosphere: Chemistry Carbon Lifeforms Prokaryotic microbes Civilization: N/A
Astrological Survey, Newna
SUBMITTED: Stardate 95246.6 FILED BY: CAPT A. A. Timoreev, U.S.S. Attar SECURITY: Level 1 - Open
LOCATION: Newna (Forged Earth)
MISSION: Astrological survey of Newna
OUTCOME: All data collected and duly stored; currently under second-step analysis
KEY PERSONNEL:
CAPT A. A. Timoreev NARRATIVE: The Attar has kept its position in orbit of Newna (Forged Earth) for one week in order to collect as many astrological data as possible while the first ethnological and anthropological surveys (see the report here). All data have passed through a first analysis by the ship's Astronomy Department. Second-step analysis currently underway. DATA: Physics: Type Large iron/silicate Radius 9507.68 km (1.49 x earth) Surface Area 1.14 x 109 km2 Land Area 7.72 x 108 km2 (5.19 x earth) Mass 1.83 x 1025 kg (3.06 x earth) Density 5.07 g/cm3 (0.92 x earth) Composition 40.3% iron, 31.2% oxygen, 18.8% silicon, 5.4% calcium, 3.0% other metals, 1.3% other elements Gravimetry: Gravity 13.41 m/s2 (1.37 x earth) Escape Velocity 15.97 km/s Rotation: Period 27.66 hours Axis Tilt 55.58 ° Hydrosphere: Water 53 % Ice 33 % Atmosphere: Type Dense breathable Pressure 170.13 kPa (1.68 x earth) Composition 73.7% oxygen, 26.3% argon, trace other gases Climate: Type Standard Min Temp 240 K (-33 °C) Avg Temp 302 K (29 °C) Max Temp 401 K (128 °C) Biosphere: Chemistry Carbon Lifeforms Prokaryotic microbes, fungi, bryophytes, flora & fauna, land mammals, aquatic, humanoid Civilization: Type Colony Population 216,433,038 Society Representative Democracy Tech Level Spacefaring Special: Features Planetary rings, wreckage of a crashed starship (Valley Forge ~2150)
RECOMMENDATIONS: The survey has been extremely thourough, and has amply exploited the sensors and data collection capabilites of the Attar. Thus, it is my opinion that, on this front, no further developments are necessary. However, we are dealing with a planetary body which has been home of a non-indigenous species, for unknown reasons, for centuries. First of all, we could profit from this by collecting historical astrological data by the inhabitants of Newna; second, we should further study the relationship eventually existing between this planet and any astronomical phenomenon present inside or nearby this system. On a side note, this has been also a good occasion to further enhance the Attar sensors, and particularly the multi-linear band sensor suites, in order to improve their overall performance in detecting tectonic fluctuations under high-density metallic soils. Further data about these improvements will be delivered by the ship Engineering Department as soon as they are processed.
//signed//
Captain Andrej A. Timoreev,
Commanding Officer, U.S.S. Attar
38th Fleet
Archaeological Report, Newfrika
SUBMITTED: Stardate 95268.2 FILED BY: CMDR Iria, U.S.S. Attar SECURITY: Level 1 - Open
LOCATION: Newfrika, Newna System
MISSION: Archaeological exploration of site of presumed Iconian gateway on the planet's surface
OUTCOME: Preliminary data collected and currently under examination; exploration still on going
KEY PERSONNEL:
CMDR Iria LCDR Lendaria ENS V. Monnir Prof. Lycas NARRATIVE: Under the leadership of prof. Lycas, as expert in the field, the expedition has explored the caves that lead to the entrance of the Iconian facility under the surface of Newfrika. Preliminary findings confirm a natural origin of the caves themselves, which is also further confirmed by the first chronological data available at the moment regarding the time the faciltiy was built. Further geological analysis in this sense is still on going to help determine chronology with higher accuracy. Also, geological analysis is underway on the crystals which have been found, in huge deposites, all around the caves.Though no particular or unexpected element has been detected yet, the nature of these formations may be somehow connected to the facility itself. Significant samples have been transpored on the U.S.S. Kassandra, which is currently en route to bring them to Deep Space 13 for more accurate analysis. Until now, only a part of the Iconian faciltiy has been explored. Accordingly to our first estimates, this part accounts to less than a quarter of the total surface occupied by the facility itself. The explored section contains two huge rooms and a number of corridors. Overall, it has been proven impossible to determine the exact nature and purpose of the facility. However, in this sense, Lt. Cmdr. Lendaria have uncovered the fragments of a tablet (see attachment below for a visual representation): accordin to the first attempts of translation, it may contain useful evidence concerning the facility purpose. RECOMMENDATIONS: As already mentioned, the U.S.S. Kassandra is currently bringing geological samples to Deep Space 13. Analysis of these samples is deemed to be of the utmost interest in order to understand more of the planet's geological evolution, and in order to uncover any possible relation with the Iconian presence on it. The expedition is already moving forward to clear more sections of the Iconian facility. However, due to the peculiar nature of the site, it is proceeding with extreme caution. Translations attempts of the tablet will be intensified. However, it is the opinion of the author of this report that only the discovery of further writing samples could produce significant progresses in this sense.
Geological Report, Newfrika
SUBMITTED: Stardate 95313.6 FILED BY: ENS Sorik SECURITY: Level 1 - Open
TITLE: Newfrika Geological Sample Analysis
LEAD SCIENTIST: ENS Sorik
ABSTRACT: Samples were provided to the geological laboratory for analysis: general core sample 95248_C_Newfrika; mineral sample 95251.1a, and fuel sample E-On_I. General chemical and engineering analysis was done for samples 95248_C_Newfrika, while 95251.1a underwent more in-depth chemical and structural analysis. Sample E-On_I underwent some basic scans and virtual testing. Results suggest that the mineral and fuel samples are related, specifically that E-On_I is a dilithium product somehow extracted from the minerals. This has implications for the Forged people of Newfrika, as well as for Iconian technology found in proximity to the mineral.
INTRODUCTION: Newfrika is a planet in the Forged Earth System, and is populated by the Forged, humanoids of human ancestry. It was recently (stardate 95126.1) visited by a Starfleet team (AAR; CAPT K Se'Lai) and found to contain non-indigenous technology, close to which were found a large number of clear crystal deposits, some of which contained a rare fuel source utilized by the Forged called Element One. The crystals were identified in the field as decrystallized dilithium, but samples were collected for further analysis. The non-indigenous technology was discovered to be Iconian in origin, and the mineral deposits were localized near it.
On a subsequent trip to the planet (stardate 95268.2), an archeological team led by a Professor Lycas (AAR; CMDR Iria) collected more samples, some of which were sent to this lab for analysis. It was theorized at the time that the crystal formations were related to the presence of the Iconian technology.
METHODS:
- 95248_C_Newfrika: This a single core sample from the local strata. Log of boring transferred with sample, attached below. Sample 1 is of the topsoil, and represents depth approx 0-4m. Silty gravel, loose, not very moist. No further tests conducted. Sample 2 is made up of variously colored clays, 4-17m, very stiff. Took moisture sample from various depths, ranges from approx 20% at the top to 44% at the bottom, where groundwater was observed. Below this is bedrock, as represented by sample 3. Shale, various fossils, mostly trace fossils. Nothing unusual. Below this is sample 4, dolomite, nothing unusual. Below that is a gneiss of some type.
Sample 1 tested for nutrient load and engineering properties; sieve testing and hydrometer tests confirmed initial observation as silty gravel. pH of 7.3, phosphate of 68 mg/L, potassium of 342 mg/L, magnesium of 422 mg/L; nickel, zinc, copper, and other metals are negligible. Sample 2 tested for chemical composition and structure: chemically consists of a mix of clay minerals, including kaolins and illites, generally arranged in randomly ordered layers. Liquid limit of 64, plastic limit of 23, plasticity index of 41 (CH).
- 95251.1a: Clear crystalline samples, found in mining tunnels. Visually appears very much like dilithium or common quartz, although the crystal system appears slightly different than both of those. Luster: non-metallic, vitreous. Color: colorless, and very clear, lacking even small spots of impurities besides dirt particles clinging to surface. Streak: n/a, too hard. Mohs Hardness: 9. Fracture: conchoidal. Specific gravity: roughly 3 but must refine. Effervescence: none. Taste:... not recommended. Smell: none.
Samples tested for chemical and structural composition by use of X-ray fluorescence and diffraction, ICP-MS, and replicator analysis. Chemically most closely matches almandine, which has a general formula of Fe2+3Al2Si3O12, but structurally more closely resembles common quartz, with a trigonal crystal system and a trapezohedral (class 3 2) crystal class. Mineral has a relatively high conductivity for a silicate, of approximately 6x103 S/m, similar to graphite. Overall has many of the same characteristics as decrystallized dilithium.
- E-On_I: Sample isotope of the Forged 'Element-One' fuel source. Isotope samples so general observation impossible, with the exception of density. Sample appears unusually heavy for its size.
Replicator was unable to analyze the sample, but some basic passive tricorder scans were able to return results. Sample produced a small amount of gamma radiation (about 0.42 mSv) and trace amounts of Illium-629 were detected in the sample. On a hunch that this was some kind of dilithium analogue or surrogate, collected as much data about the sample as possible in the tricorder, then fed it into the computer and took it to the holodeck, where a larger amount of virtual fuel was fed into a simulated warp core. The core rapidly created a massive spike of energy (enough to power 30 Galaxy-class starships) before promptly exploding. Back in the lab, placed sample in a containment field for safety and took more passive scans, as well as analyzed the holodeck results. Power signature is consistent with that of dilithium, but increased exponentially.
RESULTS AND DISCUSSION: The general core sample was unremarkable, as it had average engineering and nutrient qualities. Some of the same elements found in the crystals was found in the underlying bedrocks, suggesting a mechanism of crystal formation inside the caves where they were found.
The crystals are, essentially, decrystallized dilithium, but with several small differences in chemical composition and structure, which indicates that they were drained by a mechanism that hasn't yet been observed in, for example, starship warp cores. Their clear color is surprising given the amount of impurities, including iron and aluminum, in the crystal structure. It also has an unusually high conductivity for a silicate mineral, which could be partially attributable to its metal content but may, as with its transparency, be related to the crystal's unusual formation or use.
The Element One fuel testing results indicate that it is essentially a highly refined dilithium-like substance, but with a much higher power density. There were, however, sources of error during my experiments, as the fuel's exact characteristics could not be determined by passive scanning, and what information could be gained was fed into the computer for simulated testing manually. Given Element One's proximity to the crystals, and the crystals' similarity to decrystallized dilithium, it can be theorized that Element One is a dilithium product that has been extracted from the crystals. I did not have access (perhaps wisely) to Iconian technology so I could not test the crystal or fuel's relation or interactions with it, but given the crystals' proximity to the Iconian technology found in the caves, initial reports that it was the Iconians who did this refining may be correct.
RECOMMENDATIONS: Further, and more specific, engineering or nutrient studies are recommended if specific engineering or farming operations are to be performed, as the core sample tested represented only one location.
Further examination of the Element One fuel source will be necessary to determine its exact properties. But if it is indeed a dilithium derivative, these findings may allow the Forged to adapt their tech from running on the extremely rare Element One fuel to running on relatively more common dilithium. This would increase their technological advancement and undoubtedly increase trade.
The findings that the crystals are essentially decrystallized dilithium warrants further study. If so, it may be possible to adapt current dilithium recrystallization procedures to suit the crystals. Additionally, if there is a connection between the crystals and the Iconian tech found in the caves, it may provide a mechanism for repowering it.
Geological Survey logs
Security Level 1 - Open Project Title: Newfrika Geological Sample Analysis Key Personnel: ENS Sorik Materials in Use: Newfrika samples, preparation tools (laser cutter, rock granulator, rock hammer, etc.), replicator, plasma mass spectrometer, scanning electron microscope, X-ray diffractometer Lab Space in Use: Geology Lab 3
Stardate 95288.6
Initial observations:
- 95248_C_Newfrika: This a single core sample from the local strata. Log of boring transferred with sample, attached below. Sample 1 is of the topsoil, and represents depth approx 0-4m. Silty gravel, loose, not very moist. No further tests conducted. Sample 2 is made up of variously colored clays, 4-17m, very stiff. Took moisture sample from various depths, ranges from approx 20% at the top to 44% at the bottom, where groundwater was observed. Below this is bedrock, as represented by sample 3. Shale, various fossils, mostly trace fossils. Nothing unusual. Below this is sample 4, dolomite, nothing unusual. Below that is a gneiss of some type.
- 95251.1a: Clear crystalline samples, found in mining tunnels. Visually appears very much like dilithium or common quartz, although the crystal system appears slightly different than both of those. Luster: non-metallic, vitreous. Color: colorless, and very clear, lacking even small spots of impurities besides dirt particles clinging to surface. Streak: n/a, too hard. Mohs Hardness: 9. Fracture: conchoidal. Specific gravity: roughly 3 but must refine. Effervescence: none. Taste:... not recommended. Smell: none. Will prepare samples for chemical and physical analysis.
E-On_I: Sample isotope of the Forged 'Element-One' fuel source. Isotope samples so general observation impossible, with the exception of density. Sample appears unusually heavy for its size.
Next steps:
Will take various samples of 95248_C_Newfrika samples 3-5 for chemical analysis, and will take intact core segments for structural testing. Will prepare 95251.1a samples for chemical and physical analysis. Will keep E-On_I sample isolated for now, until non-destructive testing regimen can be developed.
Attachment:
95248_C_Newfrika.log
95313.4
Lab testing:
- 95248_C_Newfrika: Sample 1 tested for nutrient load and engineering properties; sieve testing and hydrometer tests confirmed initial observation as silty gravel. pH of 7.3, phosphate of 68 mg/L, potassium of 342 mg/L, magnesium of 422 mg/L; nickel, zinc, copper, and other metals are negligible. Sample 2 tested for chemical composition and structure: chemically consists of a mix of clay minerals, including kaolins and illites, generally arranged in randomly ordered layers. Liquid limit of 64, plastic limit of 23, plasticity index of 41 (CH).
- 95251.1a: Samples tested for chemical and structural composition by use of X-ray fluorescence and diffraction, ICP-MS, and replicator analysis. Chemically most closely matches almandine, which has a general formula of Fe2+3Al2Si3O12, but structurally more closely resembles common quartz, with a trigonal crystal system and a trapezohedral (class 3 2) crystal class. Mineral has a relatively high conductivity for a silicate, of approximately 6x103 S/m, similar to graphite. Overall has many of the same characteristics as decrystallized dilithium.
- E-On_I: Replicator was unable to analyze the sample, but some basic passive tricorder scans were able to return results. Sample produced a small amount of gamma radiation (about 0.42 mSv) and trace amounts of Illium-629 were detected in the sample. On a hunch that this was some kind of dilithium analogue or surrogate, collected as much data about the sample as possible in the tricorder, then fed it into the computer and took it to the holodeck, where a larger amount of virtual fuel was fed into a simulated warp core. The core rapidly created a massive spike of energy (enough to power 30 Galaxy-class starships) before promptly exploding. Back in the lab, placed sample in a containment field for safety and took more passive scans, as well as analyzed the holodeck results. Power signature is consistent with that of dilithium, but increased exponentially.
Next steps:
Will write formal report with analysis